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Update copyright for Kepert wind field
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wcarthur committed Mar 3, 2024
1 parent 46ab80b commit 43b5215
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16 changes: 15 additions & 1 deletion wind/windmodels.f90
@@ -1,9 +1,23 @@
subroutine fkerpert(R, lam, f, rMax, Vm, thetaFm, vFm, d2Vm, dVm, dP, beta, rho, Ux, Uy, n)
!$ use omp_lib

! Kepert, J., 2001: The Dynamics of Boundary Layer Jets within the
! Analytical linear model of the tropical cyclone boundary layer
! as in Kepert, J., 2001: The Dynamics of Boundary Layer Jets within the
! Tropical Cyclone Core. Part I: Linear Theory. J. Atmos. Sci., 58,
! 2469-2484

! Written Jeff Kepert, Bureau of Meteorology, 1998-2000.
! Copyright the Bureau of Meteorology.
! Please do not distribute without my knowledge.

! The model is, so far as I know, robust, except if the storm is
! close to inertially neutral (e.g. b too big). Note that it was written
! to understand the dynamics, not to make accurate predictions -
! the constants (C, K, etc) have not been tuned to observations.
! Note also that because of a linearisation in the derivation, the
! model does not produce the correct limit in the limit r -> infinity.

! Modified by Craig Arthur, Geoscience Australia

! This calculates the Kepert wind field with a Holland pressure profile.

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16 changes: 15 additions & 1 deletion wind/windmodels.py
Expand Up @@ -1054,9 +1054,23 @@ def field(self, R, lam, vFm, thetaFm, thetaMax=0.):
class KepertWindField(WindFieldModel):

"""
Kepert, J., 2001: The Dynamics of Boundary Layer Jets within the
Analytical linear model of the tropical cyclone boundary layer
as in Kepert, J., 2001: The Dynamics of Boundary Layer Jets within the
Tropical Cyclone Core. Part I: Linear Theory. J. Atmos. Sci., 58,
2469-2484
Written Jeff Kepert, Bureau of Meteorology, 1998-2000.
Copyright the Bureau of Meteorology.
Please do not distribute without my knowledge.
The model is, so far as I know, robust, except if the storm is
close to inertially neutral (e.g. b too big). Note that it was written
to understand the dynamics, not to make accurate predictions -
the constants (C, K, etc) have not been tuned to observations.
Note also that because of a linearisation in the derivation, the
model does not produce the correct limit in the limit r -> infinity.
Modified by Craig Arthur, Geoscience Australia
"""

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