Former-commit-id:a02aeb236c
[formerly9f19e3f712
] [formerlya02aeb236c
[formerly9f19e3f712
] [formerly06a8b51d6d
[formerly 64fa9254b946eae7e61bbc3f513b7c3696c4f54f]]] Former-commit-id:06a8b51d6d
Former-commit-id:8e80217e59
[formerly3360eb6c5f
] Former-commit-id:377dcd10b9
69 lines
No EOL
2.5 KiB
Python
69 lines
No EOL
2.5 KiB
Python
##
|
|
# This software was developed and / or modified by Raytheon Company,
|
|
# pursuant to Contract DG133W-05-CQ-1067 with the US Government.
|
|
#
|
|
# U.S. EXPORT CONTROLLED TECHNICAL DATA
|
|
# This software product contains export-restricted data whose
|
|
# export/transfer/disclosure is restricted by U.S. law. Dissemination
|
|
# to non-U.S. persons whether in the United States or abroad requires
|
|
# an export license or other authorization.
|
|
#
|
|
# Contractor Name: Raytheon Company
|
|
# Contractor Address: 6825 Pine Street, Suite 340
|
|
# Mail Stop B8
|
|
# Omaha, NE 68106
|
|
# 402.291.0100
|
|
#
|
|
# See the AWIPS II Master Rights File ("Master Rights File.pdf") for
|
|
# further licensing information.
|
|
###
|
|
|
|
import IsenStability
|
|
import Vorticity
|
|
|
|
##
|
|
# Calculate the isentropic potential vorticity through a layer.
|
|
#
|
|
# @change: Adapted from calcpv.f 2008-18-06
|
|
# User Notes:
|
|
#
|
|
# 1. Stability is defined as -dP/d(theta). We calculate this through
|
|
# the layer from the isentropic surface 'n' to the surface above it,
|
|
# 'n+1'.
|
|
#
|
|
# 2. Since we are dealing with a layer, we calculate a mean absolute
|
|
# vorticity using the winds at the upper and lower layers.
|
|
#
|
|
# 3. The PV is then [mean abs. vort.]/[stability]
|
|
#
|
|
# @param p_up: Pressure on upper isentrope (mb)
|
|
# @param p_lo: Pressure on lower isentrope (mb)
|
|
# @param o_up: Upper isentrope (K) (usually scalar)
|
|
# @param o_lo: This (lower) isentrope (K) (usually scalar)
|
|
# @param Wind_up: tuple(U,V) of winds on upper isentrope (m/s)
|
|
# @param Wind_lo: tuple(U,V) of winds on lower isentrope (m/s)
|
|
# @param dx: Spacing between data points in X direction (m)
|
|
# @param dy: Spacing between data points in Y direction (m)
|
|
# @param coriolis: Coriolis parameters (/s)
|
|
# @return: isentropic potential vorticity array
|
|
#
|
|
def execute(p_up, p_lo, o_up, o_lo, vector_up, vector_lo, dx, dy, coriolis):
|
|
"Calculate the isentropic potential vorticity through a layer."
|
|
|
|
u_up, v_up = vector_up[2], vector_up[3]
|
|
u_lo, v_lo = vector_lo[2], vector_lo[3]
|
|
|
|
|
|
# Calculate the absolute vorticity at each isentropic surface.
|
|
avort1 = Vorticity.execute(u_up, v_up, coriolis, dx, dy)
|
|
avort2 = Vorticity.execute(u_lo, v_lo, coriolis, dx, dy)
|
|
|
|
# Calculate the isentropic stability through the layer.
|
|
pvort = IsenStability.execute(p_up, p_lo, o_up, o_lo)
|
|
|
|
# Calculate isentropic potential vorticity
|
|
result = avort1 + avort2
|
|
result *= 0.5
|
|
result /= pvort
|
|
|
|
return result |