/* DOD World Magnetic Model 2010-2015 

See bottom of file for info from original Fortran source code 

Reminder - this is just a model! See the USGS and BGS sites for predicted accuracy.

Usage is 

    var wmm = new WorldMagneticModel();

    then
    
    var dec = wmm.declination(0.0, 59.0, -2.0, 2010.5); 
    
    parameters are 
        altitude in kilometres
        decimal degree latitude, -ve for south
        decimal degree longitude, -ve for west
        date as year + fraction of year
        
    return is declination angle in decimal degrees, 
    +ve for Magnetic North East of True North
    (-999 for < 2010.0 and >= 2015.0)
            
The method knownAnswerTest yields a maximum declination error of 0.007% on the small 2010 USGS test data set. 
The maximum error is at 80S latitude, 120W longitude. The value produced by this code at this point is 70.215 degrees.
This is the same answer as produced by the BGS calculator at http://www.geomag.bgs.ac.uk/gifs/wmm_calc.html

This javascript port by Bill Chadwick, 27-Oct-2008, updated with 2010 coefficients on 3 Jan 2010 
email: w.chadwick<at>sky.com

*/

function WorldMagneticModel (){

/* 2010 - 2015 coefficients from WMM.COF */

this.coff = [
"  1,  0,  -29496.6  ,    0.0     ,   11.6  ,      0.0",
"  1,  1,   -1586.3  ,  4944.4    ,   16.5  ,    -25.9",
"  2,  0,   -2396.6  ,     0.0    ,  -12.1  ,      0.0",
"  2,  1,    3026.1  , -2707.7    ,   -4.4  ,    -22.5",
"  2,  2,    1668.6  ,  -576.1    ,    1.9  ,    -11.8",
"  3,  0,    1340.1  ,     0.0    ,    0.4  ,      0.0",
"  3,  1,   -2326.2  ,  -160.2    ,   -4.1  ,      7.3",
"  3,  2,    1231.9  ,   251.9    ,   -2.9  ,     -3.9",
"  3,  3,     634.0  ,  -536.6    ,   -7.7  ,     -2.6",
"  4,  0,     912.6  ,     0.0    ,   -1.8  ,      0.0",
"  4,  1,     808.9  ,   286.4    ,    2.3  ,      1.1",
"  4,  2,     166.7  ,  -211.2    ,   -8.7  ,      2.7",
"  4,  3,    -357.1  ,   164.3    ,    4.6  ,      3.9",
"  4,  4,      89.4  ,  -309.1    ,   -2.1  ,     -0.8",
"  5,  0,    -230.9  ,     0.0    ,   -1.0  ,      0.0",
"  5,  1,     357.2  ,    44.6    ,    0.6  ,      0.4",
"  5,  2,     200.3  ,   188.9    ,   -1.8  ,      1.8",
"  5,  3,    -141.1  ,  -118.2    ,   -1.0  ,      1.2",
"  5,  4,    -163.0  ,     0.0    ,    0.9  ,      4.0",
"  5,  5,      -7.8  ,   100.9    ,    1.0  ,     -0.6",
"  6,  0,      72.8  ,     0.0    ,   -0.2  ,      0.0",
"  6,  1,      68.6  ,   -20.8    ,   -0.2  ,     -0.2",
"  6,  2,      76.0  ,    44.1    ,   -0.1  ,     -2.1",
"  6,  3,    -141.4  ,    61.5    ,    2.0  ,     -0.4",
"  6,  4,     -22.8  ,   -66.3    ,   -1.7  ,     -0.6",
"  6,  5,      13.2  ,     3.1    ,   -0.3  ,      0.5",
"  6,  6,     -77.9  ,    55.0    ,    1.7  ,      0.9",
"  7,  0,      80.5  ,     0.0    ,    0.1  ,      0.0",
"  7,  1,     -75.1  ,   -57.9    ,   -0.1  ,      0.7",
"  7,  2,      -4.7  ,   -21.1    ,   -0.6  ,      0.3",
"  7,  3,      45.3  ,     6.5    ,    1.3  ,     -0.1",
"  7,  4,      13.9  ,    24.9    ,    0.4  ,     -0.1",
"  7,  5,      10.4  ,     7.0    ,    0.3  ,     -0.8",
"  7,  6,       1.7  ,   -27.7    ,   -0.7  ,     -0.3",
"  7,  7,       4.9  ,    -3.3    ,    0.6  ,      0.3",
"  8,  0,      24.4  ,     0.0    ,   -0.1  ,      0.0",
"  8,  1,       8.1  ,    11.0    ,    0.1  ,     -0.1",
"  8,  2,     -14.5  ,   -20.0    ,   -0.6  ,      0.2",
"  8,  3,      -5.6  ,    11.9    ,    0.2  ,      0.4",
"  8,  4,     -19.3  ,   -17.4    ,   -0.2  ,      0.4",
"  8,  5,      11.5  ,    16.7    ,    0.3  ,      0.1",
"  8,  6,      10.9  ,     7.0    ,    0.3  ,     -0.1",
"  8,  7,     -14.1  ,   -10.8    ,   -0.6  ,      0.4",
"  8,  8,      -3.7  ,     1.7    ,    0.2  ,      0.3",
"  9,  0,       5.4  ,     0.0    ,    0.0  ,      0.0",
"  9,  1,       9.4  ,   -20.5    ,   -0.1  ,      0.0",
"  9,  2,       3.4  ,    11.5    ,    0.0  ,     -0.2",
"  9,  3,      -5.2  ,    12.8    ,    0.3  ,      0.0",
"  9,  4,       3.1  ,    -7.2    ,   -0.4  ,     -0.1",
"  9,  5,     -12.4  ,    -7.4    ,   -0.3  ,      0.1",
"  9,  6,      -0.7  ,     8.0    ,    0.1  ,      0.0",
"  9,  7,       8.4  ,     2.1    ,   -0.1  ,     -0.2",
"  9,  8,      -8.5  ,    -6.1    ,   -0.4  ,      0.3",
"  9,  9,     -10.1  ,     7.0    ,   -0.2  ,      0.2",
" 10,  0,      -2.0  ,     0.0    ,    0.0  ,      0.0",
" 10,  1,      -6.3  ,     2.8    ,    0.0  ,      0.1",
" 10,  2,       0.9  ,    -0.1    ,   -0.1  ,     -0.1",
" 10,  3,      -1.1  ,     4.7    ,    0.2  ,      0.0",
" 10,  4,      -0.2  ,     4.4    ,    0.0  ,     -0.1",
" 10,  5,       2.5  ,    -7.2    ,   -0.1  ,     -0.1",
" 10,  6,      -0.3  ,    -1.0    ,   -0.2  ,      0.0",
" 10,  7,       2.2  ,    -3.9    ,    0.0  ,     -0.1",
" 10,  8,       3.1  ,    -2.0    ,   -0.1  ,     -0.2",
" 10,  9,      -1.0  ,    -2.0    ,   -0.2  ,      0.0",
" 10, 10,      -2.8  ,    -8.3    ,   -0.2  ,     -0.1",
" 11,  0,       3.0  ,     0.0    ,    0.0  ,      0.0",
" 11,  1,      -1.5  ,     0.2    ,    0.0  ,      0.0",
" 11,  2,      -2.1  ,     1.7    ,    0.0  ,      0.1",
" 11,  3,       1.7  ,    -0.6    ,    0.1  ,      0.0",
" 11,  4,      -0.5  ,    -1.8    ,    0.0  ,      0.1",
" 11,  5,       0.5  ,     0.9    ,    0.0  ,      0.0",
" 11,  6,      -0.8  ,    -0.4    ,    0.0  ,      0.1",
" 11,  7,       0.4  ,    -2.5    ,    0.0  ,      0.0",
" 11,  8,       1.8  ,    -1.3    ,    0.0  ,     -0.1",
" 11,  9,       0.1  ,    -2.1    ,    0.0  ,     -0.1",
" 11, 10,       0.7  ,    -1.9    ,   -0.1  ,      0.0",
" 11, 11,       3.8  ,    -1.8    ,    0.0  ,     -0.1",
" 12,  0,      -2.2  ,     0.0    ,    0.0  ,      0.0",
" 12,  1,      -0.2  ,    -0.9    ,    0.0  ,      0.0",
" 12,  2,       0.3  ,     0.3    ,    0.1  ,      0.0",
" 12,  3,       1.0  ,     2.1    ,    0.1  ,      0.0",
" 12,  4,      -0.6  ,    -2.5    ,   -0.1  ,      0.0",
" 12,  5,       0.9  ,     0.5    ,    0.0  ,      0.0",
" 12,  6,      -0.1  ,     0.6    ,    0.0  ,      0.1",
" 12,  7,       0.5  ,     0.0    ,    0.0  ,      0.0",
" 12,  8,      -0.4  ,     0.1    ,    0.0  ,      0.0",
" 12,  9,      -0.4  ,     0.3    ,    0.0  ,      0.0",
" 12, 10,       0.2  ,    -0.9    ,    0.0  ,      0.0",
" 12, 11,      -0.8  ,    -0.2    ,   -0.1  ,      0.0",
" 12, 12,       0.0  ,     0.9    ,    0.1  ,      0.0"
];

/* static variables */

/* some 13x13 2D arrays */
this.c = new Array(13); 
this.cd = new Array(13); 
this.tc = new Array(13); 
this.dp = new Array(13); 
this.k = new Array(13); 

for(var i=0; i< 13; i++)
{
    this.c[i] = new Array(13); 
    this.cd[i] = new Array(13); 
    this.tc[i] = new Array(13); 
    this.dp[i] = new Array(13); 
    this.k[i] = new Array(13); 
}

/* some 1D arrays */
this.snorm = new Array(169); 
this.sp = new Array(13); 
this.cp = new Array(13); 
this.fn = new Array(13); 
this.fm = new Array(13); 
this.pp = new Array(13); 


/* locals */

var maxdeg = 12;
var maxord;
var i,j,D1,D2,n,m;
var a,b,a2,b2,c2,a4,b4,c4,re;
var gnm,hnm,dgnm,dhnm,flnmj;
var c_str;
var c_flds;

/* INITIALIZE CONSTANTS */

maxord = maxdeg;
this.sp[0] = 0.0;
this.cp[0] = this.snorm[0] = this.pp[0] = 1.0;
this.dp[0][0] = 0.0;
a = 6378.137;
b = 6356.7523142;
re = 6371.2;
a2 = a*a;
b2 = b*b;
c2 = a2-b2;
a4 = a2*a2;
b4 = b2*b2;
c4 = a4 - b4;

/* READ WORLD MAGNETIC MODEL SPHERICAL HARMONIC COEFFICIENTS */
this.c[0][0] = 0.0;
this.cd[0][0] = 0.0;

for(i=0; i<this.coff.length; i++)
{
  c_str = this.coff[i];
  c_flds = c_str.split(",");

  n = parseInt(c_flds[0],10);   
  m = parseInt(c_flds[1],10);   
  gnm = parseFloat(c_flds[2]);
  hnm = parseFloat(c_flds[3]);
  dgnm = parseFloat(c_flds[4]);
  dhnm = parseFloat(c_flds[5]);
     
  if (m <= n)
  {
	this.c[m][n] = gnm;
	this.cd[m][n] = dgnm;
	if (m != 0) 
	{
	  this.c[n][m-1] = hnm;
	  this.cd[n][m-1] = dhnm;
	}
  }
}

/* CONVERT SCHMIDT NORMALIZED GAUSS COEFFICIENTS TO UNNORMALIZED */

this.snorm[0] = 1.0;
for (n=1; n<=maxord; n++) 
{
    this.snorm[n] = this.snorm[n-1]*(2*n-1)/n;
    j = 2;
    for (m=0,D1=1,D2=(n-m+D1)/D1; D2>0; D2--,m+=D1) 
    {
        this.k[m][n] = (((n-1)*(n-1))-(m*m))/((2*n-1)*(2*n-3));
        if (m > 0) 
        {
        flnmj = ((n-m+1)*j)/(n+m);
        this.snorm[n+m*13] = this.snorm[n+(m-1)*13]*Math.sqrt(flnmj);
        j = 1;
        this.c[n][m-1] = this.snorm[n+m*13]*this.c[n][m-1];
        this.cd[n][m-1] = this.snorm[n+m*13]*this.cd[n][m-1];
        }
        this.c[m][n] = this.snorm[n+m*13]*this.c[m][n];
        this.cd[m][n] = this.snorm[n+m*13]*this.cd[m][n];
    }
    this.fn[n] = (n+1);
    this.fm[n] = n;
}
this.k[1][1] = 0.0;
this.fm[0] = 0.0;// !!!!!! WMM C and Fortran both have a bug in that fm[0] is not initialised 

}

WorldMagneticModel.prototype.declination = function(altitudeKm, latitudeDegrees, longitudeDegrees, yearFloat){
		


/* locals */

var a = 6378.137;
var b = 6356.7523142;
var re = 6371.2;
var a2 = a*a;
var b2 = b*b;
var c2 = a2-b2;
var a4 = a2*a2;
var b4 = b2*b2;
var c4 = a4 - b4;
var D3, D4;
var dip, ti, gv, dec;
var n,m;
	  
var pi, dt, rlon, rlat, srlon, srlat, crlon, crlat,srlat2,
crlat2, q, q1, q2, ct, d,aor,ar, br, r2, bpp, par,
temp1,parp,temp2,bx,by,bz,bh,dtr,bp,bt, st,ca,sa;

var maxord = 12;
var alt = altitudeKm;
var glon = longitudeDegrees;
var glat = latitudeDegrees;

/*************************************************************************/

dt = yearFloat - 2010.0;
//if more then 5 years has passed since last epoch update then return invalid
if ((dt < 0.0) || (dt > 5.0)) 
    return -999;


pi = 3.14159265359;
dtr = pi/180.0;
rlon = glon*dtr;
rlat = glat*dtr;
srlon = Math.sin(rlon);
srlat = Math.sin(rlat);
crlon = Math.cos(rlon);
crlat = Math.cos(rlat);
srlat2 = srlat*srlat;
crlat2 = crlat*crlat;
this.sp[1] = srlon;
this.cp[1] = crlon;

/* CONVERT FROM GEODETIC COORDS. TO SPHERICAL COORDS. */

q = Math.sqrt(a2-c2*srlat2);
q1 = alt*q;
q2 = ((q1+a2)/(q1+b2))*((q1+a2)/(q1+b2));
ct = srlat/Math.sqrt(q2*crlat2+srlat2);
st = Math.sqrt(1.0-(ct*ct));
r2 = (alt*alt)+2.0*q1+(a4-c4*srlat2)/(q*q);
r = Math.sqrt(r2);
d = Math.sqrt(a2*crlat2+b2*srlat2);
ca = (alt+d)/r;
sa = c2*crlat*srlat/(r*d);

for (m=2; m<=maxord; m++)
{
    this.sp[m] = this.sp[1]*this.cp[m-1]+this.cp[1]*this.sp[m-1];
    this.cp[m] = this.cp[1]*this.cp[m-1]-this.sp[1]*this.sp[m-1];
}
     
aor = re/r;
ar = aor*aor;
br = bt = bp = bpp = 0.0;

for (n=1; n<=maxord; n++) 
{
    ar = ar*aor;
    for (m=0,D3=1,D4=(n+m+D3)/D3; D4>0; D4--,m+=D3) 
    {
        /*
           COMPUTE UNNORMALIZED ASSOCIATED LEGENDRE POLYNOMIALS
           AND DERIVATIVES VIA RECURSION RELATIONS
        */
            
          
        if (n == m) 
        {
          this.snorm[n+m*13] = st*this.snorm[n-1+(m-1)*13];
          this.dp[m][n] = st*this.dp[m-1][n-1]+ct*this.snorm[n-1+(m-1)*13];
        }
        else if (n == 1 && m == 0) 
        {
          this.snorm[n+m*13] = ct*this.snorm[n-1+m*13];
          this.dp[m][n] = ct*this.dp[m][n-1]-st*this.snorm[n-1+m*13];
        }
        else if (n > 1 && n != m) 
        {
          if (m > n-2) this.snorm[n-2+m*13] = 0.0;
          if (m > n-2) this.dp[m][n-2] = 0.0;
          this.snorm[n+m*13] = ct*this.snorm[n-1+m*13]-this.k[m][n]*this.snorm[n-2+m*13];
          this.dp[m][n] = ct*this.dp[m][n-1] - st*this.snorm[n-1+m*13]-this.k[m][n]*this.dp[m][n-2];
         }
         
        /*
        TIME ADJUST THE GAUSS COEFFICIENTS
        */
        this.tc[m][n] = this.c[m][n]+dt*this.cd[m][n];
        if (m != 0) this.tc[n][m-1] = this.c[n][m-1]+dt*this.cd[n][m-1];
        
        /*
        ACCUMULATE TERMS OF THE SPHERICAL HARMONIC EXPANSIONS
        */
        par = ar*this.snorm[n+m*13];
        if (m == 0) 
        {
            temp1 = this.tc[m][n]*this.cp[m];
            temp2 = this.tc[m][n]*this.sp[m];
        }
        else 
        {
            temp1 = this.tc[m][n]*this.cp[m]+this.tc[n][m-1]*this.sp[m];
            temp2 = this.tc[m][n]*this.sp[m]-this.tc[n][m-1]*this.cp[m];
        }
        bt = bt-ar*temp1*this.dp[m][n];
        bp += (this.fm[m]*temp2*par);
        br += (this.fn[n]*temp1*par);
        /*
        SPECIAL CASE:  NORTH/SOUTH GEOGRAPHIC POLES
        */
        if (st == 0.0 && m == 1) 
        {
            if (n == 1) this.pp[n] = this.pp[n-1];
            else this.pp[n] = this.ct*this.pp[n-1]-this.k[m][n]*this.pp[n-2];
            parp = ar*this.pp[n];
            bpp += (this.fm[m]*temp2*parp);
        }
    }
}

if (st == 0.0) 
    bp = bpp;
else 
    bp /= st;
    
/*
    ROTATE MAGNETIC VECTOR COMPONENTS FROM SPHERICAL TO
    GEODETIC COORDINATES
*/
bx = -bt*ca-br*sa;
by = bp;
bz = bt*sa-br*ca;
/*
    COMPUTE DECLINATION (DEC), INCLINATION (DIP) AND
    TOTAL INTENSITY (TI)
*/
bh = Math.sqrt((bx*bx)+(by*by));
ti = Math.sqrt((bh*bh)+(bz*bz));
dec = Math.atan2(by,bx)/dtr;
dip = Math.atan2(bz,bh)/dtr;
/*
    COMPUTE MAGNETIC GRID VARIATION IF THE CURRENT
    GEODETIC POSITION IS IN THE ARCTIC OR ANTARCTIC
    (I.E. GLAT > +55 DEGREES OR GLAT < -55 DEGREES)

    OTHERWISE, SET MAGNETIC GRID VARIATION TO -999.0
*/
gv = -999.0;
if (Math.abs(glat) >= 55.0) 
{
    if (glat > 0.0 && glon >= 0.0) gv = dec-glon;
    if (glat > 0.0 && glon < 0.0) gv = dec+Math.abs(glon);
    if (glat < 0.0 && glon >= 0.0) gv = dec+glon;
    if (glat < 0.0 && glon < 0.0) gv = dec-Math.abs(glon);
    if (gv > +180.0) gv -= 360.0;
    if (gv < -180.0) gv += 360.0;
}
      
return dec;
}

WorldMagneticModel.prototype.knownAnswerTest = function(){

/* http://www.ngdc.noaa.gov/geomag/WMM WMM2010testvalues.pdf */

/* Lat	Lon Dec	    */
/* Lon 240 = 120W, Lon 300 = 60W */

/* Alt 0 km */
var kat2010 = [
"80.00	,0.00	 ,-6.13	    ",	     
"0.00	,120.00	 ,0.97	    ",	        
"-80.00	,240.00	 ,70.21	    "	   
];

var kat2012p5 = [
"80.00	,0.00	 ,-5.21	    ",
"0.00	,120.00	 ,0.88	    ",
"-80.00	,240.00	 ,70.04	    "
];

var maxErr = 0.0;

for(var i=0; i<kat2010.length; i++){

    var c_str = kat2010[i];
  var c_flds = c_str.split(",");
 
  var lat = parseFloat(c_flds[0]);
  var lon = parseFloat(c_flds[1]);
  var exp = parseFloat(c_flds[2]);
  var maxExp;

  var dec = this.declination(0,lat,lon,2010.0); 
  if(Math.abs(dec-exp) > maxErr){
      maxErr = Math.abs(dec-exp);
      maxExp = exp;
  } 

}

for (var i = 0; i < kat2012p5.length; i++) {

    var c_str = kat2012p5[i];
    var c_flds = c_str.split(",");

    var lat = parseFloat(c_flds[0]);
    var lon = parseFloat(c_flds[1]);
    var exp = parseFloat(c_flds[2]);
    var maxExp;

    var dec = this.declination(0, lat, lon, 2012.5);
    if (Math.abs(dec - exp) > maxErr) {
        maxErr = Math.abs(dec - exp);
        maxExp = exp;
    }

}


return maxErr * 100 / maxExp;//max % error

}

/*

C***********************************************************************
C
C
C     SUBROUTINE GEOMAG (GEOMAGNETIC FIELD COMPUTATION)
C
C
C***********************************************************************
C
C     GEOMAG IS A NATIONAL GEOSPATIAL INTELLIGENCE AGENCY (NGA) STANDARD
C     PRODUCT.  IT IS COVERED UNDER NGA MILITARY SPECIFICATION:
C     MIL-W-89500 (1993).
C
C***********************************************************************
C     Contact Information
C
C     Software and Model Support
C     	National Geophysical Data Center
C     	NOAA EGC/2
C     	325 Broadway
C     	Boulder, CO 80303 USA
C     	Attn: Susan McLean or Stefan Maus
C     	Phone:  (303) 497-6478 or -6522
C     	Email:  Susan.McLean@noaa.gov or Stefan.Maus@noaa.gov
C		Web: http://www.ngdc.noaa.gov/seg/WMM/
C
C     Sponsoring Government Agency
C	   National Geospatial-Intelligence Agency
C    	   PRG / CSAT, M.S. L-41
C    	   3838 Vogel Road
C    	   Arnold, MO 63010
C    	   Attn: Craig Rollins
C    	   Phone:  (314) 263-4186
C    	   Email:  Craig.M.Rollins@Nga.Mil
C
C      Original Program By:
C        Dr. John Quinn
C        FLEET PRODUCTS DIVISION, CODE N342
C        NAVAL OCEANOGRAPHIC OFFICE (NAVOCEANO)
C        STENNIS SPACE CENTER (SSC), MS 39522-5001
C
C***********************************************************************
C
C     PURPOSE:  THIS ROUTINE COMPUTES THE DECLINATION (DEC),
C               INCLINATION (DIP), TOTAL INTENSITY (TI) AND
C               GRID VARIATION (GV - POLAR REGIONS ONLY, REFERENCED
C               TO GRID NORTH OF A STEREOGRAPHIC PROJECTION) OF THE
C               EARTH'S MAGNETIC FIELD IN GEODETIC COORDINATES
C               FROM THE COEFFICIENTS OF THE CURRENT OFFICIAL
C               DEPARTMENT OF DEFENSE (DOD) SPHERICAL HARMONIC WORLD
C               MAGNETIC MODEL (WMM.COF).  THE WMM SERIES OF MODELS IS
C               UPDATED EVERY 5 YEARS ON JANUARY 1ST OF THOSE YEARS
C               WHICH ARE DIVISIBLE BY 5 (I.E. 2000, 2005, 2010 ETC.)
C               BY NOAA'S NATIONAL GEOPHYSICAL DATA CENTER IN
C               COOPERATION WITH THE BRITISH GEOLOGICAL SURVEY (BGS).
C               THE MODEL IS BASED ON GEOMAGNETIC FIELD MEASUREMENTS
C               FROM SATELLITE AND GROUND OBSERVATORIES.
C
C***********************************************************************
C
C     MODEL:  THE WMM SERIES GEOMAGNETIC MODELS ARE COMPOSED
C             OF TWO PARTS:  THE MAIN FIELD MODEL, WHICH IS
C             VALID AT THE BASE EPOCH OF THE CURRENT MODEL AND
C             A SECULAR VARIATION MODEL, WHICH ACCOUNTS FOR SLOW
C             TEMPORAL VARIATIONS IN THE MAIN GEOMAGNETIC FIELD
C             FROM THE BASE EPOCH TO A MAXIMUM OF 5 YEARS BEYOND
C             THE BASE EPOCH.  FOR EXAMPLE, THE BASE EPOCH OF
C             THE WMM-2005 MODEL IS 2005.0.  THIS MODEL IS THEREFORE
C             CONSIDERED VALID BETWEEN 2005.0 AND 2010.0. THE
C             COMPUTED MAGNETIC PARAMETERS ARE REFERENCED TO THE
C             WGS-84 ELLIPSOID.
C
C***********************************************************************
C
C     ACCURACY:  IN OCEAN AREAS AT THE EARTH'S SURFACE OVER THE
C                ENTIRE 5 YEAR LIFE OF THE DEGREE AND ORDER 12
C                SPHERICAL HARMONIC MODEL WMM-2005, THE ESTIMATED
C                MAXIMUM RMS ERRORS FOR THE VARIOUS MAGNETIC COMPONENTS
C                ARE:
C
C                DEC  -   0.5 Degrees
C                DIP  -   0.5 Degrees
C                TI   - 280.0 nanoTeslas (nT)
C                GV   -   0.5 Degrees
C
C                OTHER MAGNETIC COMPONENTS THAT CAN BE DERIVED FROM
C                THESE FOUR BY SIMPLE TRIGONOMETRIC RELATIONS WILL
C                HAVE THE FOLLOWING APPROXIMATE ERRORS OVER OCEAN AREAS:
C
C                X    - 140 nT (North)
C                Y    - 140 nT (East)
C                Z    - 200 nT (Vertical) Positive is down
C                H    - 200 nT (Horizontal)
C
C                OVER LAND THE MAXIMUM RMS ERRORS ARE EXPECTED TO BE
C                HIGHER, ALTHOUGH THE RMS ERRORS FOR DEC, DIP, AND GV
C                ARE STILL ESTIMATED TO BE LESS THAN 1.0 DEGREE, FOR
C                THE ENTIRE 5-YEAR LIFE OF THE MODEL AT THE EARTH's
C                SURFACE.  THE OTHER COMPONENT ERRORS OVER LAND ARE
C                MORE DIFFICULT TO ESTIMATE AND SO ARE NOT GIVEN.
C
C                THE ACCURACY AT ANY GIVEN TIME FOR ALL OF THESE
C                GEOMAGNETIC PARAMETERS DEPENDS ON THE GEOMAGNETIC
C                LATITUDE.  THE ERRORS ARE LEAST FROM THE EQUATOR TO
C                MID-LATITUDES AND GREATEST NEAR THE MAGNETIC POLES.
C
C                IT IS VERY IMPORTANT TO NOTE THAT A DEGREE AND
C                ORDER 12 MODEL, SUCH AS WMM-2005, DESCRIBES ONLY
C                THE LONG WAVELENGTH SPATIAL MAGNETIC FLUCTUATIONS
C                DUE TO EARTH'S CORE.  NOT INCLUDED IN THE WMM SERIES
C                MODELS ARE INTERMEDIATE AND SHORT WAVELENGTH
C                SPATIAL FLUCTUATIONS OF THE GEOMAGNETIC FIELD
C                WHICH ORIGINATE IN THE EARTH'S MANTLE AND CRUST.
C                CONSEQUENTLY, ISOLATED ANGULAR ERRORS AT VARIOUS
C                POSITIONS ON THE SURFACE (PRIMARILY OVER LAND, IN
C                CONTINENTAL MARGINS AND OVER OCEANIC SEAMOUNTS,
C                RIDGES AND TRENCHES) OF SEVERAL DEGREES MAY BE
C                EXPECTED. ALSO NOT INCLUDED IN THE MODEL ARE
C                NONSECULAR TEMPORAL FLUCTUATIONS OF THE GEOMAGNETIC
C                FIELD OF MAGNETOSPHERIC AND IONOSPHERIC ORIGIN.
C                DURING MAGNETIC STORMS, TEMPORAL FLUCTUATIONS CAN
C                CAUSE SUBSTANTIAL DEVIATIONS OF THE GEOMAGNETIC
C                FIELD FROM MODEL VALUES.  IN ARCTIC AND ANTARCTIC
C                REGIONS, AS WELL AS IN EQUATORIAL REGIONS, DEVIATIONS
C                FROM MODEL VALUES ARE BOTH FREQUENT AND PERSISTENT.
C
C                IF THE REQUIRED DECLINATION ACCURACY IS MORE
C                STRINGENT THAN THE WMM SERIES OF MODELS PROVIDE, THEN
C                THE USER IS ADVISED TO REQUEST SPECIAL (REGIONAL OR
C                LOCAL) SURVEYS BE PERFORMED AND MODELS PREPARED.
C                REQUESTS OF THIS NATURE SHOULD BE MADE TO NIMA
C                AT THE ADDRESS ABOVE.
C
C***********************************************************************
C
C     USAGE:  THIS ROUTINE IS BROKEN UP INTO TWO PARTS:
C
C             A) AN INITIALIZATION MODULE, WHICH IS CALLED ONLY
C                ONCE AT THE BEGINNING OF THE MAIN (CALLING)
C                PROGRAM
C             B) A PROCESSING MODULE, WHICH COMPUTES THE MAGNETIC
C                FIELD PARAMETERS FOR EACH SPECIFIED GEODETIC
C                POSITION (ALTITUDE, LATITUDE, LONGITUDE) AND TIME
C
C             INITIALIZATION IS MADE VIA A SINGLE CALL TO THE MAIN
C             ENTRY POINT (GEOMAG), WHILE SUBSEQUENT PROCESSING
C             CALLS ARE MADE THROUGH THE SECOND ENTRY POINT (GEOMG1).
C             ONE CALL TO THE PROCESSING MODULE IS REQUIRED FOR EACH
C             POSITION AND TIME.
C
C             THE VARIABLE MAXDEG IN THE INITIALIZATION CALL IS THE
C             MAXIMUM DEGREE TO WHICH THE SPHERICAL HARMONIC MODEL
C             IS TO BE COMPUTED.  IT MUST BE SPECIFIED BY THE USER
C             IN THE CALLING ROUTINE.  NORMALLY IT IS 12 BUT IT MAY
C             BE SET LESS THAN 12 TO INCREASE COMPUTATIONAL SPEED AT
C             THE EXPENSE OF REDUCED ACCURACY.
C
C             THE PC VERSION OF THIS SUBROUTINE MUST BE COMPILED
C             WITH A FORTRAN 77 COMPATIBLE COMPILER SUCH AS THE
C             MICROSOFT OPTIMIZING FORTRAN COMPILER VERSION 4.1
C             OR LATER.
C
C**********************************************************************
C
C     REFERENCES:
C
C       JOHN M. QUINN, DAVID J. KERRIDGE AND DAVID R. BARRACLOUGH,
C            WORLD MAGNETIC CHARTS FOR 1985 - SPHERICAL HARMONIC
C            MODELS OF THE GEOMAGNETIC FIELD AND ITS SECULAR
C            VARIATION, GEOPHYS. J. R. ASTR. SOC. (1986) 87,
C            PP 1143-1157
C
C       DEFENSE MAPPING AGENCY TECHNICAL REPORT, TR 8350.2:
C            DEPARTMENT OF DEFENSE WORLD GEODETIC SYSTEM 1984,
C            SEPT. 30 (1987)
C
C       JOHN M. QUINN, RACHEL J. COLEMAN, MICHAEL R. PECK, AND
C            STEPHEN E. LAUBER; THE JOINT US/UK 1990 EPOCH
C            WORLD MAGNETIC MODEL, TECHNICAL REPORT NO. 304,
C            NAVAL OCEANOGRAPHIC OFFICE (1991)
C
C       JOHN M. QUINN, RACHEL J. COLEMAN, DONALD L. SHIEL, AND
C            JOHN M. NIGRO; THE JOINT US/UK 1995 EPOCH WORLD
C            MAGNETIC MODEL, TECHNICAL REPORT NO. 314, NAVAL
C            OCEANOGRAPHIC OFFICE (1995)
C
C            SUSAN AMCMILLAN, DAVID R. BARRACLOUGH, JOHN M. QUINN, AND
C            RACHEL J. COLEMAN;  THE 1995 REVISION OF THE JOINT US/UK
C            GEOMAGNETIC FIELD MODELS - I. SECULAR VARIATION, JOURNAL OF
C            GEOMAGNETISM AND GEOELECTRICITY, VOL. 49, PP. 229-243
C            (1997)
C
C            JOHN M. QUINN, RACHEL J. COELMAN, SUSAM MACMILLAN, AND
C            DAVID R. BARRACLOUGH;  THE 1995 REVISION OF THE JOINT
C            US/UK GEOMAGNETIC FIELD MODELS: II. MAIN FIELD,JOURNAL OF
C            GEOMAGNETISM AND GEOELECTRICITY, VOL. 49, PP. 245 - 261
C            (1997)
C
C***********************************************************************
C
C     PARAMETER DESCRIPTIONS:
C
C       A      - SEMIMAJOR AXIS OF WGS-84 ELLIPSOID (KM)
C       B      - SEMIMINOR AXIS OF WGS-84 ELLIPSOID (KM)
C       RE     - MEAN RADIUS OF IAU-66 ELLIPSOID (KM)
C       SNORM  - SCHMIDT NORMALIZATION FACTORS
C       C      - GAUSS COEFFICIENTS OF MAIN GEOMAGNETIC MODEL (NT)
C       CD     - GAUSS COEFFICIENTS OF SECULAR GEOMAGNETIC MODEL (NT/YR)
C       TC     - TIME ADJUSTED GEOMAGNETIC GAUSS COEFFICIENTS (NT)
C       OTIME  - TIME ON PREVIOUS CALL TO GEOMAG (YRS)
C       OALT   - GEODETIC ALTITUDE ON PREVIOUS CALL TO GEOMAG (YRS)
C       OLAT   - GEODETIC LATITUDE ON PREVIOUS CALL TO GEOMAG (DEG.)
C       TIME   - COMPUTATION TIME (YRS)                        (INPUT)
C                (EG. 1 JULY 1995 = 1995.500)
C       ALT    - GEODETIC ALTITUDE (KM)                        (INPUT)
C       GLAT   - GEODETIC LATITUDE (DEG.)                      (INPUT)
C       GLON   - GEODETIC LONGITUDE (DEG.)                     (INPUT)
C       EPOCH  - BASE TIME OF GEOMAGNETIC MODEL (YRS)
C       DTR    - DEGREE TO RADIAN CONVERSION
C       SP(M)  - SINE OF (M*SPHERICAL COORD. LONGITUDE)
C       CP(M)  - COSINE OF (M*SPHERICAL COORD. LONGITUDE)
C       ST     - SINE OF (SPHERICAL COORD. LATITUDE)
C       CT     - COSINE OF (SPHERICAL COORD. LATITUDE)
C       R      - SPHERICAL COORDINATE RADIAL POSITION (KM)
C       CA     - COSINE OF SPHERICAL TO GEODETIC VECTOR ROTATION ANGLE
C       SA     - SINE OF SPHERICAL TO GEODETIC VECTOR ROTATION ANGLE
C       BR     - RADIAL COMPONENT OF GEOMAGNETIC FIELD (NT)
C       BT     - THETA COMPONENT OF GEOMAGNETIC FIELD (NT)
C       BP     - PHI COMPONENT OF GEOMAGNETIC FIELD (NT)
C       P(N,M) - ASSOCIATED LEGENDRE POLYNOMIALS (UNNORMALIZED)
C       PP(N)  - ASSOCIATED LEGENDRE POLYNOMIALS FOR M=1 (UNNORMALIZED)
C       DP(N,M)- THETA DERIVATIVE OF P(N,M) (UNNORMALIZED)
C       BX     - NORTH GEOMAGNETIC COMPONENT (NT)
C       BY     - EAST GEOMAGNETIC COMPONENT (NT)
C       BZ     - VERTICALLY DOWN GEOMAGNETIC COMPONENT (NT)
C       BH     - HORIZONTAL GEOMAGNETIC COMPONENT (NT)
C       DEC    - GEOMAGNETIC DECLINATION (DEG.)                (OUTPUT)
C                  EAST=POSITIVE ANGLES
C                  WEST=NEGATIVE ANGLES
C       DIP    - GEOMAGNETIC INCLINATION (DEG.)                (OUTPUT)
C                  DOWN=POSITIVE ANGLES
C                    UP=NEGATIVE ANGLES
C       TI     - GEOMAGNETIC TOTAL INTENSITY (NT)              (OUTPUT)
C       GV     - GEOMAGNETIC GRID VARIATION (DEG.)             (OUTPUT)
C                REFERENCED TO GRID NORTH
C                GRID NORTH REFERENCED TO 0 MERIDIAN
C                OF A POLAR STEREOGRAPHIC PROJECTION
C                (ARCTIC/ANTARCTIC ONLY)
C       MAXDEG - MAXIMUM DEGREE OF SPHERICAL HARMONIC MODEL    (INPUT)
C       MOXORD - MAXIMUM ORDER OF SPHERICAL HARMONIC MODEL
C
C***********************************************************************
C
C     NOTE:  THIS VERSION OF GEOMAG USES A WMM SERIES GEOMAGNETIC
C            FIELS MODEL REFERENCED TO THE WGS-84 GRAVITY MODEL
C            ELLIPSOID
C


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