From 9e968ba8330f2eab4c192e1e5b2bb10b762137d8 Mon Sep 17 00:00:00 2001 From: Patrick Peglar Date: Tue, 15 Aug 2023 13:59:21 +0100 Subject: [PATCH] Update standard-names to #82, and add version info into generated 'std_names' module. --- etc/cf-standard-name-table.xml | 2463 ++++++++++++++++-------------- lib/iris/tests/test_std_names.py | 10 +- tools/generate_std_names.py | 9 +- 3 files changed, 1328 insertions(+), 1154 deletions(-) diff --git a/etc/cf-standard-name-table.xml b/etc/cf-standard-name-table.xml index 3b145ae86ed..6e3c0148490 100644 --- a/etc/cf-standard-name-table.xml +++ b/etc/cf-standard-name-table.xml @@ -1,7 +1,7 @@ - 81 - 2023-04-25T10:43:33Z + 82 + 2023-07-06T13:17:07Z Centre for Environmental Data Analysis support@ceda.ac.uk @@ -269,14 +269,14 @@ m - The altitude at top of atmosphere boundary layer is the elevation above sea level of the top of the (atmosphere) planetary boundary layer. The phrase "defined_by" provides the information of the tracer used for identifying the atmospheric boundary layer top. "Ambient_aerosol" means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. "Ambient aerosol particles" are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles. "By ranging instrument" means that the backscattering is obtained through ranging techniques like lidar and radar. + The altitude at top of atmosphere boundary layer is the elevation above sea level of the top of the (atmosphere) planetary boundary layer. The phrase "defined_by" provides the information of the tracer used for identifying the atmospheric boundary layer top. "Ambient_aerosol" means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. "Ambient aerosol particles" are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles. "By ranging instrument" means that the backscattering is obtained through ranging techniques like lidar and radar. m - The altitude at top of atmosphere mixed layer is the elevation above sea level of the top of the (atmosphere) mixed layer or convective boundary layer. The phrase "defined_by" provides the information of the tracer used for identifying the atmospheric boundary layer top. "Ambient_aerosol" means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. "Ambient aerosol particles" are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles. "By ranging instrument" means that the volume backscattering coefficient is obtained through ranging techniques like lidar and radar. + The altitude at top of atmosphere mixed layer is the elevation above sea level of the top of the (atmosphere) mixed layer or convective boundary layer. The phrase "defined_by" provides the information of the tracer used for identifying the atmospheric boundary layer top. "Ambient_aerosol" means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. "Ambient aerosol particles" are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles. "By ranging instrument" means that the volume backscattering coefficient is obtained through ranging techniques like lidar and radar. @@ -469,21 +469,21 @@ - J kg -1 + J kg-1 Convective(ly) available potential energy (often abbreviated CAPE) is a stability measure calculated by integrating the positive temperature difference between the surrounding atmosphere and a parcel of air lifted adiabatically from the surface to its equilibrium level. CAPE exists under conditions of potential instability, and measures the potential energy per unit mass that would be released by the unstable parcel if it were able to convect upwards to equilibrium. - J kg -1 + J kg-1 Convective inhibition is the amount of energy per unit mass required to overcome the negatively buoyant energy exerted by the environment on a parcel of air. Convective inhibition is often abbreviated as "CIN" or "CINH". It is calculated by integrating the negative temperature difference between the surrounding atmosphere and a parcel of air lifted adiabatically from a given starting height to its equilibrium level. A coordinate variable of original_air_pressure_of_lifted_parcel should be specified to indicate the starting height of the lifted parcel. - J kg -1 + J kg-1 Convective inhibition is the amount of energy per unit mass required to overcome the negatively buoyant energy exerted by the environment on a parcel of air. Convective inhibition is often abbreviated as "CIN" or "CINH". It is calculated by integrating the negative temperature difference between the surrounding atmosphere and a parcel of air lifted adiabatically from the surface to its equilibrium level. @@ -3170,6 +3170,20 @@ The phrase "ratio_of_X_to_Y" means X/Y. It may be expressed as a fraction, a percentage, or any other dimensionless representation of a fraction. Also known as specific gravity, where soil represents a dry soil sample. The density of a substance is its mass per unit volume. + + degree_north + + + The latitude of deployment of a station or instrument. The term can be used whenever the deployment position of a station or instrument needs to be supplied along with other types of positions. If a data variable has only one latitude coordinate variable, the standard name of latitude should generally be preferred to deployment_latitude, because latitude is recognised by generic software. If the deployment latitude is also the nominal latitude for a discrete geometry (as in Section 9.5 of the CF convention), the deployment latitude should also, or instead, be recorded in a coordinate variable with the standard name of latitude and axis="Y". Latitude is positive northward; its units of "degree_north" (or equivalent) indicate this explicitly. + + + + degree_east + + + The longitude of deployment of a station or instrument. The term can be used whenever the deployment position of a station or instrument needs to be supplied along with other types of positions. If a data variable has only one longitude coordinate variable, the standard name of longitude should generally be preferred to deployment_longitude, because longitude is recognised by generic software. If the deployment longitude is also the nominal longitude for a discrete geometry (as in Section 9.5 of the CF convention), the deployment longitude should also, or instead, be recorded in a coordinate variable with the standard name of longitude and axis="X". Longitude is positive eastward; its units of "degree_east" (or equivalent) indicate this explicitly. + + m @@ -3720,7 +3734,7 @@ kg m-2 - The quantity with standard name drainage_amount_through_base_of_soil_model is the amount of water that drains through the bottom of a soil column extending from the surface to a specified depth. “Drainage” is the process of removal of excess water from soil by gravitational flow. "Amount" means mass per unit area. A vertical coordinate variable or scalar coordinate with standard name "depth" should be used to specify the depth to which the soil column extends. + The quantity with standard name drainage_amount_through_base_of_soil_model is the amount of water that drains through the bottom of a soil column extending from the surface to a specified depth. "Drainage" is the process of removal of excess water from soil by gravitational flow. "Amount" means mass per unit area. A vertical coordinate variable or scalar coordinate with standard name "depth" should be used to specify the depth to which the soil column extends. @@ -4437,6 +4451,13 @@ Longitude is positive eastward; its units of degree_east (or equivalent) indicate this explicitly. In a latitude-longitude system defined with respect to a rotated North Pole, the standard name of grid_longitude should be used instead of longitude. Grid longitude is positive in the grid-eastward direction, but its units should be plain degree. + + mol m-3 s-1 + + + "Gross mole production" means the rate of creation of biomass per unit volume with no correction for respiration loss in terms of quantity of matter (moles). The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. "Prokaryotes" means all Bacteria and Archaea excluding photosynthetic cyanobacteria such as Synechococcus and Prochlorococcus or other separately named components of the prokaryotic population. + + kg m-2 s-1 @@ -4458,6 +4479,13 @@ "Production of carbon" means the production of biomass expressed as the mass of carbon which it contains. Gross primary production is the rate of synthesis of biomass from inorganic precursors by autotrophs ("producers"), for example, photosynthesis in plants or phytoplankton. The producers also respire some of this biomass and the difference is "net_primary_production". "Productivity" means production per unit area. The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. + + kg m-3 s-1 + + + "Gross production" means the rate of creation of biomass per unit volume with no correction for respiration. The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. "Prokaryotes" means all Bacteria and Archaea excluding photosynthetic cyanobacteria such as Synechococcus and Prochlorococcus or other separately named components of the prokaryotic population. + + 1 @@ -7854,7 +7882,7 @@ - J Kg-1 + J kg-1 The lightning_potential_index measures the potential for charge generation and separation that leads to lightning flashes in convective thunderstorms. It is derived from the model simulated grid-scale updraft velocity and the mass mixing-ratios of liquid water, cloud ice, snow, and graupel. @@ -8539,6 +8567,13 @@ Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for chlorine nitrate is ClONO2. + + kg m-3 + + + "Mass concentration" means mass per unit volume and is used in the construction "mass_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". Chlorophylls are the green pigments found in most plants, algae and cyanobacteria; their presence is essential for photosynthesis to take place. There are several different forms of chlorophyll that occur naturally. All contain a chlorin ring (chemical formula C20H16N4) which gives the green pigment and a side chain whose structure varies. The naturally occurring forms of chlorophyll contain between 35 and 55 carbon atoms. Chlorophyll-a is the most commonly occurring form of natural chlorophyll. The chemical formula of chlorophyll-a is C55H72O5N4Mg. "Sea ice" means all ice floating in the sea which has formed from freezing sea water, rather than by other processes such as calving of land ice to form icebergs. + + kg m-3 @@ -9260,6 +9295,13 @@ Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of X to the mass of Y (including X). A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". Petroleum hydrocarbons are compounds containing just carbon and hydrogen originating from the fossil fuel crude oil. + + kg m-3 + + + "Mass concentration" means mass per unit volume and is used in the construction "mass_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". Phaeopigments are non-photosynthetic pigments that are the degradation product of algal chlorophyll pigments. It is commonly formed during and after marine phytoplankton blooms. "Sea ice" means all ice floating in the sea which has formed from freezing sea water, rather than by other processes such as calving of land ice to form icebergs. + + kg m-3 @@ -9351,6 +9393,13 @@ Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. Aerosol takes up ambient water (a process known as hygroscopic growth) depending on the relative humidity and the composition of the aerosol. "Dry aerosol particles" means aerosol particles without any water uptake. "Primary particulate organic matter " means all organic matter emitted directly to the atmosphere as particles except elemental carbon. The sum of primary_particulate_organic_matter_dry_aerosol and secondary_particulate_organic_matter_dry_aerosol is particulate_organic_matter_dry_aerosol. + + kg m-3 + + + "Mass concentration" means mass per unit volume and is used in the construction "mass_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. "Prokaryotes" means all Bacteria and Archaea excluding photosynthetic cyanobacteria such as Synechococcus and Prochlorococcus or other separately named components of the prokaryotic population. + + kg m-3 @@ -11669,7 +11718,7 @@ - mol/m3 + mol m-3 "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Dissolved organic nitrogen" describes the nitrogen held in carbon compounds in solution. These are mostly generated by plankton excretion and decay. @@ -12123,6 +12172,13 @@ Mole concentration means number of moles per unit volume, also called "molarity", and is used in the construction mole_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. The chemical formula for ozone is O3. + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. + + mol m-3 @@ -12130,6 +12186,41 @@ "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. + + + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. + + + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. + + + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. Phosphorus means phosphorus in all chemical forms, commonly referred to as "total phosphorus". + + + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. + + mol m-3 @@ -12137,6 +12228,27 @@ Mole concentration means number of moles per unit volume, also called"molarity", and is used in the construction mole_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. + + + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. + + + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Particulate means suspended solids of all sizes. + + mol m-3 @@ -12235,6 +12347,13 @@ Mole concentration means number of moles per unit volume, also called "molarity", and is used in the construction mole_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Picophytoplankton are phytoplankton of less than 2 micrometers in size. Phytoplankton are algae that grow where there is sufficient light to support photosynthesis. + + mol m-3 + + + "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical species or biological group denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". The phrase "expressed_as" is used in the construction "A_expressed_as_B", where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. "Prokaryotes" means all Bacteria and Archaea excluding photosynthetic cyanobacteria such as Synechococcus and Prochlorococcus or other separately named components of the prokaryotic population. + + mol m-3 @@ -13877,7 +13996,7 @@ W - "Northward" indicates a vector component which is positive when directed northward (negative southward). The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. + "Northward" indicates a vector component which is positive when directed northward (negative southward). The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. @@ -14409,7 +14528,7 @@ kg s-1 - The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. + The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. @@ -14759,7 +14878,7 @@ kg s-1 - "y" indicates a vector component along the grid y-axis, positive with increasing y. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. + "y" indicates a vector component along the grid y-axis, positive with increasing y. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. @@ -14920,7 +15039,7 @@ m s-1 - "Heave rate" is the rate of displacement along the local vertical axis. Heave rate might not include changes to the “at rest” position of the platform with respect to the axis of displacement, which may change over time. The standard name platform_heave_rate should be chosen only if the sign convention of the data is unknown. For cases where the sign convention of the heave rate is known, a standard name of platform_heave_rate_down or platform_heave_rate_up should be chosen, as appropriate. A "platform" is a structure or vehicle that serves as a base for mounting sensors. Platforms include, but are not limited to, satellites, aeroplanes, ships, buoys, instruments, ground stations, and masts. + "Heave rate" is the rate of displacement along the local vertical axis. Heave rate might not include changes to the "at rest" position of the platform with respect to the axis of displacement, which may change over time. The standard name platform_heave_rate should be chosen only if the sign convention of the data is unknown. For cases where the sign convention of the heave rate is known, a standard name of platform_heave_rate_down or platform_heave_rate_up should be chosen, as appropriate. A "platform" is a structure or vehicle that serves as a base for mounting sensors. Platforms include, but are not limited to, satellites, aeroplanes, ships, buoys, instruments, ground stations, and masts. @@ -18154,7 +18273,7 @@ sr - The ratio of volume extinction coefficient to volume backwards scattering coefficient by ranging instrument in air due to ambient aerosol particles (often called "lidar ratio") is the ratio of the "volume extinction coefficient" and the "volume backwards scattering coefficient of radiative flux by ranging instrument in air due to ambient aerosol particles". The ratio is assumed to be related to the same wavelength as the incident radiation. "Ambient_aerosol" means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. "Ambient aerosol particles" are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. + The ratio of volume extinction coefficient to volume backwards scattering coefficient by ranging instrument in air due to ambient aerosol particles (often called "lidar ratio") is the ratio of the "volume extinction coefficient" and the "volume backwards scattering coefficient of radiative flux by ranging instrument in air due to ambient aerosol particles". The ratio is assumed to be related to the same wavelength of incident radiation. "Ambient_aerosol" means that the aerosol is measured or modelled at the ambient state of pressure, temperature and relative humidity that exists in its immediate environment. "Ambient aerosol particles" are aerosol particles that have taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the particles. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. @@ -18388,6 +18507,13 @@ The sea_floor_depth_below_sea_surface is the vertical distance between the sea surface and the seabed as measured at a given point in space including the variance caused by tides and possibly waves. + + s + + + "Sea floor sediment" is sediment deposited at the sea bed. "Sediment age" means the length of time elapsed since the sediment was deposited. The phrase "before_1950" is a transparent representation of the phrase "before_present", often used in the geological and archaeological domains to refer to time elapsed between an event and 1950 AD. + + m @@ -19704,6 +19830,13 @@ Speed is the magnitude of velocity. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Due to tides" means due to all astronomical gravity changes which manifest as tides. No distinction is made between different tidal components. + + s-1 + + + Speed is the magnitude of velocity. Sea water speed shear is the derivative of sea water speed with respect to depth. + + K 80 @@ -20355,6 +20488,13 @@ "specific" means per unit mass. Dry energy is the sum of dry static energy and kinetic energy. Dry static energy is the sum of enthalpy and potential energy (itself the sum of gravitational and centripetal potential energy). Enthalpy can be written either as (1) CpT, where Cp is heat capacity at constant pressure, T is absolute temperature, or (2) U+pV, where U is internal energy, p is pressure and V is volume. + + J kg-1 + + + The specific_enthalpy_of_air is the enthalpy of air per unit mass, which can be computed for an air sample as the sum of the enthalpy of the dry air and the enthalpy of the water vapor in that air, divided by the mass of dry air. + + J kg-1 @@ -20404,6 +20544,13 @@ "Specific" means per unit mass. "Turbulent kinetic energy" is the kinetic energy of chaotic fluctuations of the fluid flow. The dissipation of kinetic energy arises in ocean models as a result of the viscosity of sea water. + + m2 s-2 + + + Specific means per unit mass. "Turbulent kinetic energy" is the kinetic energy of all eddy-induced motion that is not resolved on the grid scale of the model. + + m2 s-2 @@ -24594,8 +24741,7 @@ kg m-2 s-1 - Methane emitted from the surface, generated by biomass burning (fires). Positive direction upwards. -The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. The chemical formula for methane is CH4. The mass is the total mass of the molecules. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. the surface of the earth). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. The term "fires" means all biomass fires, whether naturally occurring or ignited by humans. The precise conditions under which fires produce and consume methane can vary between models. + Methane emitted from the surface, generated by biomass burning (fires). Positive direction upwards. The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. The chemical formula for methane is CH4. The mass is the total mass of the molecules. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. "Emission" means emission from a primary source located anywhere within the atmosphere, including at the lower boundary (i.e. the surface of the earth). "Emission" is a process entirely distinct from "re-emission" which is used in some standard names. The term "fires" means all biomass fires, whether naturally occurring or ignited by humans. The precise conditions under which fires produce and consume methane can vary between models. @@ -30335,7 +30481,7 @@ The surface called "surface" means the lower boundary of the atmospher W m-2 - The phrase "tendency_of_X" means derivative of X with respect to time. The phrase "expressed_as_heat_content" means that this quantity is calculated as the specific heat capacity times density of sea water multiplied by the conservative temperature of the sea water in the grid cell and integrated over depth. If used for a layer heat content, coordinate bounds should be used to define the extent of the layers. If no coordinate bounds are specified, it is assumed that the integral is calculated over the entire vertical extent of the medium, e.g, if the medium is sea water the integral is assumed to be calculated over the full depth of the ocean. Conservative Temperature is defined as part of the Thermodynamic Equation of Seawater 2010 (TEOS-10) which was adopted in 2010 by the International Oceanographic Commission (IOC). Conservative Temperature is specific potential enthalpy (which has the standard name sea_water_specific_potential_enthalpy) divided by a fixed value of the specific heat capacity of sea water, namely cp_0 = 3991.86795711963 J kg-1 K-1. Conservative Temperature is a more accurate measure of the "heat content" of sea water, by a factor of one hundred, than is potential temperature. Because of this, it can be regarded as being proportional to the heat content of sea water per unit mass. Reference: www.teos-10.org; McDougall, 2003 doi: 10.1175/1520-0485(2003)033<0945:PEACOV>2.0.CO;2. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. Additionally, when the parameterized advective process is represented in the model as a skew-diffusion rather than an advection, then the parameterized skew diffusion should be included in this diagnostic. The convergence of a skew-flux is identical (in the continuous formulation) to the convergence of an advective flux, making their tendencies the same. + The phrase "tendency_of_X" means derivative of X with respect to time. The phrase "expressed_as_heat_content" means that this quantity is calculated as the specific heat capacity times density of sea water multiplied by the conservative temperature of the sea water in the grid cell and integrated over depth. If used for a layer heat content, coordinate bounds should be used to define the extent of the layers. If no coordinate bounds are specified, it is assumed that the integral is calculated over the entire vertical extent of the medium, e.g, if the medium is sea water the integral is assumed to be calculated over the full depth of the ocean. Conservative Temperature is defined as part of the Thermodynamic Equation of Seawater 2010 (TEOS-10) which was adopted in 2010 by the International Oceanographic Commission (IOC). Conservative Temperature is specific potential enthalpy (which has the standard name sea_water_specific_potential_enthalpy) divided by a fixed value of the specific heat capacity of sea water, namely cp_0 = 3991.86795711963 J kg-1 K-1. Conservative Temperature is a more accurate measure of the "heat content" of sea water, by a factor of one hundred, than is potential temperature. Because of this, it can be regarded as being proportional to the heat content of sea water per unit mass. Reference: www.teos-10.org; McDougall, 2003 doi: 10.1175/1520-0485(2003)033<0945:PEACOV>2.0.CO;2. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. Additionally, when the parameterized advective process is represented in the model as a skew-diffusion rather than an advection, then the parameterized skew diffusion should be included in this diagnostic. The convergence of a skew-flux is identical (in the continuous formulation) to the convergence of an advective flux, making their tendencies the same. @@ -30384,7 +30530,7 @@ The surface called "surface" means the lower boundary of the atmospher W m-2 - The phrase "tendency_of_X" means derivative of X with respect to time. The phrase "expressed_as_heat_content" means that this quantity is calculated as the specific heat capacity times density of sea water multiplied by the potential temperature of the sea water in the grid cell and integrated over depth. If used for a layer heat content, coordinate bounds should be used to define the extent of the layers. If no coordinate bounds are specified, it is assumed that the integral is calculated over the entire vertical extent of the medium, e.g, if the medium is sea water the integral is assumed to be calculated over the full depth of the ocean. Potential temperature is the temperature a parcel of air or sea water would have if moved adiabatically to sea level pressure. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. Additionally, when the parameterized advective process is represented in the model as a skew-diffusion rather than an advection, then the parameterized skew diffusion should be included in this diagnostic. The convergence of a skew-flux is identical (in the continuous formulation) to the convergence of an advective flux, making their tendencies the same. + The phrase "tendency_of_X" means derivative of X with respect to time. The phrase "expressed_as_heat_content" means that this quantity is calculated as the specific heat capacity times density of sea water multiplied by the potential temperature of the sea water in the grid cell and integrated over depth. If used for a layer heat content, coordinate bounds should be used to define the extent of the layers. If no coordinate bounds are specified, it is assumed that the integral is calculated over the entire vertical extent of the medium, e.g, if the medium is sea water the integral is assumed to be calculated over the full depth of the ocean. Potential temperature is the temperature a parcel of air or sea water would have if moved adiabatically to sea level pressure. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. Additionally, when the parameterized advective process is represented in the model as a skew-diffusion rather than an advection, then the parameterized skew diffusion should be included in this diagnostic. The convergence of a skew-flux is identical (in the continuous formulation) to the convergence of an advective flux, making their tendencies the same. @@ -30475,7 +30621,7 @@ The surface called "surface" means the lower boundary of the atmospher kg m-2 s-1 - The phrase "tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. Additionally, when the parameterized advective process is represented in the model as a skew-diffusion rather than an advection, then the parameterized skew diffusion should be included in this diagnostic. The convergence of a skew-flux is identical (in the continuous formulation) to the convergence of an advective flux, making their tendencies the same. + The phrase "tendency_of_X" means derivative of X with respect to time. "Content" indicates a quantity per unit area. The specification of a physical process by the phrase due_to_process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized eddy advection in an ocean model means the part due to a scheme representing parameterized eddy-induced advective effects not included in the resolved model velocity field. Parameterized submesoscale eddy advection occurs on a spatial scale of the order of 1 km horizontally. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. There are also standard names for parameterized_mesoscale_eddy_advection which, along with parameterized_submesoscale_eddy_advection, contributes to the total parameterized eddy advection. Additionally, when the parameterized advective process is represented in the model as a skew-diffusion rather than an advection, then the parameterized skew diffusion should be included in this diagnostic. The convergence of a skew-flux is identical (in the continuous formulation) to the convergence of an advective flux, making their tendencies the same. @@ -31388,7 +31534,7 @@ The surface called "surface" means the lower boundary of the atmospher The "Ultraviolet Index" (UVI) is a measure of the amount of solar ultraviolet radiation that reaches the surface of the earth depending on factors such as time of day and cloud cover. It is often used to alert the public of the need to limit sun exposure and use sun creams to protect the skin. Each point on the Index scale is equivalent to 25 mW m-2 of UV radiation (reference: Australian Bureau of Meteorology, http://www.bom.gov.au/uv/about_uv_index.shtml). The UVI range is expressed as a numeric value from 0 to 20 and sometimes graphically as bands of color indicating the attendant risk of skin damage. A UVI of 0-2 is described as 'Low' (represented graphically in green); a UVI of 11 or greater is described as "Extreme" (represented graphically in purple). The higher the UVI, the greater the potential health risk to humans and the less time it takes for harm to occur. A phrase "assuming_condition" indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "Overcast" means a fractional sky cover of 95% or more when at least a portion of this amount is attributable to clouds or obscuring phenomena (such as haze, dust, smoke, fog, etc.) aloft. (Reference: AMS Glossary: http://glossary.ametsoc.org/wiki/Main_Page). Standard names are also defined for the quantities ultraviolet_index and ultraviolet_index_assuming_clear_sky. - + degree_C @@ -31724,13 +31870,6 @@ The surface called "surface" means the lower boundary of the atmospher The vertical_component_of_ocean_xy_tracer_diffusivity means the vertical component of the diffusivity of tracers in the ocean due to lateral mixing. This quantity could appear in formulations of lateral diffusivity in which "lateral" does not mean "iso-level", e.g. it would not be used for isopycnal diffusivity. "Tracer diffusivity" means the diffusivity of heat and salinity due to motion which is not resolved on the grid scale of the model. - - kg m-2 - - - “Drainage” is the process of removal of excess water from soil by gravitational flow. "Amount" means mass per unit area. The vertical drainage amount in soil is the amount of water that drains through the bottom of a soil column extending from the surface to a specified depth. - - m @@ -32298,6 +32437,20 @@ The surface called "surface" means the lower boundary of the atmospher Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity. A gust is a sudden brief period of high wind speed. In an observed timeseries of wind speed, the gust wind speed can be indicated by a cell_methods of maximum for the time-interval. In an atmospheric model which has a parametrised calculation of gustiness, the gust wind speed may be separately diagnosed from the wind speed. + + m s-1 + + + Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity. A gust is a sudden brief period of high wind speed. In an observed timeseries of wind speed, the gust wind speed can be indicated by a cell_methods of maximum for the time-interval. In an atmospheric model which has a parametrised calculation of gustiness, the gust wind speed may be separately diagnosed from the wind speed. The specification of a physical process by the phrase "due_to" process means that the quantity named is a single term in a list of terms, the maximum of which composes the general quantity named by omitting the phrase. + + + + m s-1 + + + Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity. A gust is a sudden brief period of high wind speed. In an observed timeseries of wind speed, the gust wind speed can be indicated by a cell_methods of maximum for the time-interval. In an atmospheric model which has a parametrised calculation of gustiness, the gust wind speed may be separately diagnosed from the wind speed. The specification of a physical process by the phrase "due_to" process means that the quantity named is a single term in a list of terms, the maximum of which composes the general quantity named by omitting the phrase. + + s-1 N136 @@ -32390,2248 +32543,2256 @@ The surface called "surface" means the lower boundary of the atmospher - - moles_of_particulate_inorganic_carbon_per_unit_mass_in_sea_water + + isotropic_longwave_radiance_in_air - - temperature_in_ground + + isotropic_shortwave_radiance_in_air - - biological_taxon_lsid + + water_evapotranspiration_flux - - tendency_of_atmosphere_number_content_of_aerosol_particles_due_to_turbulent_deposition + + drainage_amount_through_base_of_soil_model - - lagrangian_tendency_of_atmosphere_sigma_coordinate + + mole_fraction_of_ozone_in_air - - lagrangian_tendency_of_atmosphere_sigma_coordinate + + product_of_northward_wind_and_specific_humidity - - electrical_mobility_diameter_of_ambient_aerosol_particles + + radiation_wavelength - - diameter_of_ambient_aerosol_particles + + specific_gravitational_potential_energy - - mass_concentration_of_biomass_burning_dry_aerosol_particles_in_air + + surface_drag_coefficient_for_heat_in_air - - effective_radius_of_stratiform_cloud_rain_particles + + surface_drag_coefficient_for_momentum_in_air - - effective_radius_of_stratiform_cloud_ice_particles + + surface_drag_coefficient_in_air - - effective_radius_of_stratiform_cloud_graupel_particles + + water_flux_into_sea_water - - effective_radius_of_convective_cloud_snow_particles + + wind_mixing_energy_flux_into_sea_water - - effective_radius_of_convective_cloud_rain_particles + + mole_fraction_of_chlorine_dioxide_in_air - - effective_radius_of_convective_cloud_ice_particles + + mole_fraction_of_chlorine_monoxide_in_air - - histogram_of_backscattering_ratio_in_air_over_height_above_reference_ellipsoid + + mole_fraction_of_hypochlorous_acid_in_air - - backscattering_ratio_in_air + + surface_net_downward_radiative_flux - - soot_content_of_surface_snow + + surface_temperature - - liquid_water_content_of_surface_snow + + surface_temperature - - surface_snow_thickness + + surface_temperature - - thermal_energy_content_of_surface_snow + + surface_upward_sensible_heat_flux - - temperature_in_surface_snow + + mass_concentration_of_suspended_matter_in_sea_water - - integral_wrt_time_of_surface_downward_eastward_stress + + universal_thermal_comfort_index - - integral_wrt_time_of_surface_downward_northward_stress + + sea_surface_swell_wave_period - - sea_water_velocity_from_direction + + sea_surface_wind_wave_period - - sea_water_velocity_to_direction + + atmosphere_net_upward_convective_mass_flux - - sea_water_velocity_to_direction + + tendency_of_mass_content_of_water_vapor_in_atmosphere_layer_due_to_deep_convection - - integral_wrt_depth_of_product_of_salinity_and_sea_water_density + + tendency_of_mass_content_of_water_vapor_in_atmosphere_layer_due_to_shallow_convection - - integral_wrt_depth_of_product_of_conservative_temperature_and_sea_water_density + + tendency_of_mass_content_of_water_vapor_in_atmosphere_layer_due_to_turbulence - - integral_wrt_depth_of_product_of_potential_temperature_and_sea_water_density + + wave_frequency - - volume_fraction_of_condensed_water_in_soil_at_wilting_point + + northward_eliassen_palm_flux_in_air - - volume_fraction_of_condensed_water_in_soil_at_field_capacity + + northward_heat_flux_in_air_due_to_eddy_advection - - volume_fraction_of_condensed_water_in_soil_at_critical_point + + upward_eliassen_palm_flux_in_air - - volume_fraction_of_condensed_water_in_soil + + upward_eastward_momentum_flux_in_air_due_to_nonorographic_eastward_gravity_waves - - product_of_lagrangian_tendency_of_air_pressure_and_specific_humidity + + upward_eastward_momentum_flux_in_air_due_to_nonorographic_westward_gravity_waves - - product_of_lagrangian_tendency_of_air_pressure_and_specific_humidity + + upward_eastward_momentum_flux_in_air_due_to_orographic_gravity_waves - - product_of_lagrangian_tendency_of_air_pressure_and_geopotential_height + + lwe_thickness_of_atmosphere_mass_content_of_water_vapor - - product_of_lagrangian_tendency_of_air_pressure_and_air_temperature + + mass_content_of_cloud_condensed_water_in_atmosphere_layer - - product_of_lagrangian_tendency_of_air_pressure_and_air_temperature + + mass_content_of_cloud_ice_in_atmosphere_layer - - tendency_of_sea_water_salinity_expressed_as_salt_content_due_to_parameterized_dianeutral_mixing + + mass_content_of_water_in_atmosphere_layer - - tendency_of_sea_water_potential_temperature_expressed_as_heat_content_due_to_parameterized_dianeutral_mixing + + mass_content_of_water_vapor_in_atmosphere_layer - - tendency_of_sea_water_conservative_temperature_expressed_as_heat_content_due_to_parameterized_dianeutral_mixing + + tendency_of_atmosphere_mass_content_of_water_due_to_advection - - rate_of_hydroxyl_radical_destruction_due_to_reaction_with_nmvoc + + tendency_of_atmosphere_mass_content_of_water_vapor - - net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_miscellaneous_phytoplankton + + tendency_of_atmosphere_mass_content_of_water_vapor_due_to_convection - - mole_fraction_of_inorganic_bromine_in_air + + tendency_of_atmosphere_mass_content_of_water_vapor_due_to_deep_convection - - water_vapor_saturation_deficit_in_air + + tendency_of_atmosphere_mass_content_of_water_vapor_due_to_shallow_convection - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_agricultural_waste_burning + + tendency_of_atmosphere_mass_content_of_water_vapor_due_to_turbulence - - tendency_of_atmosphere_moles_of_carbon_tetrachloride + + tendency_of_mass_content_of_water_vapor_in_atmosphere_layer - - tendency_of_atmosphere_moles_of_carbon_monoxide + + tendency_of_mass_content_of_water_vapor_in_atmosphere_layer_due_to_convection - - platform_yaw + + tendency_of_middle_atmosphere_moles_of_carbon_monoxide - - platform_pitch + + tendency_of_middle_atmosphere_moles_of_methane - - platform_roll + + tendency_of_middle_atmosphere_moles_of_methyl_bromide - - net_primary_mole_productivity_of_biomass_expressed_as_carbon_due_to_nitrate_utilization + + tendency_of_middle_atmosphere_moles_of_methyl_chloride - - net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_picophytoplankton + + tendency_of_middle_atmosphere_moles_of_molecular_hydrogen - - net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_phytoplankton + + tendency_of_troposphere_moles_of_carbon_monoxide - - net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_diatoms + + tendency_of_troposphere_moles_of_methane - - net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_calcareous_phytoplankton + + tendency_of_troposphere_moles_of_methyl_bromide - - mole_concentration_of_diatoms_expressed_as_nitrogen_in_sea_water + + tendency_of_troposphere_moles_of_methyl_chloride - - tendency_of_mole_concentration_of_dissolved_inorganic_silicon_in_sea_water_due_to_biological_processes + + tendency_of_troposphere_moles_of_molecular_hydrogen - - tendency_of_mole_concentration_of_dissolved_inorganic_phosphorus_in_sea_water_due_to_biological_processes + + mass_fraction_of_convective_cloud_condensed_water_in_air - - tendency_of_atmosphere_mole_concentration_of_carbon_monoxide_due_to_chemical_destruction + + mass_fraction_of_ozone_in_air - - volume_extinction_coefficient_in_air_due_to_ambient_aerosol_particles + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_due_to_emission - - mole_fraction_of_noy_expressed_as_nitrogen_in_air + + tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_emission - - tendency_of_atmosphere_moles_of_methane + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_residential_and_commercial_combustion - - tendency_of_specific_humidity_due_to_stratiform_precipitation + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_waste_treatment_and_disposal - - tendency_of_air_temperature_due_to_stratiform_precipitation + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_savanna_and_grassland_fires - - stratiform_precipitation_flux + + tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_particles_due_to_emission - - stratiform_precipitation_amount + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_land_transport - - lwe_thickness_of_stratiform_precipitation_amount + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_agricultural_waste_burning - - lwe_stratiform_precipitation_rate + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_energy_production_and_distribution - - water_evaporation_amount_from_canopy + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_maritime_transport - - water_evaporation_flux_from_canopy + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_net_chemical_production_and_emission - - precipitation_flux_onto_canopy + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_net_chemical_production_and_emission - - outgoing_water_volume_transport_along_river_channel + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_forest_fires - - tendency_of_sea_ice_amount_due_to_conversion_of_snow_to_sea_ice + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_industrial_processes_and_combustion - - tendency_of_atmosphere_mass_content_of_mercury_dry_aerosol_particles_due_to_emission + + sea_surface_swell_wave_significant_height - - mass_fraction_of_mercury_dry_aerosol_particles_in_air + + sea_surface_wind_wave_significant_height - - tendency_of_atmosphere_mass_content_of_water_vapor_due_to_sublimation_of_surface_snow_and_ice + + sea_surface_wave_significant_height - - surface_snow_density + + mass_content_of_water_in_soil_layer - - atmosphere_upward_relative_vorticity + + mass_content_of_water_in_soil - - atmosphere_upward_absolute_vorticity + + sea_surface_swell_wave_to_direction - - area_type + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_gravitational_settling - - area_type + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_gravitational_settling - - mass_fraction_of_liquid_precipitation_in_air + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_turbulent_deposition - - mass_fraction_of_liquid_precipitation_in_air + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_turbulent_deposition - - tendency_of_mole_concentration_of_particulate_organic_matter_expressed_as_carbon_in_sea_water_due_to_net_primary_production_by_diazotrophic_phytoplankton + + tendency_of_atmosphere_moles_of_nitric_acid_trihydrate_ambient_aerosol_particles - - nitrogen_growth_limitation_of_diazotrophic_phytoplankton + + eastward_water_vapor_flux_in_air - - net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_diazotrophic_phytoplankton + + kinetic_energy_dissipation_in_atmosphere_boundary_layer - - net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_diazotrophic_phytoplankton + + lwe_stratiform_snowfall_rate - - mole_concentration_of_diazotrophic_phytoplankton_expressed_as_carbon_in_sea_water + + lwe_thickness_of_stratiform_snowfall_amount - - mass_concentration_of_diazotrophic_phytoplankton_expressed_as_chlorophyll_in_sea_water + + northward_water_vapor_flux_in_air - - iron_growth_limitation_of_diazotrophic_phytoplankton + + stratiform_rainfall_amount - - growth_limitation_of_diazotrophic_phytoplankton_due_to_solar_irradiance + + stratiform_rainfall_flux - - air_pseudo_equivalent_potential_temperature + + stratiform_rainfall_rate - - tendency_of_mass_fraction_of_stratiform_cloud_ice_in_air_due_to_melting_to_cloud_liquid_water + + stratiform_snowfall_amount - - tendency_of_mass_fraction_of_stratiform_cloud_ice_in_air_due_to_heterogeneous_nucleation_from_cloud_liquid_water + + stratiform_snowfall_flux - - tendency_of_mass_fraction_of_stratiform_cloud_ice_in_air_due_to_riming_from_cloud_liquid_water + + thickness_of_stratiform_rainfall_amount - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_wet_deposition - + + thickness_of_stratiform_snowfall_amount + - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_wet_deposition + + atmosphere_mass_content_of_cloud_condensed_water - - stratiform_cloud_area_fraction + + atmosphere_mass_content_of_cloud_ice - - surface_upwelling_radiance_per_unit_wavelength_in_air_reflected_by_sea_water + + atmosphere_mass_content_of_convective_cloud_condensed_water - - surface_upwelling_radiance_per_unit_wavelength_in_air_emerging_from_sea_water + + atmosphere_mass_content_of_water_vapor - - surface_upwelling_radiance_per_unit_wavelength_in_air + + surface_downward_mole_flux_of_carbon_dioxide - - surface_upwelling_longwave_flux_in_air + + surface_upward_mole_flux_of_carbon_dioxide - - incoming_water_volume_transport_along_river_channel + + atmosphere_mass_content_of_sulfate - - sea_water_potential_temperature_expressed_as_heat_content + + atmosphere_mass_content_of_sulfate - - sea_water_potential_temperature_expressed_as_heat_content + + change_over_time_in_atmosphere_mass_content_of_water_due_to_advection - - sea_ice_temperature_expressed_as_heat_content + + change_over_time_in_atmosphere_mass_content_of_water_due_to_advection - - sea_ice_temperature_expressed_as_heat_content + + atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles - - surface_downwelling_spherical_irradiance_per_unit_wavelength_in_sea_water + + atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_particles - - surface_downwelling_shortwave_flux_in_air_assuming_clear_sky_and_no_aerosol + + mass_fraction_of_particulate_organic_matter_dry_aerosol_particles_in_air - - surface_downwelling_shortwave_flux_in_air_assuming_clear_sky + + mass_fraction_of_primary_particulate_organic_matter_dry_aerosol_particles_in_air - - surface_downwelling_shortwave_flux_in_air + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_dry_deposition - - surface_downwelling_radiative_flux_per_unit_wavelength_in_sea_water + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_gravitational_settling - - surface_downwelling_radiative_flux_per_unit_wavelength_in_air + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_turbulent_deposition - - surface_downwelling_radiance_per_unit_wavelength_in_sea_water + + tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_wet_deposition - - surface_downwelling_photon_spherical_irradiance_per_unit_wavelength_in_sea_water + + tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_particles_due_to_dry_deposition - - surface_downwelling_photon_radiance_per_unit_wavelength_in_sea_water + + tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_particles_due_to_wet_deposition - - surface_downwelling_photon_flux_per_unit_wavelength_in_sea_water + + atmosphere_absorption_optical_thickness_due_to_ambient_aerosol_particles - - surface_downwelling_longwave_flux_in_air + + angstrom_exponent_of_ambient_aerosol_in_air - - integral_wrt_time_of_surface_downwelling_shortwave_flux_in_air + + atmosphere_absorption_optical_thickness_due_to_dust_ambient_aerosol_particles - - integral_wrt_time_of_surface_downwelling_longwave_flux_in_air + + atmosphere_absorption_optical_thickness_due_to_particulate_organic_matter_ambient_aerosol_particles - - downwelling_spherical_irradiance_per_unit_wavelength_in_sea_water + + atmosphere_absorption_optical_thickness_due_to_sulfate_ambient_aerosol_particles - - downwelling_shortwave_flux_in_air_assuming_clear_sky_and_no_aerosol + + atmosphere_mass_content_of_ammonium_dry_aerosol_particles - - downwelling_radiative_flux_per_unit_wavelength_in_sea_water + + atmosphere_mass_content_of_dust_dry_aerosol_particles - - downwelling_radiative_flux_per_unit_wavelength_in_air + + atmosphere_mass_content_of_mercury_dry_aerosol_particles - - downwelling_radiance_per_unit_wavelength_in_sea_water + + atmosphere_mass_content_of_nitrate_dry_aerosol_particles - - downwelling_radiance_per_unit_wavelength_in_air + + atmosphere_mass_content_of_nitric_acid_trihydrate_ambient_aerosol_particles - - downwelling_photon_spherical_irradiance_per_unit_wavelength_in_sea_water + + atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles - - downwelling_photon_radiance_per_unit_wavelength_in_sea_water + + atmosphere_mass_content_of_sulfate_ambient_aerosol_particles - - downwelling_photon_flux_per_unit_wavelength_in_sea_water + + atmosphere_mass_content_of_sulfate_ambient_aerosol_particles - - surface_upwelling_shortwave_flux_in_air_assuming_clear_sky + + atmosphere_mass_content_of_sulfate_dry_aerosol_particles - - surface_upwelling_longwave_flux_in_air_assuming_clear_sky + + atmosphere_mass_content_of_water_in_ambient_aerosol_particles - - upwelling_shortwave_flux_in_air_assuming_clear_sky_and_no_aerosol + + atmosphere_moles_of_nitric_acid_trihydrate_ambient_aerosol_particles - - upwelling_radiative_flux_per_unit_wavelength_in_sea_water + + atmosphere_optical_thickness_due_to_ambient_aerosol_particles - - upwelling_radiative_flux_per_unit_wavelength_in_air + + atmosphere_optical_thickness_due_to_ambient_aerosol_particles - - upwelling_radiance_per_unit_wavelength_in_air + + atmosphere_optical_thickness_due_to_dust_ambient_aerosol_particles - - surface_upwelling_shortwave_flux_in_air_assuming_clear_sky_and_no_aerosol + + atmosphere_optical_thickness_due_to_dust_dry_aerosol_particles - - surface_upwelling_shortwave_flux_in_air + + atmosphere_optical_thickness_due_to_particulate_organic_matter_ambient_aerosol_particles - - surface_upwelling_radiative_flux_per_unit_wavelength_in_sea_water + + mass_concentration_of_dust_dry_aerosol_particles_in_air - - surface_upwelling_radiative_flux_per_unit_wavelength_in_air + + mass_concentration_of_coarse_mode_ambient_aerosol_particles_in_air - - surface_upwelling_radiance_per_unit_wavelength_in_sea_water + + mass_concentration_of_ammonium_dry_aerosol_particles_in_air - - platform_name + + atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur - - water_vapor_partial_pressure_in_air + + atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur - - effective_radius_of_stratiform_cloud_snow_particles + + mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_particles_in_air - - tendency_of_atmosphere_moles_of_cfc11 + + mass_concentration_of_particulate_organic_matter_dry_aerosol_particles_in_air - - moles_of_cfc11_per_unit_mass_in_sea_water + + atmosphere_optical_thickness_due_to_water_in_ambient_aerosol_particles - - atmosphere_moles_of_cfc11 + + mass_concentration_of_mercury_dry_aerosol_particles_in_air - - tendency_of_atmosphere_moles_of_cfc113 + + mass_concentration_of_nitrate_dry_aerosol_particles_in_air - - atmosphere_moles_of_cfc113 + + mass_concentration_of_nitric_acid_trihydrate_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_moles_of_cfc114 + + mass_concentration_of_secondary_particulate_organic_matter_dry_aerosol_particles_in_air - - atmosphere_moles_of_cfc114 + + mass_concentration_of_sulfate_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_moles_of_cfc115 + + mass_concentration_of_sulfate_ambient_aerosol_particles_in_air - - atmosphere_moles_of_cfc115 + + mass_concentration_of_sulfate_dry_aerosol_particles_in_air - - tendency_of_atmosphere_moles_of_cfc12 + + mass_concentration_of_water_in_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_moles_of_halon2402 + + mass_fraction_of_ammonium_dry_aerosol_particles_in_air - - atmosphere_moles_of_halon2402 + + mass_fraction_of_dust_dry_aerosol_particles_in_air - - tendency_of_atmosphere_moles_of_hcc140a + + mass_fraction_of_nitrate_dry_aerosol_particles_in_air - - atmosphere_moles_of_hcc140a + + mass_fraction_of_nitric_acid_trihydrate_ambient_aerosol_particles_in_air - - tendency_of_troposphere_moles_of_hcc140a + + mass_fraction_of_secondary_particulate_organic_matter_dry_aerosol_particles_in_air - - tendency_of_middle_atmosphere_moles_of_hcc140a + + mass_fraction_of_sulfate_dry_aerosol_particles_in_air - - tendency_of_troposphere_moles_of_hcfc22 + + mass_fraction_of_water_in_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_moles_of_hcfc22 + + mole_concentration_of_nitric_acid_trihydrate_ambient_aerosol_particles_in_air - - atmosphere_moles_of_hcfc22 + + mole_fraction_of_nitric_acid_trihydrate_ambient_aerosol_particles_in_air - - product_of_northward_wind_and_lagrangian_tendency_of_air_pressure + + number_concentration_of_ambient_aerosol_particles_in_air - - product_of_eastward_wind_and_lagrangian_tendency_of_air_pressure + + number_concentration_of_coarse_mode_ambient_aerosol_particles_in_air - - carbon_mass_flux_into_litter_and_soil_due_to_anthropogenic_land_use_or_land_cover_change + + number_concentration_of_nucleation_mode_ambient_aerosol_particles_in_air - - floating_ice_shelf_area_fraction + + optical_thickness_of_atmosphere_layer_due_to_ambient_aerosol_particles - - atmosphere_moles_of_carbon_tetrachloride + + optical_thickness_of_atmosphere_layer_due_to_ambient_aerosol_particles - - mole_fraction_of_methylglyoxal_in_air + + tendency_of_atmosphere_mass_content_of_ammonium_dry_aerosol_particles_due_to_dry_deposition - - mole_fraction_of_dichlorine_peroxide_in_air + + tendency_of_atmosphere_mass_content_of_ammonium_dry_aerosol_particles_due_to_wet_deposition - - volume_scattering_coefficient_of_radiative_flux_in_air_due_to_ambient_aerosol_particles + + tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_dry_deposition - - volume_scattering_coefficient_of_radiative_flux_in_air_due_to_dried_aerosol_particles + + tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_gravitational_settling - - soil_mass_content_of_carbon + + tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_turbulent_deposition - - slow_soil_pool_mass_content_of_carbon + + tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_wet_deposition - - root_mass_content_of_carbon + + tendency_of_atmosphere_mass_content_of_mercury_dry_aerosol_particles_due_to_dry_deposition - - miscellaneous_living_matter_mass_content_of_carbon + + tendency_of_atmosphere_mass_content_of_mercury_dry_aerosol_particles_due_to_wet_deposition - - fast_soil_pool_mass_content_of_carbon + + tendency_of_atmosphere_mass_content_of_nitrate_dry_aerosol_particles_due_to_dry_deposition - - medium_soil_pool_mass_content_of_carbon + + tendency_of_atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles_due_to_dry_deposition - - leaf_mass_content_of_carbon + + tendency_of_atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles_due_to_net_chemical_production - - carbon_mass_content_of_forestry_and_agricultural_products + + tendency_of_atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles_due_to_net_chemical_production - - carbon_mass_content_of_forestry_and_agricultural_products + + tendency_of_atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles_due_to_wet_deposition - - surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_plant_respiration_for_biomass_maintenance + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_due_to_dry_deposition - - surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_plant_respiration_for_biomass_growth + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_dry_deposition - - surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_plant_respiration + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_dry_deposition - - surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_respiration_in_soil + + x_wind - - surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_heterotrophic_respiration + + y_wind - - eastward_transformed_eulerian_mean_air_velocity + + land_ice_surface_specific_mass_balance_rate - - surface_litter_mass_content_of_carbon + + land_ice_lwe_surface_specific_mass_balance_rate - - litter_mass_content_of_carbon + + isotropic_radiance_per_unit_wavelength_in_air - - tendency_of_atmosphere_mass_content_of_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition + + isotropic_radiance_per_unit_wavelength_in_air - - mole_concentration_of_phytoplankton_expressed_as_nitrogen_in_sea_water + + omnidirectional_spherical_irradiance_per_unit_wavelength_in_sea_water - - atmosphere_mass_content_of_convective_cloud_liquid_water + + mass_concentration_of_chlorophyll_in_sea_water - - effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top + + mass_concentration_of_chlorophyll_in_sea_water - - air_equivalent_temperature + + tendency_of_atmosphere_moles_of_sulfate_dry_aerosol_particles - - air_pseudo_equivalent_temperature + + tendency_of_atmosphere_moles_of_methyl_bromide - - mass_content_of_cloud_liquid_water_in_atmosphere_layer + + tendency_of_atmosphere_moles_of_methyl_chloride - - air_equivalent_potential_temperature + + tendency_of_atmosphere_moles_of_molecular_hydrogen - - number_concentration_of_stratiform_cloud_liquid_water_particles_at_stratiform_liquid_water_cloud_top + + tendency_of_atmosphere_moles_of_nitrous_oxide - - number_concentration_of_convective_cloud_liquid_water_particles_at_convective_liquid_water_cloud_top + + tendency_of_atmosphere_mass_content_of_water_vapor_due_to_advection - - effective_radius_of_stratiform_cloud_liquid_water_particles_at_stratiform_liquid_water_cloud_top + + atmosphere_moles_of_carbon_monoxide - - effective_radius_of_stratiform_cloud_liquid_water_particles + + sea_surface_wind_wave_to_direction - - effective_radius_of_convective_cloud_liquid_water_particles_at_convective_liquid_water_cloud_top + + sea_surface_wave_mean_period - - effective_radius_of_convective_cloud_liquid_water_particles + + equivalent_thickness_at_stp_of_atmosphere_ozone_content - - effective_radius_of_cloud_liquid_water_particles + + atmosphere_moles_of_methane - - atmosphere_mass_content_of_cloud_liquid_water + + atmosphere_moles_of_methyl_bromide - - atmosphere_moles_of_cfc12 + + atmosphere_moles_of_methyl_chloride - - tendency_of_atmosphere_moles_of_halon1202 + + atmosphere_moles_of_molecular_hydrogen - - atmosphere_moles_of_halon1202 + + atmosphere_moles_of_nitrous_oxide - - tendency_of_atmosphere_moles_of_halon1211 + + sea_water_x_velocity - - atmosphere_moles_of_halon1211 + + sea_water_y_velocity - - tendency_of_atmosphere_moles_of_halon1301 + + integral_wrt_time_of_air_temperature_deficit - - atmosphere_moles_of_halon1301 + + integral_wrt_time_of_air_temperature_excess - - platform_id + + integral_wrt_time_of_surface_downward_latent_heat_flux - - mass_flux_of_carbon_into_litter_from_vegetation + + integral_wrt_time_of_surface_downward_sensible_heat_flux - - subsurface_litter_mass_content_of_carbon + + atmosphere_convective_available_potential_energy - - stem_mass_content_of_carbon + + atmosphere_convective_available_potential_energy - - mole_concentration_of_dissolved_inorganic_14C_in_sea_water + + gross_primary_productivity_of_biomass_expressed_as_carbon - - surface_downward_mass_flux_of_14C_dioxide_abiotic_analogue_expressed_as_carbon + + net_primary_productivity_of_biomass_expressed_as_carbon - - surface_downward_mass_flux_of_13C_dioxide_abiotic_analogue_expressed_as_13C + + net_primary_productivity_of_biomass_expressed_as_carbon_accumulated_in_leaves - - mole_concentration_of_dissolved_inorganic_13C_in_sea_water + + net_primary_productivity_of_biomass_expressed_as_carbon_accumulated_in_roots - - northward_transformed_eulerian_mean_air_velocity + + net_primary_productivity_of_biomass_expressed_as_carbon_accumulated_in_wood - - surface_water_evaporation_flux + + tendency_of_atmosphere_mass_content_of_pm2p5_sea_salt_dry_aerosol_particles_due_to_dry_deposition - - water_volume_transport_into_sea_water_from_rivers + + tendency_of_atmosphere_mass_content_of_pm2p5_sea_salt_dry_aerosol_particles_due_to_emission - - stratiform_graupel_flux + + sea_surface_wind_wave_mean_period - - wood_debris_mass_content_of_carbon + + sea_surface_swell_wave_mean_period - - toa_outgoing_shortwave_flux_assuming_clear_sky_and_no_aerosol + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_emission - - water_flux_into_sea_water_from_rivers + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_emission - - integral_wrt_height_of_product_of_northward_wind_and_specific_humidity + + sea_surface_height_above_geoid - - integral_wrt_height_of_product_of_eastward_wind_and_specific_humidity + + sea_surface_height_above_geoid - - integral_wrt_depth_of_sea_water_temperature + + sea_floor_depth_below_geoid - - integral_wrt_depth_of_sea_water_temperature + + air_pressure_at_mean_sea_level - - integral_wrt_depth_of_sea_water_temperature + + lagrangian_tendency_of_air_pressure - - integral_wrt_depth_of_sea_water_temperature + + lagrangian_tendency_of_air_pressure - - integral_wrt_depth_of_sea_water_practical_salinity + + mass_concentration_of_elemental_carbon_dry_aerosol_particles_in_air - - magnitude_of_sea_ice_displacement + + atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles - - atmosphere_absorption_optical_thickness_due_to_sea_salt_ambient_aerosol_particles + + mass_fraction_of_elemental_carbon_dry_aerosol_particles_in_air - - atmosphere_absorption_optical_thickness_due_to_sea_salt_ambient_aerosol_particles + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_dry_deposition - - tendency_of_atmosphere_mass_content_of_nitrogen_compounds_expressed_as_nitrogen_due_to_deposition + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission - - tendency_of_atmosphere_mass_content_of_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_energy_production_and_distribution - - surface_geostrophic_eastward_sea_water_velocity + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_forest_fires - - surface_geostrophic_northward_sea_water_velocity + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_industrial_processes_and_combustion - - tendency_of_sea_surface_height_above_mean_sea_level + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_land_transport - - surface_geostrophic_sea_water_y_velocity_assuming_mean_sea_level_for_geoid + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_maritime_transport - - surface_geostrophic_sea_water_x_velocity_assuming_mean_sea_level_for_geoid + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_residential_and_commercial_combustion - - surface_geostrophic_northward_sea_water_velocity_assuming_mean_sea_level_for_geoid + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_savanna_and_grassland_fires - - surface_geostrophic_northward_sea_water_velocity_assuming_mean_sea_level_for_geoid + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_waste_treatment_and_disposal - - surface_geostrophic_eastward_sea_water_velocity_assuming_mean_sea_level_for_geoid + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_gravitational_settling - - surface_geostrophic_eastward_sea_water_velocity_assuming_mean_sea_level_for_geoid + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_turbulent_deposition - - sea_surface_height_above_mean_sea_level + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_wet_deposition - - sea_surface_height_above_mean_sea_level + + tendency_of_mass_concentration_of_elemental_carbon_dry_aerosol_particles_in_air_due_to_emission_from_aviation - - sea_floor_depth_below_mean_sea_level + + integral_wrt_time_of_surface_net_downward_longwave_flux - - mass_fraction_of_pm10_ambient_aerosol_particles_in_air + + integral_wrt_time_of_surface_net_downward_shortwave_flux - - mass_fraction_of_pm10_ambient_aerosol_particles_in_air + + integral_wrt_time_of_toa_net_downward_shortwave_flux - - mass_concentration_of_pm10_ambient_aerosol_particles_in_air + + integral_wrt_time_of_toa_outgoing_longwave_flux - - atmosphere_optical_thickness_due_to_pm10_ambient_aerosol_particles + + northward_ocean_freshwater_transport_due_to_parameterized_eddy_advection - - mass_fraction_of_pm2p5_ambient_aerosol_particles_in_air + + northward_ocean_salt_transport_due_to_parameterized_eddy_advection - - mass_fraction_of_pm2p5_ambient_aerosol_particles_in_air + + ocean_heat_x_transport_due_to_parameterized_eddy_advection - - mass_concentration_of_pm2p5_ambient_aerosol_particles_in_air + + ocean_heat_y_transport_due_to_parameterized_eddy_advection - - atmosphere_optical_thickness_due_to_pm2p5_ambient_aerosol_particles + + ocean_mass_x_transport_due_to_advection_and_parameterized_eddy_advection - - mass_fraction_of_pm1_ambient_aerosol_particles_in_air + + ocean_mass_y_transport_due_to_advection_and_parameterized_eddy_advection - - mass_fraction_of_pm1_ambient_aerosol_particles_in_air + + ocean_meridional_overturning_mass_streamfunction_due_to_parameterized_eddy_advection - - mass_concentration_of_pm1_ambient_aerosol_particles_in_air + + ocean_y_overturning_mass_streamfunction_due_to_parameterized_eddy_advection - - atmosphere_optical_thickness_due_to_pm1_ambient_aerosol_particles + + tendency_of_sea_water_salinity_due_to_parameterized_eddy_advection - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_wet_deposition + + tendency_of_sea_water_temperature_due_to_parameterized_eddy_advection - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_wet_deposition + + northward_sea_water_velocity_due_to_parameterized_mesoscale_eddies - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_turbulent_deposition + + eastward_sea_water_velocity_due_to_parameterized_mesoscale_eddies - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_turbulent_deposition + + sea_water_x_velocity_due_to_parameterized_mesoscale_eddies - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_gravitational_settling + + sea_water_y_velocity_due_to_parameterized_mesoscale_eddies - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_gravitational_settling + + upward_sea_water_velocity_due_to_parameterized_mesoscale_eddies - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_dry_deposition + + ocean_tracer_biharmonic_diffusivity_due_to_parameterized_mesoscale_eddy_advection - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_dry_deposition + + ocean_tracer_laplacian_diffusivity_due_to_parameterized_mesoscale_eddy_advection - - tendency_of_atmosphere_mass_content_of_pm2p5_sea_salt_dry_aerosol_particles_due_to_wet_deposition + + tendency_of_ocean_eddy_kinetic_energy_content_due_to_parameterized_eddy_advection - - tendency_of_atmosphere_mass_content_of_pm10_sea_salt_dry_aerosol_particles_due_to_wet_deposition + + mole_concentration_of_mesozooplankton_expressed_as_nitrogen_in_sea_water - - tendency_of_atmosphere_mass_content_of_pm10_sea_salt_dry_aerosol_particles_due_to_emission + + mole_concentration_of_microzooplankton_expressed_as_nitrogen_in_sea_water - - tendency_of_atmosphere_mass_content_of_pm10_sea_salt_dry_aerosol_particles_due_to_dry_deposition + + mole_concentration_of_organic_detritus_expressed_as_nitrogen_in_sea_water - - mass_fraction_of_sea_salt_dry_aerosol_particles_in_air + + mole_concentration_of_organic_detritus_expressed_as_silicon_in_sea_water - - mass_fraction_of_sea_salt_dry_aerosol_particles_in_air + + northward_ocean_heat_transport_due_to_parameterized_eddy_advection - - mass_concentration_of_sea_salt_dry_aerosol_particles_in_air + + integral_wrt_depth_of_sea_water_practical_salinity - - mass_concentration_of_sea_salt_dry_aerosol_particles_in_air + + integral_wrt_depth_of_sea_water_temperature - - atmosphere_optical_thickness_due_to_sea_salt_ambient_aerosol_particles + + integral_wrt_depth_of_sea_water_temperature - - atmosphere_optical_thickness_due_to_sea_salt_ambient_aerosol_particles + + integral_wrt_depth_of_sea_water_temperature - - atmosphere_mass_content_of_sea_salt_dry_aerosol_particles + + integral_wrt_depth_of_sea_water_temperature - - atmosphere_mass_content_of_sea_salt_dry_aerosol_particles + + integral_wrt_height_of_product_of_eastward_wind_and_specific_humidity - - ocean_mixed_layer_thickness_defined_by_vertical_tracer_diffusivity_deficit + + integral_wrt_height_of_product_of_northward_wind_and_specific_humidity - - northward_ocean_heat_transport_due_to_parameterized_eddy_advection + + water_flux_into_sea_water_from_rivers - - tendency_of_ocean_eddy_kinetic_energy_content_due_to_parameterized_eddy_advection + + toa_outgoing_shortwave_flux_assuming_clear_sky_and_no_aerosol - - ocean_tracer_laplacian_diffusivity_due_to_parameterized_mesoscale_eddy_advection + + wood_debris_mass_content_of_carbon - - ocean_tracer_biharmonic_diffusivity_due_to_parameterized_mesoscale_eddy_advection + + stratiform_graupel_flux - - upward_sea_water_velocity_due_to_parameterized_mesoscale_eddies + + water_volume_transport_into_sea_water_from_rivers - - sea_water_y_velocity_due_to_parameterized_mesoscale_eddies + + surface_water_evaporation_flux - - sea_water_x_velocity_due_to_parameterized_mesoscale_eddies + + northward_transformed_eulerian_mean_air_velocity - - eastward_sea_water_velocity_due_to_parameterized_mesoscale_eddies + + ocean_mixed_layer_thickness_defined_by_vertical_tracer_diffusivity_deficit - - northward_sea_water_velocity_due_to_parameterized_mesoscale_eddies + + atmosphere_mass_content_of_sea_salt_dry_aerosol_particles - - tendency_of_sea_water_temperature_due_to_parameterized_eddy_advection + + atmosphere_mass_content_of_sea_salt_dry_aerosol_particles - - tendency_of_sea_water_salinity_due_to_parameterized_eddy_advection + + atmosphere_optical_thickness_due_to_sea_salt_ambient_aerosol_particles - - ocean_y_overturning_mass_streamfunction_due_to_parameterized_eddy_advection + + atmosphere_optical_thickness_due_to_sea_salt_ambient_aerosol_particles - - ocean_meridional_overturning_mass_streamfunction_due_to_parameterized_eddy_advection + + mass_concentration_of_sea_salt_dry_aerosol_particles_in_air - - ocean_mass_y_transport_due_to_advection_and_parameterized_eddy_advection + + mass_concentration_of_sea_salt_dry_aerosol_particles_in_air - - ocean_mass_x_transport_due_to_advection_and_parameterized_eddy_advection + + mass_fraction_of_sea_salt_dry_aerosol_particles_in_air - - ocean_heat_y_transport_due_to_parameterized_eddy_advection + + mass_fraction_of_sea_salt_dry_aerosol_particles_in_air - - ocean_heat_x_transport_due_to_parameterized_eddy_advection + + tendency_of_atmosphere_mass_content_of_pm10_sea_salt_dry_aerosol_particles_due_to_dry_deposition - - northward_ocean_salt_transport_due_to_parameterized_eddy_advection + + tendency_of_atmosphere_mass_content_of_pm10_sea_salt_dry_aerosol_particles_due_to_emission - - northward_ocean_freshwater_transport_due_to_parameterized_eddy_advection + + tendency_of_atmosphere_mass_content_of_pm10_sea_salt_dry_aerosol_particles_due_to_wet_deposition - - integral_wrt_time_of_toa_outgoing_longwave_flux + + tendency_of_atmosphere_mass_content_of_pm2p5_sea_salt_dry_aerosol_particles_due_to_wet_deposition + + + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_dry_deposition + + + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_dry_deposition - - integral_wrt_time_of_toa_net_downward_shortwave_flux + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_gravitational_settling - - integral_wrt_time_of_surface_net_downward_shortwave_flux + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_gravitational_settling - - integral_wrt_time_of_surface_net_downward_longwave_flux + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_turbulent_deposition - - tendency_of_mass_concentration_of_elemental_carbon_dry_aerosol_particles_in_air_due_to_emission_from_aviation + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_turbulent_deposition - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_wet_deposition + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_wet_deposition - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_turbulent_deposition + + tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_wet_deposition - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_gravitational_settling + + atmosphere_optical_thickness_due_to_pm1_ambient_aerosol_particles - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_waste_treatment_and_disposal + + mass_concentration_of_pm1_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_savanna_and_grassland_fires + + mass_fraction_of_pm1_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_residential_and_commercial_combustion + + mass_fraction_of_pm1_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_maritime_transport + + atmosphere_optical_thickness_due_to_pm2p5_ambient_aerosol_particles - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_land_transport + + mass_concentration_of_pm2p5_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_industrial_processes_and_combustion + + mass_fraction_of_pm2p5_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_forest_fires + + mass_fraction_of_pm2p5_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_energy_production_and_distribution + + atmosphere_optical_thickness_due_to_pm10_ambient_aerosol_particles - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission + + mass_concentration_of_pm10_ambient_aerosol_particles_in_air - - tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_dry_deposition + + mass_fraction_of_pm10_ambient_aerosol_particles_in_air - - mass_fraction_of_elemental_carbon_dry_aerosol_particles_in_air + + mass_fraction_of_pm10_ambient_aerosol_particles_in_air - - atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles + + sea_floor_depth_below_mean_sea_level - - mass_concentration_of_elemental_carbon_dry_aerosol_particles_in_air + + sea_surface_height_above_mean_sea_level - - lagrangian_tendency_of_air_pressure + + sea_surface_height_above_mean_sea_level - - lagrangian_tendency_of_air_pressure + + surface_geostrophic_eastward_sea_water_velocity_assuming_mean_sea_level_for_geoid - - air_pressure_at_mean_sea_level + + surface_geostrophic_eastward_sea_water_velocity_assuming_mean_sea_level_for_geoid - - sea_floor_depth_below_geoid + + surface_geostrophic_northward_sea_water_velocity_assuming_mean_sea_level_for_geoid - - sea_surface_height_above_geoid + + surface_geostrophic_northward_sea_water_velocity_assuming_mean_sea_level_for_geoid - - sea_surface_height_above_geoid + + surface_geostrophic_sea_water_x_velocity_assuming_mean_sea_level_for_geoid - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_emission + + surface_geostrophic_sea_water_y_velocity_assuming_mean_sea_level_for_geoid - - tendency_of_atmosphere_mass_content_of_sea_salt_dry_aerosol_particles_due_to_emission + + tendency_of_sea_surface_height_above_mean_sea_level - - sea_surface_swell_wave_mean_period + + surface_geostrophic_northward_sea_water_velocity - - sea_surface_wind_wave_mean_period + + surface_geostrophic_eastward_sea_water_velocity - - sea_surface_wave_mean_period + + tendency_of_atmosphere_mass_content_of_nitrogen_compounds_expressed_as_nitrogen_due_to_dry_deposition - - sea_surface_wind_wave_to_direction + + tendency_of_atmosphere_mass_content_of_nitrogen_compounds_expressed_as_nitrogen_due_to_deposition - - atmosphere_moles_of_carbon_monoxide + + atmosphere_absorption_optical_thickness_due_to_sea_salt_ambient_aerosol_particles - - tendency_of_atmosphere_mass_content_of_water_vapor_due_to_advection + + atmosphere_absorption_optical_thickness_due_to_sea_salt_ambient_aerosol_particles - - tendency_of_atmosphere_moles_of_nitrous_oxide + + mole_concentration_of_dissolved_inorganic_13C_in_sea_water - - tendency_of_atmosphere_moles_of_molecular_hydrogen + + surface_downward_mass_flux_of_13C_dioxide_abiotic_analogue_expressed_as_13C - - tendency_of_atmosphere_moles_of_methyl_chloride + + surface_downward_mass_flux_of_14C_dioxide_abiotic_analogue_expressed_as_carbon - - tendency_of_atmosphere_moles_of_methyl_bromide + + mole_concentration_of_dissolved_inorganic_14C_in_sea_water - - y_wind + + stem_mass_content_of_carbon - - x_wind + + subsurface_litter_mass_content_of_carbon - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_dry_deposition + + mass_flux_of_carbon_into_litter_from_vegetation - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_dry_deposition + + platform_id - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_due_to_dry_deposition + + atmosphere_moles_of_halon1301 - - tendency_of_atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles_due_to_wet_deposition + + tendency_of_atmosphere_moles_of_halon1301 - - tendency_of_atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles_due_to_net_chemical_production + + atmosphere_moles_of_halon1211 - - tendency_of_atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles_due_to_net_chemical_production + + tendency_of_atmosphere_moles_of_halon1211 - - tendency_of_atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles_due_to_dry_deposition + + atmosphere_moles_of_halon1202 - - tendency_of_atmosphere_mass_content_of_nitrate_dry_aerosol_particles_due_to_dry_deposition + + tendency_of_atmosphere_moles_of_halon1202 - - tendency_of_atmosphere_mass_content_of_mercury_dry_aerosol_particles_due_to_wet_deposition + + atmosphere_moles_of_cfc12 - - tendency_of_atmosphere_mass_content_of_mercury_dry_aerosol_particles_due_to_dry_deposition + + atmosphere_mass_content_of_cloud_liquid_water - - tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_wet_deposition + + effective_radius_of_cloud_liquid_water_particles - - tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_turbulent_deposition + + effective_radius_of_convective_cloud_liquid_water_particles - - tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_gravitational_settling + + effective_radius_of_convective_cloud_liquid_water_particles_at_convective_liquid_water_cloud_top - - tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_dry_deposition + + effective_radius_of_stratiform_cloud_liquid_water_particles - - tendency_of_atmosphere_mass_content_of_ammonium_dry_aerosol_particles_due_to_wet_deposition + + effective_radius_of_stratiform_cloud_liquid_water_particles_at_stratiform_liquid_water_cloud_top - - tendency_of_atmosphere_mass_content_of_ammonium_dry_aerosol_particles_due_to_dry_deposition + + magnitude_of_sea_ice_displacement - - optical_thickness_of_atmosphere_layer_due_to_ambient_aerosol_particles + + number_concentration_of_convective_cloud_liquid_water_particles_at_convective_liquid_water_cloud_top - - optical_thickness_of_atmosphere_layer_due_to_ambient_aerosol_particles + + number_concentration_of_stratiform_cloud_liquid_water_particles_at_stratiform_liquid_water_cloud_top - - number_concentration_of_nucleation_mode_ambient_aerosol_particles_in_air + + air_equivalent_potential_temperature - - number_concentration_of_coarse_mode_ambient_aerosol_particles_in_air + + mass_content_of_cloud_liquid_water_in_atmosphere_layer - - number_concentration_of_ambient_aerosol_particles_in_air + + air_pseudo_equivalent_temperature - - mole_fraction_of_nitric_acid_trihydrate_ambient_aerosol_particles_in_air + + air_equivalent_temperature - - mole_concentration_of_nitric_acid_trihydrate_ambient_aerosol_particles_in_air + + effective_radius_of_cloud_liquid_water_particles_at_liquid_water_cloud_top - - mass_fraction_of_water_in_ambient_aerosol_particles_in_air + + atmosphere_mass_content_of_convective_cloud_liquid_water - - mass_fraction_of_sulfate_dry_aerosol_particles_in_air + + mole_concentration_of_phytoplankton_expressed_as_nitrogen_in_sea_water - - mass_fraction_of_secondary_particulate_organic_matter_dry_aerosol_particles_in_air + + tendency_of_mass_fraction_of_stratiform_cloud_ice_in_air_due_to_riming_from_cloud_liquid_water - - mass_fraction_of_nitric_acid_trihydrate_ambient_aerosol_particles_in_air + + tendency_of_mass_fraction_of_stratiform_cloud_ice_in_air_due_to_heterogeneous_nucleation_from_cloud_liquid_water - - mass_fraction_of_nitrate_dry_aerosol_particles_in_air + + tendency_of_mass_fraction_of_stratiform_cloud_ice_in_air_due_to_melting_to_cloud_liquid_water - - mass_fraction_of_dust_dry_aerosol_particles_in_air + + air_pseudo_equivalent_potential_temperature - - mass_fraction_of_ammonium_dry_aerosol_particles_in_air + + growth_limitation_of_diazotrophic_phytoplankton_due_to_solar_irradiance - - mass_concentration_of_water_in_ambient_aerosol_particles_in_air + + iron_growth_limitation_of_diazotrophic_phytoplankton - - mass_concentration_of_sulfate_dry_aerosol_particles_in_air + + mass_concentration_of_diazotrophic_phytoplankton_expressed_as_chlorophyll_in_sea_water - - mass_concentration_of_sulfate_ambient_aerosol_particles_in_air + + mole_concentration_of_diazotrophic_phytoplankton_expressed_as_carbon_in_sea_water - - mass_concentration_of_sulfate_ambient_aerosol_particles_in_air + + net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_diazotrophic_phytoplankton - - mass_concentration_of_secondary_particulate_organic_matter_dry_aerosol_particles_in_air + + net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_diazotrophic_phytoplankton - - mass_concentration_of_nitric_acid_trihydrate_ambient_aerosol_particles_in_air + + nitrogen_growth_limitation_of_diazotrophic_phytoplankton - - mass_concentration_of_nitrate_dry_aerosol_particles_in_air + + tendency_of_mole_concentration_of_particulate_organic_matter_expressed_as_carbon_in_sea_water_due_to_net_primary_production_by_diazotrophic_phytoplankton - - mass_concentration_of_mercury_dry_aerosol_particles_in_air + + mass_fraction_of_liquid_precipitation_in_air - - atmosphere_optical_thickness_due_to_water_in_ambient_aerosol_particles + + mass_fraction_of_liquid_precipitation_in_air - - mass_concentration_of_particulate_organic_matter_dry_aerosol_particles_in_air + + area_type - - mass_concentration_of_primary_particulate_organic_matter_dry_aerosol_particles_in_air + + area_type - - atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur + + atmosphere_upward_absolute_vorticity - - atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur + + atmosphere_upward_relative_vorticity - - mass_concentration_of_ammonium_dry_aerosol_particles_in_air + + surface_snow_density - - mass_concentration_of_coarse_mode_ambient_aerosol_particles_in_air + + tendency_of_atmosphere_mass_content_of_water_vapor_due_to_sublimation_of_surface_snow_and_ice - - mass_concentration_of_dust_dry_aerosol_particles_in_air + + mass_fraction_of_mercury_dry_aerosol_particles_in_air - - atmosphere_optical_thickness_due_to_particulate_organic_matter_ambient_aerosol_particles + + tendency_of_atmosphere_mass_content_of_mercury_dry_aerosol_particles_due_to_emission - - atmosphere_optical_thickness_due_to_dust_dry_aerosol_particles + + tendency_of_sea_ice_amount_due_to_conversion_of_snow_to_sea_ice - - atmosphere_optical_thickness_due_to_dust_ambient_aerosol_particles + + outgoing_water_volume_transport_along_river_channel - - atmosphere_optical_thickness_due_to_ambient_aerosol_particles + + precipitation_flux_onto_canopy - - atmosphere_optical_thickness_due_to_ambient_aerosol_particles + + water_evaporation_flux_from_canopy - - atmosphere_moles_of_nitric_acid_trihydrate_ambient_aerosol_particles + + water_evaporation_amount_from_canopy - - atmosphere_mass_content_of_water_in_ambient_aerosol_particles + + lwe_stratiform_precipitation_rate - - atmosphere_mass_content_of_sulfate_dry_aerosol_particles + + lwe_thickness_of_stratiform_precipitation_amount - - atmosphere_mass_content_of_sulfate_ambient_aerosol_particles + + stratiform_precipitation_amount - - atmosphere_mass_content_of_sulfate_ambient_aerosol_particles + + stratiform_precipitation_flux - - atmosphere_mass_content_of_secondary_particulate_organic_matter_dry_aerosol_particles + + tendency_of_air_temperature_due_to_stratiform_precipitation - - atmosphere_mass_content_of_nitric_acid_trihydrate_ambient_aerosol_particles + + tendency_of_specific_humidity_due_to_stratiform_precipitation - - atmosphere_mass_content_of_nitrate_dry_aerosol_particles + + tendency_of_atmosphere_moles_of_methane - - atmosphere_mass_content_of_mercury_dry_aerosol_particles + + mole_fraction_of_noy_expressed_as_nitrogen_in_air - - atmosphere_mass_content_of_dust_dry_aerosol_particles + + volume_extinction_coefficient_in_air_due_to_ambient_aerosol_particles - - atmosphere_mass_content_of_ammonium_dry_aerosol_particles + + tendency_of_atmosphere_mole_concentration_of_carbon_monoxide_due_to_chemical_destruction - - atmosphere_absorption_optical_thickness_due_to_sulfate_ambient_aerosol_particles + + tendency_of_mole_concentration_of_dissolved_inorganic_phosphorus_in_sea_water_due_to_biological_processes - - atmosphere_absorption_optical_thickness_due_to_particulate_organic_matter_ambient_aerosol_particles + + tendency_of_mole_concentration_of_dissolved_inorganic_silicon_in_sea_water_due_to_biological_processes - - atmosphere_absorption_optical_thickness_due_to_dust_ambient_aerosol_particles + + net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_diatoms - - angstrom_exponent_of_ambient_aerosol_in_air + + net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_phytoplankton - - atmosphere_absorption_optical_thickness_due_to_ambient_aerosol_particles + + net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_picophytoplankton - - tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_particles_due_to_wet_deposition + + net_primary_mole_productivity_of_biomass_expressed_as_carbon_due_to_nitrate_utilization - - tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_particles_due_to_dry_deposition + + platform_roll - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_wet_deposition + + platform_pitch - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_turbulent_deposition + + platform_yaw - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_gravitational_settling + + tendency_of_atmosphere_moles_of_carbon_monoxide - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_dry_deposition + + tendency_of_atmosphere_moles_of_carbon_tetrachloride - - mass_fraction_of_primary_particulate_organic_matter_dry_aerosol_particles_in_air + + tendency_of_atmosphere_mass_content_of_elemental_carbon_dry_aerosol_particles_due_to_emission_from_agricultural_waste_burning - - mass_fraction_of_particulate_organic_matter_dry_aerosol_particles_in_air + + water_vapor_saturation_deficit_in_air - - atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_particles + + mole_fraction_of_inorganic_bromine_in_air - - atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles + + net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_miscellaneous_phytoplankton - - tendency_of_atmosphere_mass_content_of_pm2p5_sea_salt_dry_aerosol_particles_due_to_emission + + rate_of_hydroxyl_radical_destruction_due_to_reaction_with_nmvoc - - tendency_of_atmosphere_mass_content_of_pm2p5_sea_salt_dry_aerosol_particles_due_to_dry_deposition + + tendency_of_sea_water_conservative_temperature_expressed_as_heat_content_due_to_parameterized_dianeutral_mixing - - net_primary_productivity_of_biomass_expressed_as_carbon_accumulated_in_wood + + tendency_of_sea_water_potential_temperature_expressed_as_heat_content_due_to_parameterized_dianeutral_mixing - - net_primary_productivity_of_biomass_expressed_as_carbon_accumulated_in_roots + + tendency_of_atmosphere_mass_content_of_nitrogen_compounds_expressed_as_nitrogen_due_to_wet_deposition - - net_primary_productivity_of_biomass_expressed_as_carbon_accumulated_in_leaves + + eastward_transformed_eulerian_mean_air_velocity - - net_primary_productivity_of_biomass_expressed_as_carbon + + surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_heterotrophic_respiration - - gross_primary_productivity_of_biomass_expressed_as_carbon + + surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_respiration_in_soil - - atmosphere_convective_available_potential_energy + + surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_plant_respiration - - atmosphere_convective_available_potential_energy + + surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_plant_respiration_for_biomass_growth - - integral_wrt_time_of_surface_downward_sensible_heat_flux + + surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_plant_respiration_for_biomass_maintenance - - integral_wrt_time_of_surface_downward_latent_heat_flux + + carbon_mass_content_of_forestry_and_agricultural_products - - integral_wrt_time_of_air_temperature_excess + + carbon_mass_content_of_forestry_and_agricultural_products - - integral_wrt_time_of_air_temperature_deficit + + leaf_mass_content_of_carbon - - sea_water_y_velocity + + medium_soil_pool_mass_content_of_carbon - - sea_water_x_velocity + + fast_soil_pool_mass_content_of_carbon - - mole_concentration_of_organic_detritus_expressed_as_silicon_in_sea_water + + miscellaneous_living_matter_mass_content_of_carbon - - mole_concentration_of_organic_detritus_expressed_as_nitrogen_in_sea_water + + root_mass_content_of_carbon - - mole_concentration_of_microzooplankton_expressed_as_nitrogen_in_sea_water + + slow_soil_pool_mass_content_of_carbon - - mole_concentration_of_mesozooplankton_expressed_as_nitrogen_in_sea_water + + soil_mass_content_of_carbon - - atmosphere_moles_of_nitrous_oxide + + volume_scattering_coefficient_of_radiative_flux_in_air_due_to_dried_aerosol_particles - - atmosphere_moles_of_molecular_hydrogen + + volume_scattering_coefficient_of_radiative_flux_in_air_due_to_ambient_aerosol_particles - - atmosphere_moles_of_methyl_chloride + + mole_fraction_of_dichlorine_peroxide_in_air - - atmosphere_moles_of_methyl_bromide + + mole_fraction_of_methylglyoxal_in_air - - atmosphere_moles_of_methane + + atmosphere_moles_of_carbon_tetrachloride - - equivalent_thickness_at_stp_of_atmosphere_ozone_content + + floating_ice_shelf_area_fraction - - tendency_of_atmosphere_moles_of_nitric_acid_trihydrate_ambient_aerosol_particles + + carbon_mass_flux_into_litter_and_soil_due_to_anthropogenic_land_use_or_land_cover_change - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_turbulent_deposition + + product_of_eastward_wind_and_lagrangian_tendency_of_air_pressure - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_turbulent_deposition + + product_of_northward_wind_and_lagrangian_tendency_of_air_pressure - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_gravitational_settling + + atmosphere_moles_of_hcfc22 - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_gravitational_settling + + tendency_of_atmosphere_moles_of_hcfc22 - - sea_surface_swell_wave_to_direction + + tendency_of_troposphere_moles_of_hcfc22 - - mass_content_of_water_in_soil + + tendency_of_middle_atmosphere_moles_of_hcc140a - - mass_content_of_water_in_soil_layer + + tendency_of_troposphere_moles_of_hcc140a - - sea_surface_wave_significant_height + + atmosphere_moles_of_hcc140a - - sea_surface_wind_wave_significant_height + + tendency_of_atmosphere_moles_of_hcc140a - - sea_surface_swell_wave_significant_height + + atmosphere_moles_of_halon2402 - - tendency_of_atmosphere_moles_of_sulfate_dry_aerosol_particles + + upwelling_shortwave_flux_in_air_assuming_clear_sky_and_no_aerosol - - mass_concentration_of_chlorophyll_in_sea_water + + surface_upwelling_longwave_flux_in_air_assuming_clear_sky - - mass_concentration_of_chlorophyll_in_sea_water + + surface_upwelling_shortwave_flux_in_air_assuming_clear_sky - - omnidirectional_spherical_irradiance_per_unit_wavelength_in_sea_water + + downwelling_photon_flux_per_unit_wavelength_in_sea_water - - isotropic_radiance_per_unit_wavelength_in_air + + downwelling_photon_radiance_per_unit_wavelength_in_sea_water - - isotropic_radiance_per_unit_wavelength_in_air + + downwelling_photon_spherical_irradiance_per_unit_wavelength_in_sea_water - - land_ice_lwe_surface_specific_mass_balance_rate + + downwelling_radiance_per_unit_wavelength_in_air - - land_ice_surface_specific_mass_balance_rate + + downwelling_radiance_per_unit_wavelength_in_sea_water - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_industrial_processes_and_combustion + + downwelling_radiative_flux_per_unit_wavelength_in_air - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_forest_fires + + downwelling_radiative_flux_per_unit_wavelength_in_sea_water - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_net_chemical_production_and_emission + + downwelling_shortwave_flux_in_air_assuming_clear_sky_and_no_aerosol - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_due_to_net_chemical_production_and_emission + + downwelling_spherical_irradiance_per_unit_wavelength_in_sea_water - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_maritime_transport + + integral_wrt_time_of_surface_downwelling_longwave_flux_in_air - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_energy_production_and_distribution + + integral_wrt_time_of_surface_downwelling_shortwave_flux_in_air - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_agricultural_waste_burning + + surface_downwelling_longwave_flux_in_air - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_land_transport + + surface_downwelling_photon_flux_per_unit_wavelength_in_sea_water - - tendency_of_atmosphere_mass_content_of_primary_particulate_organic_matter_dry_aerosol_particles_due_to_emission + + surface_downwelling_photon_radiance_per_unit_wavelength_in_sea_water - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_savanna_and_grassland_fires + + surface_downwelling_photon_spherical_irradiance_per_unit_wavelength_in_sea_water - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_waste_treatment_and_disposal + + surface_downwelling_radiance_per_unit_wavelength_in_sea_water - - tendency_of_atmosphere_mass_content_of_particulate_organic_matter_dry_aerosol_particles_expressed_as_carbon_due_to_emission_from_residential_and_commercial_combustion + + surface_downwelling_radiative_flux_per_unit_wavelength_in_air - - tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_emission + + surface_downwelling_radiative_flux_per_unit_wavelength_in_sea_water - - tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_due_to_emission + + surface_downwelling_shortwave_flux_in_air - - tendency_of_troposphere_moles_of_molecular_hydrogen + + surface_downwelling_shortwave_flux_in_air_assuming_clear_sky - - tendency_of_troposphere_moles_of_methyl_chloride + + surface_downwelling_shortwave_flux_in_air_assuming_clear_sky_and_no_aerosol - - tendency_of_troposphere_moles_of_methyl_bromide + + surface_downwelling_spherical_irradiance_per_unit_wavelength_in_sea_water - - tendency_of_troposphere_moles_of_methane + + sea_ice_temperature_expressed_as_heat_content - - tendency_of_troposphere_moles_of_carbon_monoxide + + sea_ice_temperature_expressed_as_heat_content - - tendency_of_middle_atmosphere_moles_of_molecular_hydrogen + + sea_water_potential_temperature_expressed_as_heat_content - - tendency_of_middle_atmosphere_moles_of_methyl_chloride + + sea_water_potential_temperature_expressed_as_heat_content - - tendency_of_middle_atmosphere_moles_of_methyl_bromide + + incoming_water_volume_transport_along_river_channel - - tendency_of_middle_atmosphere_moles_of_methane + + surface_upwelling_longwave_flux_in_air - - tendency_of_middle_atmosphere_moles_of_carbon_monoxide + + surface_upwelling_radiance_per_unit_wavelength_in_air - - tendency_of_mass_content_of_water_vapor_in_atmosphere_layer_due_to_convection + + surface_upwelling_radiance_per_unit_wavelength_in_air_emerging_from_sea_water - - tendency_of_mass_content_of_water_vapor_in_atmosphere_layer + + surface_upwelling_radiance_per_unit_wavelength_in_air_reflected_by_sea_water - - tendency_of_atmosphere_mass_content_of_water_vapor_due_to_turbulence + + stratiform_cloud_area_fraction - - tendency_of_atmosphere_mass_content_of_water_vapor_due_to_shallow_convection + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_wet_deposition - - tendency_of_atmosphere_mass_content_of_water_vapor_due_to_deep_convection + + tendency_of_atmosphere_mass_content_of_sulfate_dry_aerosol_particles_expressed_as_sulfur_due_to_wet_deposition - - tendency_of_atmosphere_mass_content_of_water_vapor_due_to_convection + + litter_mass_content_of_carbon - - tendency_of_atmosphere_mass_content_of_water_vapor + + surface_litter_mass_content_of_carbon - - tendency_of_atmosphere_mass_content_of_water_due_to_advection + + tendency_of_sea_water_salinity_expressed_as_salt_content_due_to_parameterized_dianeutral_mixing - - mass_content_of_water_vapor_in_atmosphere_layer + + product_of_lagrangian_tendency_of_air_pressure_and_air_temperature - - mass_content_of_water_in_atmosphere_layer + + product_of_lagrangian_tendency_of_air_pressure_and_air_temperature - - mass_content_of_cloud_ice_in_atmosphere_layer + + product_of_lagrangian_tendency_of_air_pressure_and_geopotential_height - - mass_content_of_cloud_condensed_water_in_atmosphere_layer + + product_of_lagrangian_tendency_of_air_pressure_and_specific_humidity - - lwe_thickness_of_atmosphere_mass_content_of_water_vapor + + product_of_lagrangian_tendency_of_air_pressure_and_specific_humidity - - change_over_time_in_atmosphere_mass_content_of_water_due_to_advection + + volume_fraction_of_condensed_water_in_soil - - change_over_time_in_atmosphere_mass_content_of_water_due_to_advection + + volume_fraction_of_condensed_water_in_soil_at_critical_point - - atmosphere_mass_content_of_sulfate + + volume_fraction_of_condensed_water_in_soil_at_field_capacity - - atmosphere_mass_content_of_sulfate + + volume_fraction_of_condensed_water_in_soil_at_wilting_point - - surface_upward_mole_flux_of_carbon_dioxide + + integral_wrt_depth_of_product_of_potential_temperature_and_sea_water_density - - surface_downward_mole_flux_of_carbon_dioxide + + integral_wrt_depth_of_product_of_conservative_temperature_and_sea_water_density - - atmosphere_mass_content_of_water_vapor + + integral_wrt_depth_of_product_of_salinity_and_sea_water_density - - atmosphere_mass_content_of_convective_cloud_condensed_water + + sea_water_velocity_to_direction - - atmosphere_mass_content_of_cloud_ice + + sea_water_velocity_to_direction - - atmosphere_mass_content_of_cloud_condensed_water + + sea_water_velocity_from_direction - - thickness_of_stratiform_snowfall_amount + + integral_wrt_time_of_surface_downward_northward_stress - - thickness_of_stratiform_rainfall_amount + + integral_wrt_time_of_surface_downward_eastward_stress - - stratiform_snowfall_flux + + temperature_in_surface_snow - - stratiform_snowfall_amount + + thermal_energy_content_of_surface_snow - - stratiform_rainfall_rate + + surface_snow_thickness - - stratiform_rainfall_flux + + liquid_water_content_of_surface_snow - - stratiform_rainfall_amount + + soot_content_of_surface_snow - - northward_water_vapor_flux_in_air + + backscattering_ratio_in_air - - lwe_thickness_of_stratiform_snowfall_amount + + histogram_of_backscattering_ratio_in_air_over_height_above_reference_ellipsoid - - lwe_stratiform_snowfall_rate + + effective_radius_of_convective_cloud_ice_particles - - kinetic_energy_dissipation_in_atmosphere_boundary_layer + + effective_radius_of_convective_cloud_rain_particles - - eastward_water_vapor_flux_in_air + + effective_radius_of_convective_cloud_snow_particles - - upward_eastward_momentum_flux_in_air_due_to_orographic_gravity_waves + + effective_radius_of_stratiform_cloud_graupel_particles - - upward_eastward_momentum_flux_in_air_due_to_nonorographic_westward_gravity_waves + + effective_radius_of_stratiform_cloud_ice_particles - - upward_eastward_momentum_flux_in_air_due_to_nonorographic_eastward_gravity_waves + + effective_radius_of_stratiform_cloud_rain_particles - - upward_eliassen_palm_flux_in_air + + mass_concentration_of_biomass_burning_dry_aerosol_particles_in_air - - northward_heat_flux_in_air_due_to_eddy_advection + + diameter_of_ambient_aerosol_particles - - northward_eliassen_palm_flux_in_air + + electrical_mobility_diameter_of_ambient_aerosol_particles - - wave_frequency + + lagrangian_tendency_of_atmosphere_sigma_coordinate - - tendency_of_mass_content_of_water_vapor_in_atmosphere_layer_due_to_turbulence + + lagrangian_tendency_of_atmosphere_sigma_coordinate - - tendency_of_mass_content_of_water_vapor_in_atmosphere_layer_due_to_shallow_convection + + tendency_of_atmosphere_number_content_of_aerosol_particles_due_to_turbulent_deposition - - tendency_of_mass_content_of_water_vapor_in_atmosphere_layer_due_to_deep_convection + + biological_taxon_lsid - - atmosphere_net_upward_convective_mass_flux + + temperature_in_ground - - mass_fraction_of_ozone_in_air + + tendency_of_atmosphere_moles_of_halon2402 - - mass_fraction_of_convective_cloud_condensed_water_in_air + + tendency_of_atmosphere_moles_of_cfc12 - - sea_surface_wind_wave_period + + atmosphere_moles_of_cfc115 - - sea_surface_swell_wave_period + + tendency_of_atmosphere_moles_of_cfc115 - - mass_concentration_of_suspended_matter_in_sea_water + + atmosphere_moles_of_cfc114 - - surface_upward_sensible_heat_flux + + tendency_of_atmosphere_moles_of_cfc114 - - surface_temperature + + atmosphere_moles_of_cfc113 - - surface_temperature + + tendency_of_atmosphere_moles_of_cfc113 - - surface_temperature + + atmosphere_moles_of_cfc11 - - surface_net_downward_radiative_flux + + moles_of_cfc11_per_unit_mass_in_sea_water - - mole_fraction_of_hypochlorous_acid_in_air + + tendency_of_atmosphere_moles_of_cfc11 - - mole_fraction_of_chlorine_monoxide_in_air + + effective_radius_of_stratiform_cloud_snow_particles - - mole_fraction_of_chlorine_dioxide_in_air + + water_vapor_partial_pressure_in_air - - wind_mixing_energy_flux_into_sea_water + + platform_name - - water_flux_into_sea_water + + surface_upwelling_radiance_per_unit_wavelength_in_sea_water - - surface_drag_coefficient_in_air + + surface_upwelling_radiative_flux_per_unit_wavelength_in_air - - surface_drag_coefficient_for_momentum_in_air + + surface_upwelling_radiative_flux_per_unit_wavelength_in_sea_water - - surface_drag_coefficient_for_heat_in_air + + surface_upwelling_shortwave_flux_in_air - - specific_gravitational_potential_energy + + surface_upwelling_shortwave_flux_in_air_assuming_clear_sky_and_no_aerosol - - radiation_wavelength + + upwelling_radiance_per_unit_wavelength_in_air - - product_of_northward_wind_and_specific_humidity + + upwelling_radiative_flux_per_unit_wavelength_in_air - - mole_fraction_of_ozone_in_air + + upwelling_radiative_flux_per_unit_wavelength_in_sea_water - - water_evapotranspiration_flux + + mole_concentration_of_diatoms_expressed_as_nitrogen_in_sea_water - - isotropic_shortwave_radiance_in_air + + net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_calcareous_phytoplankton - - isotropic_longwave_radiance_in_air + + moles_of_particulate_inorganic_carbon_per_unit_mass_in_sea_water diff --git a/lib/iris/tests/test_std_names.py b/lib/iris/tests/test_std_names.py index 2093d14bf83..baf2ca23ae6 100644 --- a/lib/iris/tests/test_std_names.py +++ b/lib/iris/tests/test_std_names.py @@ -7,7 +7,7 @@ # import iris tests first so that some things can be initialised before importing anything else import iris.tests as tests # isort:skip -from iris.std_names import STD_NAMES +from iris.std_names import CF_STANDARD_NAME_TABLE_VERSION, STD_NAMES class TestStandardNames(tests.IrisTest): @@ -18,7 +18,7 @@ class TestStandardNames(tests.IrisTest): longMessage = True - def test_standard_names(self): + def test_standard_names_table(self): # Check we have a dict self.assertIsInstance(STD_NAMES, dict) @@ -46,6 +46,12 @@ def test_standard_names(self): "\nInvalid standard name(s) present in STD_NAMES", ) + def test_standard_names_version(self): + # Check we have a dict + self.assertIsInstance(CF_STANDARD_NAME_TABLE_VERSION, int) + # Check the value is roughly sensible. + self.assertTrue(70 < CF_STANDARD_NAME_TABLE_VERSION < 999) + if __name__ == "__main__": tests.main() diff --git a/tools/generate_std_names.py b/tools/generate_std_names.py index 08bacbe1e07..4999956b041 100644 --- a/tools/generate_std_names.py +++ b/tools/generate_std_names.py @@ -37,6 +37,8 @@ This file is automatically generated. Do not edit this file by hand. +Generated from CF standard-name table version : {table_version} + The file will be generated during a standard build/installation:: python setup.py build @@ -76,6 +78,8 @@ def to_dict(infile, outfile): tree = ET.parse(infile) + cf_table_version_string = tree.find('version_number').text + for section in process_name_table(tree, 'entry', 'canonical_units'): values.update(section) @@ -87,7 +91,10 @@ def to_dict(infile, outfile): key : {'canonical_units' : values.get(valued['entry_id']).get('canonical_units')} }) - outfile.write(STD_VALUES_FILE_TEMPLATE + pprint.pformat(values)) + text = STD_VALUES_FILE_TEMPLATE.format(table_version=cf_table_version_string) + text += pprint.pformat(values) + text += f'\n\nCF_STANDARD_NAME_TABLE_VERSION = {cf_table_version_string}\n' + outfile.write(text) if __name__ == "__main__":