Source code for geoid_toolkit.ref_ellipsoid

#!/usr/bin/env python
u"""
ref_ellipsoid.py
Written by Tyler Sutterley (12/2022)

Computes parameters for a reference ellipsoid

CALLING SEQUENCE
    wgs84 = ref_ellipsoid('WGS84', UNITS='MKS')

INPUT:
    refell - reference ellipsoid name
        CLK66 = Clarke 1866
        GRS67 = Geodetic Reference System 1967 (IAU ellipsoid)
        GRS80 = Geodetic Reference System 1980
        WGS72 = World Geodetic System 1972
        WGS84 = World Geodetic System 1984
        ATS77 = Quasi-earth centred ellipsoid for ATS77
        NAD27 = North American Datum 1927
        NAD83 = North American Datum 1983
        INTER = International
        KRASS = Krassovsky (USSR)
        MAIRY = Modified Airy (Ireland 1965/1975)
        TOPEX = TOPEX/POSEIDON ellipsoid
        EGM96 = EGM 1996 gravity model
        HGH80 = Hughes 1980 Ellipsoid used in some NSIDC data

OPTIONS:
    UNITS: output units
        MKS: meters, kilograms, seconds
        CGS: centimeters, grams, seconds

OUTPUTS:
    a: semimajor semi-axis (m)
    b: semiminor semi-axis (m)
    f: flattening
    rad_e: mean radius of ellipsoid having the same volume
    rad_p: Polar radius of curvature
    C20: Normalized C20 harmonic
    J2: Oblateness coefficient
    norm_a: Normal gravity at the equator
    norm_b: Normal gravity at the pole
    U0: Normal potential at the ellipsoid
    dk: ratio between gravity at pole versus gravity at equator
    m: m parameter (m)
    lin_ecc: Linear eccentricity
    ecc1: First eccentricity
    ecc2: Second eccentricity
    area: Area of the ellipsoid
    volume: Volume of the ellipsoid
    rho_e: Average density

PYTHON DEPENDENCIES:
    numpy: Scientific Computing Tools For Python
        https://numpy.org
        https://numpy.org/doc/stable/user/numpy-for-matlab-users.html

REFERENCE:
    Hofmann-Wellenhof and Moritz (2006)

UPDATE HISTORY:
    Updated 12/2022: output average Earth's density
    Updated 04/2022: updated docstrings to numpy documentation format
    Updated 11/2020: added function docstrings
    Updated 09/2017: added parameters for Hughes (1980) ellipsoid
    Updated 07/2017: output J2 harmonic (in addition to C20)
    Updated 06/2017: added parameters for EGM1996. CGS now True/False
    Updated 06/2016: using __future__ print function, formatted output
    Updated 08/2015: changed sys.exit to raise ValueError
    Updated 04/2015: added command line option.  little updates to comments
    Updated 06/2014: changed message to sys.exit
    Updated 02/2014: minor update to if statements
"""
import numpy as np

[docs] def ref_ellipsoid(refell, UNITS='MKS'): """ Computes parameters for a reference ellipsoid :cite:p:`HofmannWellenhof:2006hy` Parameters ---------- refell: str Reference ellipsoid name - ``'CLK66'``: Clarke 1866 - ``'GRS67'``: Geodetic Reference System 1967 - ``'GRS80'``: Geodetic Reference System 1980 - ``'HGH80'``: Hughes 1980 Ellipsoid - ``'WGS72'``: World Geodetic System 1972 - ``'WGS84'``: World Geodetic System 1984 - ``'ATS77'``: Quasi-earth centred ellipsoid for ATS77 - ``'NAD27'``: North American Datum 1927 - ``'NAD83'``: North American Datum 1983 - ``'INTER'``: International - ``'KRASS'``: Krassovsky (USSR) - ``'MAIRY'``: Modified Airy (Ireland 1965/1975) - ``'TOPEX'``: TOPEX/POSEIDON ellipsoid - ``'EGM96'``: EGM 1996 gravity model UNITS: str, default 'MKS' Output units - ``'MKS'``: meters, kilograms, seconds - ``'CGS'``: centimeters, grams, seconds Returns ------- a: float semimajor semi-axis (m) b: float semiminor semi-axis (m) f: float flattening rad_e: float Mean radius of ellipsoid having the same volume rad_p: float Polar radius of curvature C20: float Normalized C20 harmonic J2: float Oblateness coefficient norm_a: float Normal gravity at the equator norm_b: float Normal gravity at the pole U0: float Normal potential at the ellipsoid dk: float ratio between gravity at pole versus gravity at equator m: float m parameter (m) lin_ecc: float Linear eccentricity ecc1: float First eccentricity ecc2: float Second eccentricity area: float Area of the ellipsoid volume: float Volume of the ellipsoid rho_e: float Average density """ # validate units assert UNITS in ('MKS', 'CGS') # set parameters for ellipsoid if refell.upper() in ('CLK66','NAD27'): # Clarke 1866 a_axis = 6378206.4# [m] semimajor axis of the ellipsoid flat = 1.0/294.9786982# flattening of the ellipsoid elif refell.upper() in ('GRS80','NAD83'): # Geodetic Reference System 1980 # North American Datum 1983 a_axis = 6378135.0# [m] semimajor axis of the ellipsoid flat = 1.0/298.26# flattening of the ellipsoid GM = 3.986005e14# [m^3/s^2] Geocentric Gravitational Constant elif (refell.upper() == 'GRS67'): # Geodetic Reference System 1967 # International Astronomical Union (IAU ellipsoid) a_axis = 6378160.0# [m] semimajor axis of the ellipsoid flat = 1.0/298.247167427# flattening of the ellipsoid GM = 3.98603e14# [m^3/s^2] Geocentric Gravitational Constant omega = 7292115.1467e-11# angular velocity of the Earth [rad/s] elif (refell.upper() == 'WGS72'): # World Geodetic System 1972 a_axis = 6378135.0# [m] semimajor axis of the ellipsoid flat = 1.0/298.26# flattening of the ellipsoid elif (refell.upper() == 'WGS84'): # World Geodetic System 1984 a_axis = 6378137.0# [m] semimajor axis of the ellipsoid flat = 1.0/298.257223563# flattening of the ellipsoid elif (refell.upper() == 'ATS77'): # Quasi-earth centred ellipsoid for ATS77 a_axis = 6378135.0# [m] semimajor axis of the ellipsoid flat = 1.0/298.257# flattening of the ellipsoid elif (refell.upper() == 'KRASS'): # Krassovsky (USSR) a_axis = 6378245.0# [m] semimajor axis of the ellipsoid flat = 1.0/298.3# flattening of the ellipsoid elif (refell.upper() == 'INTER'): # International a_axis = 6378388.0# [m] semimajor axis of the ellipsoid flat = 1/297.0# flattening of the ellipsoid elif (refell.upper() == 'MAIRY'): # Modified Airy (Ireland 1965/1975) a_axis = 6377340.189# [m] semimajor axis of the ellipsoid flat = 1/299.3249646# flattening of the ellipsoid elif (refell.upper() == 'TOPEX'): # TOPEX/POSEIDON ellipsoid a_axis = 6378136.3# [m] semimajor axis of the ellipsoid flat = 1.0/298.257# flattening of the ellipsoid GM = 3.986004415e14# [m^3/s^2] elif (refell.upper() == 'EGM96'): # EGM 1996 gravity model a_axis = 6378136.3# [m] semimajor axis of the ellipsoid flat = 1.0/298.256415099# flattening of the ellipsoid GM = 3.986004415e14# [m^3/s^2] elif (refell.upper() == 'HGH80'): # Hughes 1980 Ellipsoid used in some NSIDC data a_axis = 6378273.0# [m] semimajor axis of the ellipsoid flat = 1.0/298.279411123064# flattening of the ellipsoid else: raise ValueError('Incorrect reference ellipsoid Name') if refell.upper() not in ('GRS80','GRS67','NAD83','TOPEX','EGM96'): # for ellipsoids not listing the Geocentric Gravitational Constant GM = 3.986004418e14# [m^3/s^2] if refell.upper() not in ('GRS67'): # for ellipsoids not listing the angular velocity of the Earth omega = 7292115e-11# [rad/s] # universal gravitational constant [N*m^2/kg^2] G = 6.67430e-11 # convert units to CGS if (UNITS == 'CGS'): a_axis *= 100.0 GM *= 1e6 G *= 1000.0 # [dyn*cm^2/g^2] # DERIVED PARAMETERS: # mean radius of the Earth having the same volume # (4pi/3)R^3 = (4pi/3)(a^2)b = (4pi/3)(a^3)(1 - f) rad_e = a_axis*(1.0 - flat)**(1.0/3.0) # semiminor axis of the ellipsoid b_axis = (1.0 -flat)*a_axis# [m] # Ratio between ellipsoidal axes ratio = (1.0 -flat) # Polar radius of curvature pol_rad=a_axis/(1.0 -flat) # Linear eccentricity lin_ecc = np.sqrt((2.0*flat - flat**2)*a_axis**2) # first numerical eccentricity ecc1 = lin_ecc/a_axis # second numerical eccentricity ecc2 = lin_ecc/b_axis # m parameter [omega^2*a^2*b/(GM)] # p. 70, Eqn.(2-137) mp = omega**2*((1 -flat)*a_axis**3)/GM # q, q_0 # p. 67, Eqn.(2-113) q = 0.5*((1.0 + 3.0/(ecc2**2))*np.arctan(ecc2)-3.0/ecc2) q_0 = 3*(1.0 +1.0/(ecc2**2))*(1.0 -1.0/ecc2*np.arctan(ecc2))-1.0 # J_2 p. 75 Eqn.(2-167), p. 76 Eqn.(2-172) j_2 = (ecc1**2)*(1.0 - 2.0*mp*ecc2/(15.0*q))/3.0 # Normalized C20 terms. # p. 60, Eqn.(2-80) C20 = -j_2/np.sqrt(5.0) # Normal gravity at the equator. # p. 71, Eqn.(2-141) ga = GM/(a_axis*b_axis)*(1.0 -mp -mp*ecc2*q_0/(6.0*q)) # Normal gravity at the pole. # p. 71, Eqn.(2-142) gb = GM/(a_axis**2.0)*(1.0 +mp*ecc2*q_0/(3.0*q)) # ratio between gravity at pole versus gravity at equator dk = b_axis*gb/(a_axis*ga) - 1.0 # Normal potential at the ellipsoid # p. 68, Eqn.(2-123) U0 = GM/lin_ecc*np.arctan(ecc2)+(1.0/3.0)*omega**2*a_axis**2 # Surface area of the reference ellipsoid [m^2] area = np.pi*a_axis**2.*(2.+((1.-ecc1**2)/ecc1)*np.log((1.+ecc1)/(1.-ecc1))) # Volume of the reference ellipsoid [m^3] vol = (4.0*np.pi/3.0)*(a_axis**3.0)*(1.0-ecc1**2.0)**0.5 # Average density [kg/m^3] rho_e = GM/(G*vol) return {'a':a_axis, 'b':b_axis, 'f':flat, 'rad_p':pol_rad, 'rad_e':rad_e, 'ratio':ratio, 'GM':GM, 'omega':omega, 'C20':C20, 'J2':j_2, 'U0':U0, 'dk':dk, 'norm_a':ga, 'norm_b':gb, 'mp':mp, 'q':q, 'q0':q_0, 'ecc':lin_ecc, 'ecc1':ecc1,'ecc2':ecc2, 'area':area, 'volume':vol, 'rho_e':rho_e}