You signed in with another tab or window. Reload to refresh your session.You signed out in another tab or window. Reload to refresh your session.You switched accounts on another tab or window. Reload to refresh your session.Dismiss alert
The overschrijdingsfrequenties derived within KWK are a combination of weibul-fit over measurement data for high frequencies and HYDRA-data for low-frequencies. The latter are still to be updated, differences are expected. However, the first ones (high frequencies) also differ from reference datasets. This is unexpected.
Some details:
the examples in this issue focus on higher frequencies (5 times per year to once per 10 years)
the data could be different in both methods. However, the KWK-python calculation is based on all available extremes for each station. If I look at the availability in Missing/duplicated values in WATHTE timeseries and extremes Rijkswaterstaat/wm-ws-dl#39, it seems that at least for Hoek van Holland and Vlissingen all extremes are available. This also seems to be the case in the locally created check-figures with extremes. It could be that not all data was available for the old method, or some data was excluded.
The method might be sligtly different. I assumed the method implemented within the kenmerkendewaarden project in 2020 by BD corresponded to what was used before, but this might not be the case. It would also not explain why some stations do come close to reference results.
The text was updated successfully, but these errors were encountered:
veenstrajelmer
changed the title
overschrijding: new values for 2011 differ from reference dataset
Exceedance frequencies for 2011 differ from reference dataset
Oct 14, 2024
The overschrijdingsfrequenties derived within KWK are a combination of weibul-fit over measurement data for high frequencies and HYDRA-data for low-frequencies. The latter are still to be updated, differences are expected. However, the first ones (high frequencies) also differ from reference datasets. This is unexpected.
Some details:
Gele-boekje-2016
values correspond to the exceedance frequencies from “Kenmerkende waarden getijgebied 2011" (juli, 2013)KWK-python
andGele-boekje-2016
both cover the exceedance waterlevel data up to 1-1-2011Some stations from south to north:
The westerly stations seem to show a shift in the frequency table (row-wise), but the northerly stations not per se. The differences can be caused by:
KWK-python
calculation is based on all available extremes for each station. If I look at the availability in Missing/duplicated values in WATHTE timeseries and extremes Rijkswaterstaat/wm-ws-dl#39, it seems that at least for Hoek van Holland and Vlissingen all extremes are available. This also seems to be the case in the locally created check-figures with extremes. It could be that not all data was available for the old method, or some data was excluded.The text was updated successfully, but these errors were encountered: