Create 2D cylindrical maps on a flattened ellipsoid of all three vector components of the magnetic field, the magnitude of the magnetic field, and the magnetic potential.
call MakeMagGridDH (cilm, lmax, r0, a, f, rad, theta, phi, total, n, sampling, lmaxcalc, potgrid, exitstatus)
cilm : input, real*8, dimension (2, lmax+1, lmax+1)
: The real Schmidt semi-normalized spherical harmonic coefficients to be expanded in the space domain. The coefficients C1lm and C2lm refer to the cosine (Clm) and sine (Slm) coefficients, respectively, with Clm=cilm(1,l+1,m+1) and Slm=cilm(2,l+1,m+1). Alternatively, C1lm and C2lm correspond to the positive and negative order coefficients, respectively.
lmax : input, integer
: The maximum spherical harmonic degree of the coefficients cilm. This determines the number of samples of the output grids, n=2*lmax+2, and the latitudinal sampling interval, 90/(lmax+1).
r0 : input, real*8
: The reference radius of the spherical harmonic coefficients.
a : input, real*8
: The semi-major axis of the flattened ellipsoid on which the field is computed.
f : input, real*8
: The flattening of the reference ellipsoid: i.e., F=(R_equator-R_pole)/R_equator.
rad : output, real*8, dimension(2*lmax+2, sampling*(2*lmax+2))
: A 2D equally sampled (n by n) or equally spaced (n by 2n) grid of the radial component of the magnetic field corresponding to the input spherical harmonic coefficients cilm. The first latitudinal band corresponds to 90 N, the latitudinal band for 90 S is not included, and the latitudinal sampling interval is 180/n degrees. The first longitudinal band is 0 E, the longitudinal band for 360 E is not included, and the longitudinal sampling interval is 360/n for an equally sampled and 180/n for an equally spaced grid, respectively.
theta : output, real*8, dimension(2*lmax+2, sampling*(2*lmax+2))
: A 2D equally sampled or equally spaced grid of the theta component of the magnetic field.
phi : output, real*8, dimension(2*lmax+2, sampling*(2*lmax+2))
: A 2D equally sampled or equally spaced grid of the phi component of the magnetic field.
total : output, real*8, dimension(2*lmax+2, sampling*(2*lmax+2))
: A 2D equally sampled or equally spaced grid of the total magnetic field strength.
n : output, integer
: The number of samples in latitude of the output grids. This is equal to 2lmax+2.
sampling : optional, input, integer, default = 1
: If 1 (default) the output grids are equally sampled (n by n). If 2, the grids are equally spaced (n by 2n).
lmaxcalc : optional, input, integer, default = lmax
: The maximum spherical harmonic degree used in evaluating the functions. This must be less than or equal to lmax.
potgrid : output, real*8, dimension(2*lmax+2, sampling*(2*lmax+2))
: A 2D equally sampled or equaly spaced grid of the magnetic potential.
exitstatus : output, optional, integer
: If present, instead of executing a STOP when an error is encountered, the variable exitstatus will be returned describing the error. 0 = No errors; 1 = Improper dimensions of input array; 2 = Improper bounds for input variable; 3 = Error allocating memory; 4 = File IO error.
MakeMagGridDH will create 2-dimensional cylindrical maps from the spherical harmonic coefficients cilm of all three components of the magnetic field, the total field strength, and the magnetic potential. The magnetic potential is given by
V = R0 Sum_{l=1}^LMAX (R0/r)^{l+1} Sum_{m=-l}^l C_{lm} Y_{lm}
and the magnetic field is
B = - Grad V.
The coefficients are referenced to a radius r0, and the function is computed on a flattened ellipsoid with semi-major axis a (i.e., the mean equatorial radius) and flattening f.
The default is to calculate grids for use in the Driscoll and Healy routines that are equally sampled (n by n), but this can be changed to calculate equally spaced grids (n by 2n) by setting the optional argument sampling to 2. The input value of lmax determines the number of samples, n=2lmax+2, and the latitudinal sampling interval, 90/(lmax+1). The first latitudinal band of the grid corresponds to 90 N, the latitudinal band for 90 S is not calculated, and the latitudinal sampling interval is 180/n degrees. The first longitudinal band is 0 E, the longitudinal band for 360 E is not calculated, and the longitudinal sampling interval is 360/n for equally sampled and 180/n for equally spaced grids, respectively.