/**
 ******************************************************************************
 *
 * @file       WorldMagModel.c
 * @author     The OpenPilot Team, http://www.openpilot.org Copyright (C) 2010.
 * @brief      Source file for the World Magnetic Model
 *             This is a port of code available from the US NOAA.
 *             The hard coded coefficients should be valid until 2015.
 *             Major changes include:
 *                - No geoid model (altitude must be geodetic WGS-84)
 *                - Floating point calculation (not double precision)
 *                - Hard coded coefficients for model
 *                - Elimination of user interface
 *                - Elimination of dynamic memory allocation
 *
 * @see        The GNU Public License (GPL) Version 3
 *
 *****************************************************************************/
/*
 * This program is free software; you can redistribute it and/or modify
 * it under the terms of the GNU General Public License as published by
 * the Free Software Foundation; either version 3 of the License, or
 * (at your option) any later version.
 *
 * This program is distributed in the hope that it will be useful, but
 * WITHOUT ANY WARRANTY; without even the implied warranty of MERCHANTABILITY
 * or FITNESS FOR A PARTICULAR PURPOSE. See the GNU General Public License
 * for more details.
 *
 * You should have received a copy of the GNU General Public License along
 * with this program; if not, write to the Free Software Foundation, Inc.,
 * 59 Temple Place, Suite 330, Boston, MA 02111-1307 USA
 */

// I don't want this dependency, but currently using pvPortMalloc
#include "openpilot.h"

#include <stdio.h>
#include <string.h>
#include <math.h>
#include <stdlib.h>
#include <stdint.h>

#include "WorldMagModel.h"
#include "WMMInternal.h"

static WMMtype_Ellipsoid * Ellip;
static WMMtype_MagneticModel * MagneticModel;

/**************************************************************************************
*   Example use - very simple - only two exposed functions
*
*	WMM_Initialize(); // Set default values and constants
*
*	WMM_GetMagVector(float Lat, float Lon, float Alt, uint16_t Month, uint16_t Day, uint16_t Year, float B[3]);
*	e.g. Iceland in may of 2012 = WMM_GetMagVector(65.0, -20.0, 0.0, 5, 5, 2012, B);
*	Alt is above the WGS-84 Ellipsoid
*	B is the NED (XYZ) magnetic vector in nTesla
**************************************************************************************/

int WMM_Initialize()
//	Sets default values for WMM subroutines.
//	UPDATES : Ellip and MagneticModel
{  
  // Sets WGS-84 parameters
	Ellip->a =		6378.137;			// semi-major axis of the ellipsoid in km
	Ellip->b =		6356.7523142;		// semi-minor axis of the ellipsoid in km
	Ellip->fla =		1/298.257223563;	// flattening
	Ellip->eps =		sqrt(1- (Ellip->b*Ellip->b)/(Ellip->a*Ellip->a ));  // first eccentricity
	Ellip->epssq =	(Ellip->eps*Ellip->eps);			// first eccentricity squared
	Ellip->re =		6371.2;							// Earth's radius in km

	// Sets Magnetic Model parameters
	MagneticModel->nMax = WMM_MAX_MODEL_DEGREES;
	MagneticModel->nMaxSecVar = WMM_MAX_SECULAR_VARIATION_MODEL_DEGREES;
	MagneticModel->SecularVariationUsed = 0;

	// Really, Really needs to be read from a file - out of date in 2015 at latest
	MagneticModel->EditionDate = 5.7863328170559505e-307;
	MagneticModel->epoch = 2010.0;
	sprintf(MagneticModel->ModelName, "WMM-2010");
	WMM_Set_Coeff_Array();
  return 0;
}

void WMM_GetMagVector(float Lat, float Lon, float AltEllipsoid, uint16_t Month, uint16_t Day, uint16_t Year, float B[3])
{
  char Error_Message[255];

  Ellip = (WMMtype_Ellipsoid *) pvPortMalloc(sizeof(WMMtype_Ellipsoid));
  MagneticModel = (WMMtype_MagneticModel *) pvPortMalloc(sizeof(WMMtype_MagneticModel));
  
	WMMtype_CoordSpherical * CoordSpherical = (WMMtype_CoordSpherical *) pvPortMalloc(sizeof(CoordSpherical));
	WMMtype_CoordGeodetic * CoordGeodetic = (WMMtype_CoordGeodetic *) pvPortMalloc(sizeof(CoordGeodetic));
	WMMtype_Date * Date = (WMMtype_Date *) pvPortMalloc(sizeof(WMMtype_Date));
	WMMtype_GeoMagneticElements * GeoMagneticElements = (WMMtype_GeoMagneticElements *) pvPortMalloc(sizeof(GeoMagneticElements));

  WMM_Initialize();
  
	CoordGeodetic->lambda = Lon;
	CoordGeodetic->phi = Lat;
	CoordGeodetic->HeightAboveEllipsoid  = AltEllipsoid;
	WMM_GeodeticToSpherical(CoordGeodetic, CoordSpherical);    /*Convert from geodeitic to Spherical Equations: 17-18, WMM Technical report*/
	
	Date->Month=Month;
	Date->Day=Day;
	Date->Year=Year;
  WMM_DateToYear (Date, Error_Message);
	WMM_TimelyModifyMagneticModel(Date);
	WMM_Geomag(CoordSpherical, CoordGeodetic, GeoMagneticElements);   /* Computes the geoMagnetic field elements and their time change*/
    
	B[0]=GeoMagneticElements->X;
	B[1]=GeoMagneticElements->Y;
	B[2]=GeoMagneticElements->Z;

  vPortFree(Ellip);
  vPortFree(MagneticModel);
  vPortFree(CoordSpherical);
  vPortFree(CoordGeodetic);
  vPortFree(Date);
  vPortFree(GeoMagneticElements);  
}

uint16_t WMM_Geomag( WMMtype_CoordSpherical * CoordSpherical, WMMtype_CoordGeodetic * CoordGeodetic,
                    WMMtype_GeoMagneticElements  *GeoMagneticElements)
   /*
   The main subroutine that calls a sequence of WMM sub-functions to calculate the magnetic field elements for a single point.
   The function expects the model coefficients and point coordinates as input and returns the magnetic field elements and
   their rate of change. Though, this subroutine can be called successively to calculate a time series, profile or grid
   of magnetic field, these are better achieved by the subroutine WMM_Grid.

   INPUT: Ellip
		 CoordSpherical
		 CoordGeodetic
		 TimedMagneticModel

   OUTPUT : GeoMagneticElements

   CALLS:  	WMM_ComputeSphericalHarmonicVariables( Ellip, CoordSpherical, TimedMagneticModel->nMax, &SphVariables); (Compute Spherical Harmonic variables  )
			WMM_AssociatedLegendreFunction(CoordSpherical, TimedMagneticModel->nMax, LegendreFunction);  	Compute ALF
			WMM_Summation(LegendreFunction, TimedMagneticModel, SphVariables, CoordSpherical, &MagneticResultsSph);  Accumulate the spherical harmonic coefficients
			WMM_SecVarSummation(LegendreFunction, TimedMagneticModel, SphVariables, CoordSpherical, &MagneticResultsSphVar); Sum the Secular Variation Coefficients
			WMM_RotateMagneticVector(CoordSpherical, CoordGeodetic, MagneticResultsSph, &MagneticResultsGeo); Map the computed Magnetic fields to Geodeitic coordinates
			WMM_RotateMagneticVector(CoordSpherical, CoordGeodetic, MagneticResultsSphVar, &MagneticResultsGeoVar);  Map the secular variation field components to Geodetic coordinates
			WMM_CalculateGeoMagneticElements(&MagneticResultsGeo, GeoMagneticElements);   Calculate the Geomagnetic elements
			WMM_CalculateSecularVariation(MagneticResultsGeoVar, GeoMagneticElements); Calculate the secular variation of each of the Geomagnetic elements

   */
{
	WMMtype_LegendreFunction LegendreFunction;
	WMMtype_SphericalHarmonicVariables SphVariables;
	WMMtype_MagneticResults MagneticResultsSph, MagneticResultsGeo, MagneticResultsSphVar, MagneticResultsGeoVar;

	WMM_ComputeSphericalHarmonicVariables( CoordSpherical, MagneticModel->nMax, &SphVariables); /* Compute Spherical Harmonic variables  */
	WMM_AssociatedLegendreFunction( CoordSpherical, MagneticModel->nMax, &LegendreFunction);  	/* Compute ALF  */
	WMM_Summation(&LegendreFunction, &SphVariables, CoordSpherical, &MagneticResultsSph); /* Accumulate the spherical harmonic coefficients*/
	WMM_SecVarSummation(&LegendreFunction, &SphVariables, CoordSpherical, &MagneticResultsSphVar); /*Sum the Secular Variation Coefficients  */
	WMM_RotateMagneticVector(CoordSpherical, CoordGeodetic, &MagneticResultsSph, &MagneticResultsGeo); /* Map the computed Magnetic fields to Geodeitic coordinates  */
	WMM_RotateMagneticVector(CoordSpherical, CoordGeodetic, &MagneticResultsSphVar, &MagneticResultsGeoVar); /* Map the secular variation field components to Geodetic coordinates*/
	WMM_CalculateGeoMagneticElements(&MagneticResultsGeo, GeoMagneticElements);   /* Calculate the Geomagnetic elements, Equation 18 , WMM Technical report */
	WMM_CalculateSecularVariation(&MagneticResultsGeoVar, GeoMagneticElements); /*Calculate the secular variation of each of the Geomagnetic elements*/
  return TRUE;
}


uint16_t WMM_ComputeSphericalHarmonicVariables(WMMtype_CoordSpherical *CoordSpherical, uint16_t nMax, WMMtype_SphericalHarmonicVariables *SphVariables)

   /* Computes Spherical variables
	  Variables computed are (a/r)^(n+2), cos_m(lamda) and sin_m(lambda) for spherical harmonic
	  summations. (Equations 10-12 in the WMM Technical Report)
	  INPUT   Ellip  data  structure with the following elements
				float a; semi-major axis of the ellipsoid
				float b; semi-minor axis of the ellipsoid
				float fla;  flattening
				float epssq; first eccentricity squared
				float eps;  first eccentricity
				float re; mean radius of  ellipsoid
			CoordSpherical 	A data structure with the following elements
				float lambda; ( longitude)
				float phig; ( geocentric latitude )
				float r;  	  ( distance from the center of the ellipsoid)
			nMax   integer 	 ( Maxumum degree of spherical harmonic secular model)\

	OUTPUT  SphVariables  Pointer to the   data structure with the following elements
		float RelativeRadiusPower[WMM_MAX_MODEL_DEGREES+1];   [earth_reference_radius_km  sph. radius ]^n
		float cos_mlambda[WMM_MAX_MODEL_DEGREES+1]; cp(m)  - cosine of (mspherical coord. longitude)
		float sin_mlambda[WMM_MAX_MODEL_DEGREES+1];  sp(m)  - sine of (mspherical coord. longitude)
	CALLS : none
	  */

	{
	float cos_lambda, sin_lambda;
	uint16_t m, n;
	cos_lambda = cos(DEG2RAD(CoordSpherical->lambda));
	sin_lambda = sin(DEG2RAD(CoordSpherical->lambda));
	/* for n = 0 ... model_order, compute (Radius of Earth / Spherica radius r)^(n+2)
	for n  1..nMax-1 (this is much faster than calling pow MAX_N+1 times).      */
	SphVariables->RelativeRadiusPower[0] = (Ellip->re / CoordSpherical->r) * (Ellip->re / CoordSpherical->r);
	for (n = 1; n <= nMax; n++)
	{
		SphVariables->RelativeRadiusPower[n] = SphVariables->RelativeRadiusPower[n-1] * (Ellip->re  / CoordSpherical->r);
	}

  /*
   Compute cos(m*lambda), sin(m*lambda) for m = 0 ... nMax
	 cos(a + b) = cos(a)*cos(b) - sin(a)*sin(b)
	 sin(a + b) = cos(a)*sin(b) + sin(a)*cos(b)
  */
	SphVariables->cos_mlambda[0] = 1.0;
	SphVariables->sin_mlambda[0] = 0.0;

	SphVariables->cos_mlambda[1] = cos_lambda;
	SphVariables->sin_mlambda[1] = sin_lambda;
	for (m = 2; m <= nMax; m++)
	{
		SphVariables->cos_mlambda[m] = SphVariables->cos_mlambda[m-1]*cos_lambda - SphVariables->sin_mlambda[m-1]*sin_lambda;
		SphVariables->sin_mlambda[m] = SphVariables->cos_mlambda[m-1]*sin_lambda + SphVariables->sin_mlambda[m-1]*cos_lambda;
	}
	return TRUE;
	}  /*WMM_ComputeSphericalHarmonicVariables*/


uint16_t WMM_AssociatedLegendreFunction(WMMtype_CoordSpherical * CoordSpherical, uint16_t nMax, WMMtype_LegendreFunction *LegendreFunction)

	/* Computes  all of the Schmidt-semi normalized associated Legendre
	functions up to degree nMax. If nMax <= 16, function WMM_PcupLow is used.
	Otherwise WMM_PcupHigh is called.
	INPUT  CoordSpherical 	A data structure with the following elements
							float lambda; ( longitude)
							float phig; ( geocentric latitude )
							float r;  	  ( distance from the center of the ellipsoid)
			nMax        	integer 	 ( Maxumum degree of spherical harmonic secular model)
			LegendreFunction Pointer to data structure with the following elements
							float *Pcup;  (  pointer to store Legendre Function  )
							float *dPcup; ( pointer to store  Derivative of Lagendre function )

	OUTPUT  LegendreFunction  Calculated Legendre variables in the data structure

	 */

	{
	float sin_phi;
	uint16_t FLAG = 1;

	sin_phi =  sin ( DEG2RAD ( CoordSpherical->phig ) );       /* sin  (geocentric latitude) */

	if (nMax <= 16 || (1 - fabs(sin_phi)) < 1.0e-10 ) 	/* If nMax is less tha 16 or at the poles */
		FLAG = WMM_PcupLow(LegendreFunction->Pcup,LegendreFunction->dPcup,sin_phi, nMax);
	else FLAG = WMM_PcupHigh(LegendreFunction->Pcup,LegendreFunction->dPcup,sin_phi, nMax);
	if (FLAG == 0) /* Error while computing  Legendre variables*/
			return FALSE;


	return TRUE;
	} /*WMM_AssociatedLegendreFunction */

uint16_t WMM_Summation(WMMtype_LegendreFunction *LegendreFunction, WMMtype_SphericalHarmonicVariables * SphVariables, WMMtype_CoordSpherical * CoordSpherical, WMMtype_MagneticResults *MagneticResults)
{
	/* Computes Geomagnetic Field Elements X, Y and Z in Spherical coordinate system using
	spherical harmonic summation.


	The vector Magnetic field is given by -grad V, where V is Geomagnetic scalar potential
	The gradient in spherical coordinates is given by:

			 dV ^     1 dV ^        1     dV ^
	grad V = -- r  +  - -- t  +  -------- -- p
			 dr       r dt       r sin(t) dp


	INPUT :  LegendreFunction
			MagneticModel
			SphVariables
			CoordSpherical
	OUTPUT : MagneticResults

	CALLS : WMM_SummationSpecial



   Manoj Nair, June, 2009 Manoj.C.Nair@Noaa.Gov
   */
	uint16_t m, n, index;
	float cos_phi;
	MagneticResults->Bz = 0.0;
	MagneticResults->By = 0.0;
	MagneticResults->Bx = 0.0;
	for (n = 1; n <=  MagneticModel->nMax; n++)
	{
		for (m=0;m<=n;m++)
		{
			index = (n * (n + 1) / 2 + m);

/*		    nMax  	(n+2) 	  n     m            m           m
	Bz =   -SUM (a/r)   (n+1) SUM  [g cos(m p) + h sin(m p)] P (sin(phi))
			n=1      	      m=0   n            n           n  */
/* Equation 12 in the WMM Technical report.  Derivative with respect to radius.*/
			MagneticResults->Bz -= 	SphVariables->RelativeRadiusPower[n] *
					(	MagneticModel->Main_Field_Coeff_G[index]*SphVariables->cos_mlambda[m] +
						MagneticModel->Main_Field_Coeff_H[index]*SphVariables->sin_mlambda[m]	)
						* (float) (n+1) * LegendreFunction-> Pcup[index];

/*		  1 nMax  (n+2)    n     m            m           m
	By =    SUM (a/r) (m)  SUM  [g cos(m p) + h sin(m p)] dP (sin(phi))
		   n=1             m=0   n            n           n  */
/* Equation 11 in the WMM Technical report. Derivative with respect to longitude, divided by radius. */
			MagneticResults->By += 	SphVariables->RelativeRadiusPower[n] *
					(	MagneticModel->Main_Field_Coeff_G[index]*SphVariables->sin_mlambda[m] -
						MagneticModel->Main_Field_Coeff_H[index]*SphVariables->cos_mlambda[m]  )
						* (float) (m) * LegendreFunction-> Pcup[index];
/*		   nMax  (n+2) n     m            m           m
	Bx = - SUM (a/r)   SUM  [g cos(m p) + h sin(m p)] dP (sin(phi))
		   n=1         m=0   n            n           n  */
/* Equation 10  in the WMM Technical report. Derivative with respect to latitude, divided by radius. */

			MagneticResults->Bx -= 	SphVariables->RelativeRadiusPower[n] *
					(	MagneticModel->Main_Field_Coeff_G[index]*SphVariables->cos_mlambda[m]  +
						MagneticModel->Main_Field_Coeff_H[index]*SphVariables->sin_mlambda[m]  )
						* LegendreFunction-> dPcup[index];



		}
	}

	cos_phi = cos ( DEG2RAD ( CoordSpherical->phig ) );
	if ( fabs(cos_phi) > 1.0e-10 )
	{
		MagneticResults->By = MagneticResults->By / cos_phi ;
	}
	else
	/* Special calculation for component - By - at Geographic poles.
	* If the user wants to avoid using this function,  please make sure that
	* the latitude is not exactly +/-90. An option is to make use the function
	* WMM_CheckGeographicPoles.
	*/

	{
		WMM_SummationSpecial(SphVariables, CoordSpherical, MagneticResults);
	}
	return TRUE;
}/*WMM_Summation */

uint16_t WMM_SecVarSummation(WMMtype_LegendreFunction *LegendreFunction, WMMtype_SphericalHarmonicVariables * SphVariables, WMMtype_CoordSpherical * CoordSpherical, WMMtype_MagneticResults *MagneticResults)
{
	/*This Function sums the secular variation coefficients to get the secular variation of the Magnetic vector.
	INPUT :  LegendreFunction
			MagneticModel
			SphVariables
			CoordSpherical
	OUTPUT : MagneticResults

	CALLS : WMM_SecVarSummationSpecial

	*/
	uint16_t m, n, index;
	float cos_phi;
	MagneticModel->SecularVariationUsed = TRUE;
	MagneticResults->Bz = 0.0;
	MagneticResults->By = 0.0;
	MagneticResults->Bx = 0.0;
	for (n = 1; n <=  MagneticModel->nMaxSecVar; n++)
	{
		for (m=0;m<=n;m++)
		{
			index = (n * (n + 1) / 2 + m);

/*		    nMax  	(n+2) 	  n     m            m           m
	Bz =   -SUM (a/r)   (n+1) SUM  [g cos(m p) + h sin(m p)] P (sin(phi))
			n=1      	      m=0   n            n           n  */
/*  Derivative with respect to radius.*/
			MagneticResults->Bz -= 	SphVariables->RelativeRadiusPower[n] *
					(	MagneticModel->Secular_Var_Coeff_G[index]*SphVariables->cos_mlambda[m] +
						MagneticModel->Secular_Var_Coeff_H[index]*SphVariables->sin_mlambda[m]	)
						* (float) (n+1) * LegendreFunction-> Pcup[index];

/*		  1 nMax  (n+2)    n     m            m           m
	By =    SUM (a/r) (m)  SUM  [g cos(m p) + h sin(m p)] dP (sin(phi))
		   n=1             m=0   n            n           n  */
/* Derivative with respect to longitude, divided by radius. */
			MagneticResults->By += 	SphVariables->RelativeRadiusPower[n] *
					(	MagneticModel->Secular_Var_Coeff_G[index]*SphVariables->sin_mlambda[m] -
						MagneticModel->Secular_Var_Coeff_H[index]*SphVariables->cos_mlambda[m]  )
						* (float) (m) * LegendreFunction-> Pcup[index];
/*		   nMax  (n+2) n     m            m           m
	Bx = - SUM (a/r)   SUM  [g cos(m p) + h sin(m p)] dP (sin(phi))
		   n=1         m=0   n            n           n  */
/* Derivative with respect to latitude, divided by radius. */

			MagneticResults->Bx -= 	SphVariables->RelativeRadiusPower[n] *
					(	MagneticModel->Secular_Var_Coeff_G[index]*SphVariables->cos_mlambda[m]  +
						MagneticModel->Secular_Var_Coeff_H[index]*SphVariables->sin_mlambda[m]  )
						* LegendreFunction-> dPcup[index];
		}
	}
	cos_phi = cos ( DEG2RAD ( CoordSpherical->phig ) );
	if ( fabs(cos_phi) > 1.0e-10 )
	{
		MagneticResults->By = MagneticResults->By / cos_phi ;
	}
	else
	/* Special calculation for component By at Geographic poles */
	{
		WMM_SecVarSummationSpecial(SphVariables, CoordSpherical, MagneticResults);
	}
	return TRUE;
} /*WMM_SecVarSummation*/

uint16_t WMM_RotateMagneticVector(WMMtype_CoordSpherical * CoordSpherical, WMMtype_CoordGeodetic * CoordGeodetic, WMMtype_MagneticResults * MagneticResultsSph, WMMtype_MagneticResults *MagneticResultsGeo)
	/* Rotate the Magnetic Vectors to Geodetic Coordinates
	Manoj Nair, June, 2009 Manoj.C.Nair@Noaa.Gov
	Equation 16, WMM Technical report

	INPUT : CoordSpherical : Data structure WMMtype_CoordSpherical with the following elements
				float lambda; ( longitude)
				float phig; ( geocentric latitude )
				float r;  	  ( distance from the center of the ellipsoid)

			CoordGeodetic : Data structure WMMtype_CoordGeodetic with the following elements
				float lambda; (longitude)
				float phi; ( geodetic latitude)
				float HeightAboveEllipsoid; (height above the ellipsoid (HaE) )
				float HeightAboveGeoid;(height above the Geoid )

			MagneticResultsSph : Data structure WMMtype_MagneticResults with the following elements
				float Bx;     North
				float By;	   East
				float Bz;    Down

	OUTPUT: MagneticResultsGeo Pointer to the data structure WMMtype_MagneticResults, with the following elements
				float Bx;     North
				float By;	   East
				float Bz;    Down

	CALLS : none

	*/
	{
	float  Psi;
		 /* Difference between the spherical and Geodetic latitudes */
	Psi =  ( M_PI/180 ) * ( CoordSpherical->phig - CoordGeodetic->phi );

		 /* Rotate spherical field components to the Geodeitic system */
		MagneticResultsGeo->Bz =     MagneticResultsSph->Bx *  sin(Psi) + MagneticResultsSph->Bz * cos(Psi);
		MagneticResultsGeo->Bx =     MagneticResultsSph->Bx *  cos(Psi) - MagneticResultsSph->Bz * sin(Psi);
		MagneticResultsGeo->By =     MagneticResultsSph->By;
	return TRUE;
	}   /*WMM_RotateMagneticVector*/

uint16_t WMM_CalculateGeoMagneticElements(WMMtype_MagneticResults *MagneticResultsGeo, WMMtype_GeoMagneticElements *GeoMagneticElements)

	/* Calculate all the Geomagnetic elements from X,Y and Z components
	INPUT     MagneticResultsGeo   Pointer to data structure with the following elements
				float Bx;    ( North )
				float By;	  ( East )
				float Bz;    ( Down )
	OUTPUT    GeoMagneticElements    Pointer to data structure with the following elements
				float Decl; (Angle between the magnetic field vector and true north, positive east)
				float Incl; Angle between the magnetic field vector and the horizontal plane, positive down
				float F; Magnetic Field Strength
				float H; Horizontal Magnetic Field Strength
				float X; Northern component of the magnetic field vector
				float Y; Eastern component of the magnetic field vector
				float Z; Downward component of the magnetic field vector
	CALLS : none
	*/
	{
	GeoMagneticElements->X = MagneticResultsGeo->Bx;
	GeoMagneticElements->Y = MagneticResultsGeo->By;
	GeoMagneticElements->Z = MagneticResultsGeo->Bz;

	GeoMagneticElements->H = sqrt (MagneticResultsGeo->Bx* MagneticResultsGeo->Bx + MagneticResultsGeo->By * MagneticResultsGeo->By);
	GeoMagneticElements->F = sqrt (GeoMagneticElements->H*GeoMagneticElements->H + MagneticResultsGeo->Bz * MagneticResultsGeo->Bz);
	GeoMagneticElements->Decl = RAD2DEG(atan2 (GeoMagneticElements->Y , GeoMagneticElements->X));
	GeoMagneticElements->Incl = RAD2DEG(atan2 (GeoMagneticElements->Z , GeoMagneticElements->H));

	return TRUE;
	}  /*WMM_CalculateGeoMagneticElements */

uint16_t WMM_CalculateSecularVariation(WMMtype_MagneticResults * MagneticVariation, WMMtype_GeoMagneticElements *MagneticElements)
/*This takes the Magnetic Variation in x, y, and z and uses it to calculate the secular variation of each of the Geomagnetic elements.
	INPUT     MagneticVariation   Data structure with the following elements
				float Bx;    ( North )
				float By;	  ( East )
				float Bz;    ( Down )
	OUTPUT   MagneticElements   Pointer to the data  structure with the following elements updated
			float Decldot; Yearly Rate of change in declination
			float Incldot; Yearly Rate of change in inclination
			float Fdot; Yearly rate of change in Magnetic field strength
			float Hdot; Yearly rate of change in horizontal field strength
			float Xdot; Yearly rate of change in the northern component
			float Ydot; Yearly rate of change in the eastern component
			float Zdot; Yearly rate of change in the downward component
			float GVdot;Yearly rate of chnage in grid variation
	CALLS : none

*/
{
	MagneticElements->Xdot = MagneticVariation->Bx;
	MagneticElements->Ydot = MagneticVariation->By;
	MagneticElements->Zdot = MagneticVariation->Bz;
	MagneticElements->Hdot = (MagneticElements->X * MagneticElements->Xdot + MagneticElements->Y * MagneticElements->Ydot) / MagneticElements->H; //See equation 19 in the WMM technical report
	MagneticElements->Fdot = (MagneticElements->X * MagneticElements->Xdot + MagneticElements->Y * MagneticElements->Ydot + MagneticElements->Z * MagneticElements->Zdot) / MagneticElements->F;
	MagneticElements->Decldot = 180.0 / M_PI * (MagneticElements->X * MagneticElements->Ydot - MagneticElements->Y * MagneticElements->Xdot) / (MagneticElements->H * MagneticElements->H);
	MagneticElements->Incldot = 180.0 / M_PI * (MagneticElements->H * MagneticElements->Zdot - MagneticElements->Z * MagneticElements->Hdot) / (MagneticElements->F * MagneticElements->F);
	MagneticElements->GVdot = MagneticElements->Decldot;
	return TRUE;
} /*WMM_CalculateSecularVariation*/

uint16_t WMM_PcupHigh(float *Pcup, float *dPcup, float x, uint16_t nMax)

/*	This function evaluates all of the Schmidt-semi normalized associated Legendre
	functions up to degree nMax. The functions are initially scaled by
	10^280 sin^m in order to minimize the effects of underflow at large m
	near the poles (see Holmes and Featherstone 2002, J. Geodesy, 76, 279-299).
	Note that this function performs the same operation as WMM_PcupLow.
	However this function also can be used for high degree (large nMax) models.

	Calling Parameters:
		INPUT
			nMax:	 Maximum spherical harmonic degree to compute.
			x:		cos(colatitude) or sin(latitude).

		OUTPUT
			Pcup:	A vector of all associated Legendgre polynomials evaluated at
					x up to nMax. The lenght must by greater or equal to (nMax+1)*(nMax+2)/2.
		  dPcup:   Derivative of Pcup(x) with respect to latitude

		CALLS : none
	Notes:



  Adopted from the FORTRAN code written by Mark Wieczorek September 25, 2005.

  Manoj Nair, Nov, 2009 Manoj.C.Nair@Noaa.Gov

  Change from the previous version
  The prevous version computes the derivatives as
  dP(n,m)(x)/dx, where x = sin(latitude) (or cos(colatitude) ).
  However, the WMM Geomagnetic routines requires dP(n,m)(x)/dlatitude.
  Hence the derivatives are multiplied by sin(latitude).
  Removed the options for CS phase and normalizations.

  Note: In geomagnetism, the derivatives of ALF are usually found with
  respect to the colatitudes. Here the derivatives are found with respect
  to the latitude. The difference is a sign reversal for the derivative of
  the Associated Legendre Functions.

  The derivates can't be computed for latitude = |90| degrees.
	*/
	{
	float  pm2, pm1, pmm, plm, rescalem, z, scalef;
	float f1[NUMPCUP], f2[NUMPCUP], PreSqr[NUMPCUP];
	uint16_t k, kstart, m, n;

	if (fabs(x) == 1.0)
	{
	  // printf("Error in PcupHigh: derivative cannot be calculated at poles\n");
	  return FALSE;
	}

	scalef = 1.0e-280;

	for(n = 0 ; n <= 2*nMax+1 ; ++n )
	{
		PreSqr[n] = sqrt((float)(n));
	}

	k = 2;

	for(n=2 ; n<=nMax ; n++)
	{
		k = k + 1;
		f1[k] = (float)(2*n-1) /(float)(n);
		f2[k] = (float)(n-1) /(float)(n);
		for(m=1 ; m<=n-2 ; m++)
		{
			k = k+1;
			f1[k] = (float)(2*n-1) / PreSqr[n+m] / PreSqr[n-m];
			f2[k] = PreSqr[n-m-1] * PreSqr[n+m-1] / PreSqr[n+m] / PreSqr[n-m];
		}
		k = k + 2;
	}

	/*z = sin (geocentric latitude) */
	z = sqrt((1.0-x)*(1.0+x));
	pm2  = 1.0;
	Pcup[0] = 1.0;
	dPcup[0] = 0.0;
	if (nMax == 0)
		return FALSE;
	pm1  		= x;
	Pcup[1] 	= pm1;
	dPcup[1] 	= z;
	k = 1;

	for(n = 2; n <= nMax; n++ )
	{
		k = k+n;
		plm = f1[k]*x*pm1-f2[k]*pm2;
		Pcup[k] = plm;
		dPcup[k] = (float)(n) * (pm1 - x * plm) / z;
		pm2  = pm1;
		pm1  = plm;
	}

	pmm = PreSqr[2]*scalef;
	rescalem = 1.0/scalef;
	kstart = 0;

	for(m = 1; m <= nMax - 1; ++m)
	{
		rescalem = rescalem*z;

		/* Calculate Pcup(m,m)*/
		kstart = kstart+m+1;
		pmm =  pmm * PreSqr[2*m+1] / PreSqr[2*m];
		Pcup[kstart] = pmm*rescalem / PreSqr[2*m+1];
		dPcup[kstart] = -((float)(m) * x * Pcup[kstart] / z);
		pm2 = pmm/PreSqr[2*m+1];
		/* Calculate Pcup(m+1,m)*/
		k = kstart+m+1 ;
		pm1 = x * PreSqr[2*m+1] * pm2;
		Pcup[k] = pm1*rescalem;
		dPcup[k] =   ((pm2*rescalem) * PreSqr[2*m+1] - x * (float)(m+1) * Pcup[k]) / z;
		/* Calculate Pcup(n,m)*/
		for(n = m+2; n <= nMax; ++n)
		{
			k = k+n;
			plm  = x*f1[k]*pm1-f2[k]*pm2;
			Pcup[k] = plm*rescalem;
			dPcup[k] = (PreSqr[n+m] * PreSqr[n-m] * (pm1 * rescalem) - (float)(n) * x * Pcup[k] ) / z;
			pm2  = pm1;
			pm1  = plm;
		}
	}

	/* Calculate Pcup(nMax,nMax)*/
	rescalem = rescalem*z;
	kstart = kstart+m+1;
	pmm =  pmm  / PreSqr[2*nMax];
	Pcup[kstart] = pmm * rescalem;
	dPcup[kstart] = -(float)(nMax) * x * Pcup[kstart] / z;

	return TRUE ;
} /* WMM_PcupHigh */

uint16_t WMM_PcupLow( float *Pcup, float *dPcup, float x, uint16_t nMax)

/*   This function evaluates all of the Schmidt-semi normalized associated Legendre
	functions up to degree nMax.

	Calling Parameters:
		INPUT
			nMax:	 Maximum spherical harmonic degree to compute.
			x:		cos(colatitude) or sin(latitude).

		OUTPUT
			Pcup:	A vector of all associated Legendgre polynomials evaluated at
					x up to nMax.
		   dPcup: Derivative of Pcup(x) with respect to latitude

	Notes: Overflow may occur if nMax > 20 , especially for high-latitudes.
	Use WMM_PcupHigh for large nMax.

   Writted by Manoj Nair, June, 2009 . Manoj.C.Nair@Noaa.Gov.

  Note: In geomagnetism, the derivatives of ALF are usually found with
  respect to the colatitudes. Here the derivatives are found with respect
  to the latitude. The difference is a sign reversal for the derivative of
  the Associated Legendre Functions.
*/
{
	uint16_t n, m, index, index1, index2;
	float k, z, schmidtQuasiNorm[NUMPCUP];
	Pcup[0] = 1.0;
	dPcup[0] = 0.0;
		/*sin (geocentric latitude) - sin_phi */
	z = sqrt( ( 1.0 - x ) * ( 1.0 + x ) ) ;

	/*	 First,	Compute the Gauss-normalized associated Legendre  functions*/
	for (n = 1; n <=  nMax; n++)
	{
		for (m=0;m<=n;m++)
		{
		index = (n * (n + 1) / 2 + m);
			if (n == m)
			{
				index1 = ( n - 1 ) * n / 2 + m -1;
				Pcup [index]  = z * Pcup[index1];
				dPcup[index] = z *  dPcup[index1] + x *  Pcup[index1];
			}
			else if (n == 1 && m == 0)
			{
				index1 = ( n - 1 ) * n / 2 + m;
				Pcup[index]  = x *  Pcup[index1];
				dPcup[index] = x *  dPcup[index1] - z *  Pcup[index1];
			}
			else if (n > 1 && n != m)
			{
				index1 = ( n - 2 ) * ( n - 1 ) / 2 + m;
				index2 = ( n - 1) * n / 2 + m;
				if (m > n - 2)
				{
					Pcup[index]  = x *  Pcup[index2];
					dPcup[index] = x *  dPcup[index2] - z *  Pcup[index2];
				}
				else
				{
					k = (float)( ( ( n - 1 ) * ( n - 1 ) ) - ( m * m ) ) / ( float ) ( ( 2 * n - 1 ) * ( 2 * n - 3 ) );
					Pcup[index]  = x *  Pcup[index2]  - k  *  Pcup[index1];
					dPcup[index] = x *  dPcup[index2] - z *  Pcup[index2] - k *  dPcup[index1];
				}
			}
		}
	}
/*Compute the ration between the Gauss-normalized associated Legendre
  functions and the Schmidt quasi-normalized version. This is equivalent to
  sqrt((m==0?1:2)*(n-m)!/(n+m!))*(2n-1)!!/(n-m)!  */

	schmidtQuasiNorm[0] = 1.0;
	for (n = 1; n <= nMax; n++)
	{
		index = (n * (n + 1) / 2);
		index1 = (n - 1)  * n / 2 ;
		/* for m = 0 */
		schmidtQuasiNorm[index] =  schmidtQuasiNorm[index1] * (float) (2 * n - 1) / (float) n;

		for ( m = 1; m <= n; m++)
		{
			index = (n * (n + 1) / 2 + m);
			index1 = (n * (n + 1) / 2 + m - 1);
			schmidtQuasiNorm[index] = schmidtQuasiNorm[index1] * sqrt( (float) ((n - m + 1) * (m == 1 ? 2 : 1)) / (float) (n + m));
		}

	}

/* Converts the  Gauss-normalized associated Legendre
	  functions to the Schmidt quasi-normalized version using pre-computed
	  relation stored in the variable schmidtQuasiNorm */

	for (n = 1; n <=  nMax; n++)
	{
		for (m=0;m<=n;m++)
		{
			 index = (n * (n + 1) / 2 + m);
			 Pcup[index]  = Pcup[index]  *  schmidtQuasiNorm[index];
			 dPcup[index] =  - dPcup[index] *  schmidtQuasiNorm[index];
			 /* The sign is changed since the new WMM routines use derivative with respect to latitude
			 insted of co-latitude */
		}
	}

	return TRUE;
}   /*WMM_PcupLow */


uint16_t WMM_SummationSpecial(WMMtype_SphericalHarmonicVariables * SphVariables, WMMtype_CoordSpherical * CoordSpherical, WMMtype_MagneticResults *MagneticResults)
	/* Special calculation for the component By at Geographic poles.
	Manoj Nair, June, 2009 manoj.c.nair@noaa.gov
    INPUT: MagneticModel
		   SphVariables
		   CoordSpherical
	OUTPUT: MagneticResults
	CALLS : none
	See Section 1.4, "SINGULARITIES AT THE GEOGRAPHIC POLES", WMM Technical report

	*/
	{
	uint16_t n, index;
	float k, sin_phi, PcupS[NUMPCUPS], schmidtQuasiNorm1, schmidtQuasiNorm2, schmidtQuasiNorm3;

	PcupS[0] = 1;
	schmidtQuasiNorm1 = 1.0;

	MagneticResults->By = 0.0;
	sin_phi = sin ( DEG2RAD ( CoordSpherical->phig ) );

	for (n = 1; n <=  MagneticModel->nMax; n++)
	{

	/*Compute the ration between the Gauss-normalized associated Legendre
  functions and the Schmidt quasi-normalized version. This is equivalent to
  sqrt((m==0?1:2)*(n-m)!/(n+m!))*(2n-1)!!/(n-m)!  */

		index = (n * (n + 1) / 2 + 1);
		schmidtQuasiNorm2 = schmidtQuasiNorm1 * (float) (2 * n - 1) / (float) n;
		schmidtQuasiNorm3 = schmidtQuasiNorm2 *  sqrt( (float) (n * 2) / (float) (n + 1));
		schmidtQuasiNorm1 = schmidtQuasiNorm2;
		if (n == 1)
		{
			PcupS[n] = PcupS[n-1];
		}
		else
		{
			k = (float)( ( (n - 1) * (n - 1) ) - 1) / ( float ) ( (2 * n - 1) * (2 * n - 3) );
			PcupS[n] =     sin_phi * PcupS[n-1] - k * PcupS[n-2];
		}

/*		  1 nMax  (n+2)    n     m            m           m
	By =    SUM (a/r) (m)  SUM  [g cos(m p) + h sin(m p)] dP (sin(phi))
		   n=1             m=0   n            n           n  */
/* Equation 11 in the WMM Technical report. Derivative with respect to longitude, divided by radius. */

		MagneticResults->By += 	SphVariables->RelativeRadiusPower[n] *
					(	MagneticModel->Main_Field_Coeff_G[index]*SphVariables->sin_mlambda[1] -
						MagneticModel->Main_Field_Coeff_H[index]*SphVariables->cos_mlambda[1]  )
						*  PcupS[n] * schmidtQuasiNorm3;
	}

	return TRUE;
	}/*WMM_SummationSpecial */

uint16_t WMM_SecVarSummationSpecial(WMMtype_SphericalHarmonicVariables * SphVariables, WMMtype_CoordSpherical * CoordSpherical, WMMtype_MagneticResults *MagneticResults)
{
	/*Special calculation for the secular variation summation at the poles.


	INPUT: MagneticModel
		   SphVariables
		   CoordSpherical
	OUTPUT: MagneticResults
	CALLS : none


	*/
	uint16_t n, index;
	float k, sin_phi, PcupS[NUMPCUPS], schmidtQuasiNorm1, schmidtQuasiNorm2, schmidtQuasiNorm3;

	PcupS[0] = 1;
	schmidtQuasiNorm1 = 1.0;

	MagneticResults->By = 0.0;
	sin_phi = sin ( DEG2RAD ( CoordSpherical->phig ) );

	for (n = 1; n <=  MagneticModel->nMaxSecVar; n++)
	{
		index = (n * (n + 1) / 2 + 1);
		schmidtQuasiNorm2 = schmidtQuasiNorm1 * (float) (2 * n - 1) / (float) n;
		schmidtQuasiNorm3 = schmidtQuasiNorm2 *  sqrt( (float) (n * 2) / (float) (n + 1));
		schmidtQuasiNorm1 = schmidtQuasiNorm2;
		if (n == 1)
		{
			PcupS[n] = PcupS[n-1];
		}
		else
		{
			k = (float)( ( (n - 1) * (n - 1) ) - 1) / ( float ) ( (2 * n - 1) * (2 * n - 3) );
			PcupS[n] =     sin_phi * PcupS[n-1] - k * PcupS[n-2];
		}

/*		  1 nMax  (n+2)    n     m            m           m
	By =    SUM (a/r) (m)  SUM  [g cos(m p) + h sin(m p)] dP (sin(phi))
		   n=1             m=0   n            n           n  */
/* Derivative with respect to longitude, divided by radius. */

		MagneticResults->By += 	SphVariables->RelativeRadiusPower[n] *
					(	MagneticModel->Secular_Var_Coeff_G[index]*SphVariables->sin_mlambda[1] -
						MagneticModel->Secular_Var_Coeff_H[index]*SphVariables->cos_mlambda[1]  )
						*  PcupS[n] * schmidtQuasiNorm3;
	}

	return TRUE;
}/*SecVarSummationSpecial*/


void WMM_TimelyModifyMagneticModel(WMMtype_Date * UserDate)
// Time change the Model coefficients from the base year of the model using secular variation coefficients.
//
// Modified to work on the global data structure to reduce memory footprint
{
	uint16_t n, m, index, a, b;
	
	a = MagneticModel->nMaxSecVar;
	b = (a * (a + 1) / 2 + a);
	for (n = 1; n <=  MagneticModel->nMax; n++)
	{
		for (m=0;m<=n;m++)
		{
			index = (n * (n + 1) / 2 + m);
			if(index <= b)
			{
				MagneticModel->Main_Field_Coeff_H[index]   +=  (UserDate->DecimalYear - MagneticModel->epoch) * MagneticModel->Secular_Var_Coeff_H[index];
				MagneticModel->Main_Field_Coeff_G[index]   +=  (UserDate->DecimalYear - MagneticModel->epoch) * MagneticModel->Secular_Var_Coeff_G[index];
			}
		}
	}
} /* WMM_TimelyModifyMagneticModel */

uint16_t WMM_DateToYear (WMMtype_Date *CalendarDate, char *Error)
// Converts a given calendar date into a decimal year
{
	uint16_t temp = 0;    // Total number of days
	uint16_t MonthDays[13] = {0, 31, 28, 31, 30, 31, 30, 31, 31, 30, 31, 30, 31};
	uint16_t ExtraDay = 0;
	uint16_t i;
    
	if((CalendarDate->Year%4 == 0 && CalendarDate->Year%100 != 0) || CalendarDate->Year%400 == 0)
		ExtraDay=1;
	MonthDays[2] += ExtraDay;

	/******************Validation********************************/
	if(CalendarDate->Month <= 0 || CalendarDate->Month > 12)
	{
		strcpy(Error, "\nError: The Month entered is invalid, valid months are '1 to 12'\n");
		return 0;
	}
	if(CalendarDate->Day <= 0 || CalendarDate->Day > MonthDays[CalendarDate->Month])
	{
		// printf("\nThe number of days in month %d is %d\n", CalendarDate->Month, MonthDays[CalendarDate->Month]);
		strcpy(Error, "\nError: The day entered is invalid\n");
		return 0;
	}
	/****************Calculation of t***************************/
	for(i = 1; i <= CalendarDate->Month; i++)
		temp+=MonthDays[i-1];
	temp+=CalendarDate->Day;
	CalendarDate->DecimalYear = CalendarDate->Year + (temp-1)/(365.0 + ExtraDay);

	return 1;
}  /*WMM_DateToYear*/

void WMM_GeodeticToSpherical(WMMtype_CoordGeodetic *CoordGeodetic, WMMtype_CoordSpherical *CoordSpherical)
// Converts Geodetic coordinates to Spherical coordinates
// Convert geodetic coordinates, (defined by the WGS-84
// reference ellipsoid), to Earth Centered Earth Fixed Cartesian
// coordinates, and then to spherical coordinates.
{
	float CosLat, SinLat, rc, xp, zp; // all local variables

	CosLat = cos(DEG2RAD(CoordGeodetic->phi));
	SinLat = sin(DEG2RAD(CoordGeodetic->phi));

	// compute the local radius of curvature on the WGS-84 reference ellipsoid
	rc = Ellip->a / sqrt(1.0 - Ellip->epssq * SinLat * SinLat);

	// compute ECEF Cartesian coordinates of specified point (for longitude=0)

	xp = (rc + CoordGeodetic->HeightAboveEllipsoid) * CosLat;
	zp = (rc*(1.0 - Ellip->epssq) + CoordGeodetic->HeightAboveEllipsoid) * SinLat;

	// compute spherical radius and angle lambda and phi of specified point

	CoordSpherical->r = sqrt(xp * xp + zp * zp);
	CoordSpherical->phig = RAD2DEG(asin(zp / CoordSpherical->r));    // geocentric latitude
	CoordSpherical->lambda = CoordGeodetic->lambda;                   // longitude

}// WMM_GeodeticToSpherical

void WMM_Set_Coeff_Array()
{
  // const should hopefully keep them in the flash region
	static const float CoeffFile[91][6] = 
	{{0, 0, 0, 0, 0, 0},
	{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}};

  // TODO: If this works here, delete first two columns to save space
	for(uint16_t i=0; i<NUMTERMS; i++){
    MagneticModel->Main_Field_Coeff_G[i]=CoeffFile[i][2];
    MagneticModel->Main_Field_Coeff_H[i]=CoeffFile[i][3];
    MagneticModel->Secular_Var_Coeff_G[i]=CoeffFile[i][4];
    MagneticModel->Secular_Var_Coeff_H[i]=CoeffFile[i][5];
  }
  
}
