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Zachary Nasipak committed Dec 22, 2023
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# Summary

In general relativity, the motion of a free falling test particle in a curved spacetime is
described by a geodesic - the generalization of a "straight line" path to a curved space.
[comment: maybe we just say "...by a geodesic - the minimal path between two points in a curved space"]
In general relativity, the motion of a free-falling test particle in a curved spacetime is
described by a timelike geodesic - the minimal path between two points in space.
The geodesics of Kerr spacetime are of particular interest in the field of black
hole perturbation theory because they describe the zeroth order motion of a small object
hole perturbation theory, because they describe the zeroth-order motion of a small object
moving through the background spacetime of a much more massive spinning black hole. For this reason, computing
geodesics is an important step in modeling the gravitational radiation emitted by an
extreme mass ratio inspiral (EMRI) - an astrophysical binary in which a stellar mass
extreme-mass-ratio inspiral (EMRI) - an astrophysical binary in which a stellar mass
compact object, such as a neutron star or black hole (with mass $10^1 - 10^2 M_\odot$),
spirals into a massive black hole (with mass $10^4 - 10^7 M_\odot$).

Kerr spacetime has several nice properties which simplify the problem of computing geodesics. Since
it has both time-translation symmetry and rotational symmetry, energy and angular momentum are conserved quantities. It is also
equipped with a higher order symmetry which gives rise to a third constant of motion called the Carter
constant. These three constants of motion, along with the spin of the black hole, uniquely define a geodesic up to
initial conditions [@schmidt]. Alternatively, geodesics can be identified using a suitably generalized
it has both time-translation symmetry and rotational symmetry, energy and (the $z$-component of) angular momentum
are conserved quantities. It is also equipped with a higher order symmetry which gives rise to a third constant of motion
called the Carter constant. These three constants of motion, along with the spin of the black hole, uniquely define
a geodesic up to initial conditions [@schmidt]. Alternatively, geodesics can be identified using a suitably generalized
version of the parameters used to define a Keplerian orbit (eccentricity, semi-latus rectum, and inclination angle).
Bound geodesics also possess fundamental frequencies since their radial, azimuthal, and polar motions are periodic.

`KerrGeoPy` is a Python package which computes both stable and plunging geodesics in Kerr spacetime using the
`KerrGeoPy` is a Python package which computes both stable and plunging timelike geodesics in Kerr spacetime using the
analytic solutions to the geodesic equation derived in [@fujita] and
[@dyson]. It mirrors and builds upon much of the functionality of the `KerrGeodesics` [@kerrgeodesics] Mathematica library.
Geodesic solutions are written in terms of Legendre elliptic integrals, which are
Expand Down Expand Up @@ -70,33 +69,34 @@ Antenna (LISA), a future space-based gravitational wave observatory consisting o
constellation of three satellites in orbit around the sun. LISA is an ESA-led mission
with significant contributions from NASA which is set to launch in the 2030s. It will
complement existing ground-based detectors by opening up the millihertz band of the
gravitational wave spectrum [@lisa]. Because sources in this band evolve slowly over time and remain observable
gravitational wave spectrum [@lisa]. Because sources in this band evolve more slowly over time and remain observable
for a period of days to years, LISA is expected to detect many overlapping signals at all times.
Thus, accurate waveform models are needed in order to identify gravitational wave sources and
perform parameter estimation - the process of approximating characteristics of a source.

For most LISA sources, well-developed waveform models based on either numerical relativity
or post-Newtonian theory already exist. However, EMRIs are instead best
or post-Newtonian theory already exist. However, EMRIs are instead more naturally
described by black hole perturbation theory, and the EMRI waveform models that currently exist
are comparatively underdeveloped. In a perturbation theory model, the orbital trajectory is assumed to be a geodesic at
leading order. Higher order corrections are then computed by introducing the gravitational
field of the inspiraling object as a perturbation to the background spacetime of the massive black hole,
expanded in powers of the mass ratio.

In order to meet the accuracy requirements for LISA parameter estimation, EMRI waveform
models must include second order corrections to the orbital trajectory. However, to date,
most development has focused on first order corrections to only the simplest cases,
such as Schwarzschild orbits and equatorial Kerr orbits [@emri]. Additionally, most development
has taken place in Mathematica, which is an expensive and proprietary piece of software. `KerrGeoPy` is
are underdeveloped compared to other LISA sources. In a perturbation theory model, the orbital trajectory
is assumed to be a geodesic at leading order. Higher-order corrections are then computed by introducing
the gravitational field of the inspiraling object as a perturbation to the background spacetime of the
massive black hole, expanded in powers of the mass ratio.

To meet the accuracy requirements for LISA parameter estimation, EMRI waveform
models must include both first- and second-order corrections to the orbital trajectory. However, to date,
second-order corrections are only available for the most simple systems,
quasi-circular inspirals in Schwarzschild [@emri]. Open-source tools can aid in rapidly expanding EMRI models
to more complicated orbits in Kerr spacetime, but at the moment many tools for modeling EMRIs
are only available in Mathematica, which is an expensive and proprietary piece of software. `KerrGeoPy` is
intended to support future development of higher-order waveform models in preparation for
LISA by providing a free alternative to the existing `KerrGeodesics` Mathematica library for other
researchers to build on in their own projects.

Although other Python packages [@kerrgeodesicgw] with similar functionality do exist, they mostly rely on numerical
integration to compute geodesics. The analytic solutions used by `KerrGeoPy` have two main advantages
over this approach. First, they can be much more numerically stable over long time periods and can be quickly evaluated at
any point in time. Second, they produce several useful intermediate terms which are not calculated by other packages that rely on
numerical integration. Modeling EMRIs typically requires long time-averages over the geodesic motion. Therefore,
any point in time. This is essential for EMRI models, which typically require taking long time-averages over the geodesic motion.
Second, they produce several useful intermediate terms which are not calculated by other packages. Therefore,
`KerrGeoPy`, with its analytic solutions and various orbital parametrizations, is specifically tuned to support
perturbative models of binary black holes and their gravitational waves.

Expand All @@ -114,6 +114,9 @@ perturbative models of binary black holes and their gravitational waves.
# Acknowledgements

We would like to thank Niels Warburton and Barry Wardell for their assistance in releasing
`KerrGeoPy` as part of the Black Hole Perturbation Toolkit.
`KerrGeoPy` as part of the Black Hole Perturbation Toolkit. SP acknowledges support through
NASA's Office of STEM Engagement, while ZN acknowledges support by an appointment
to the NASA Postdoctoral Program at the NASA Goddard Space Flight Center, administered by Oak Ridge
Associated Universities under contract with NASA.

# References

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