AP_Math: split out double precision location functions

this allows ALLOW_DOUBLE_MATH_FUNCTIONS to be used
This commit is contained in:
Andrew Tridgell 2018-05-04 11:40:36 +10:00
parent a575608110
commit 61c8dfac31
3 changed files with 134 additions and 107 deletions

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@ -2,6 +2,8 @@
// Unit tests for the AP_Math polygon code
//
#define ALLOW_DOUBLE_MATH_FUNCTIONS
#include <AP_HAL/AP_HAL.h>
#include <AP_Math/AP_Math.h>

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@ -211,113 +211,6 @@ void print_latlon(AP_HAL::BetterStream *s, int32_t lat_or_lon)
s->printf("%ld.%07ld",(long)dec_portion,(long)frac_portion);
}
#ifdef ALLOW_DOUBLE_MATH_FUNCTIONS
/*
these are not currently used. They should be moved to location_double.cpp if we do enable them in the future
*/
void wgsllh2ecef(const Vector3d &llh, Vector3d &ecef) {
double d = WGS84_E * sin(llh[0]);
double N = WGS84_A / sqrt(1 - d*d);
ecef[0] = (N + llh[2]) * cos(llh[0]) * cos(llh[1]);
ecef[1] = (N + llh[2]) * cos(llh[0]) * sin(llh[1]);
ecef[2] = ((1 - WGS84_E*WGS84_E)*N + llh[2]) * sin(llh[0]);
}
void wgsecef2llh(const Vector3d &ecef, Vector3d &llh) {
/* Distance from polar axis. */
const double p = sqrt(ecef[0]*ecef[0] + ecef[1]*ecef[1]);
/* Compute longitude first, this can be done exactly. */
if (!is_zero(p))
llh[1] = atan2(ecef[1], ecef[0]);
else
llh[1] = 0;
/* If we are close to the pole then convergence is very slow, treat this is a
* special case. */
if (p < WGS84_A * double(1e-16)) {
llh[0] = copysign(M_PI_2, ecef[2]);
llh[2] = fabs(ecef[2]) - WGS84_B;
return;
}
/* Calculate some other constants as defined in the Fukushima paper. */
const double P = p / WGS84_A;
const double e_c = sqrt(1 - WGS84_E*WGS84_E);
const double Z = fabs(ecef[2]) * e_c / WGS84_A;
/* Initial values for S and C correspond to a zero height solution. */
double S = Z;
double C = e_c * P;
/* Neither S nor C can be negative on the first iteration so
* starting prev = -1 will not cause and early exit. */
double prev_C = -1;
double prev_S = -1;
double A_n, B_n, D_n, F_n;
/* Iterate a maximum of 10 times. This should be way more than enough for all
* sane inputs */
for (int i=0; i<10; i++)
{
/* Calculate some intermmediate variables used in the update step based on
* the current state. */
A_n = sqrt(S*S + C*C);
D_n = Z*A_n*A_n*A_n + WGS84_E*WGS84_E*S*S*S;
F_n = P*A_n*A_n*A_n - WGS84_E*WGS84_E*C*C*C;
B_n = double(1.5) * WGS84_E*S*C*C*(A_n*(P*S - Z*C) - WGS84_E*S*C);
/* Update step. */
S = D_n*F_n - B_n*S;
C = F_n*F_n - B_n*C;
/* The original algorithm as presented in the paper by Fukushima has a
* problem with numerical stability. S and C can grow very large or small
* and over or underflow a double. In the paper this is acknowledged and
* the proposed resolution is to non-dimensionalise the equations for S and
* C. However, this does not completely solve the problem. The author caps
* the solution to only a couple of iterations and in this period over or
* underflow is unlikely but as we require a bit more precision and hence
* more iterations so this is still a concern for us.
*
* As the only thing that is important is the ratio T = S/C, my solution is
* to divide both S and C by either S or C. The scaling is chosen such that
* one of S or C is scaled to unity whilst the other is scaled to a value
* less than one. By dividing by the larger of S or C we ensure that we do
* not divide by zero as only one of S or C should ever be zero.
*
* This incurs an extra division each iteration which the author was
* explicityl trying to avoid and it may be that this solution is just
* reverting back to the method of iterating on T directly, perhaps this
* bears more thought?
*/
if (S > C) {
C = C / S;
S = 1;
} else {
S = S / C;
C = 1;
}
/* Check for convergence and exit early if we have converged. */
if (fabs(S - prev_S) < double(1e-16) && fabs(C - prev_C) < double(1e-16)) {
break;
} else {
prev_S = S;
prev_C = C;
}
}
A_n = sqrt(S*S + C*C);
llh[0] = copysign(1.0, ecef[2]) * atan(S / (e_c*C));
llh[2] = (p*e_c*C + fabs(ecef[2])*S - WGS84_A*e_c*A_n) / sqrt(e_c*e_c*C*C + S*S);
}
#endif // ALLOW_DOUBLE_MATH_FUNCTIONS
// return true when lat and lng are within range
bool check_lat(float lat)
{

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@ -0,0 +1,132 @@
/*
* location_double.cpp
*
* This file 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 file 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, see <http://www.gnu.org/licenses/>.
*/
/*
this is for double precision functions related to the location structure
*/
#define ALLOW_DOUBLE_MATH_FUNCTIONS
#include <AP_HAL/AP_HAL.h>
#include <stdlib.h>
#include "AP_Math.h"
#include "location.h"
/*
these are not currently used. They should be moved to location_double.cpp if we do enable them in the future
*/
void wgsllh2ecef(const Vector3d &llh, Vector3d &ecef) {
double d = WGS84_E * sin(llh[0]);
double N = WGS84_A / sqrt(1 - d*d);
ecef[0] = (N + llh[2]) * cos(llh[0]) * cos(llh[1]);
ecef[1] = (N + llh[2]) * cos(llh[0]) * sin(llh[1]);
ecef[2] = ((1 - WGS84_E*WGS84_E)*N + llh[2]) * sin(llh[0]);
}
void wgsecef2llh(const Vector3d &ecef, Vector3d &llh) {
/* Distance from polar axis. */
const double p = sqrt(ecef[0]*ecef[0] + ecef[1]*ecef[1]);
/* Compute longitude first, this can be done exactly. */
if (!is_zero(p))
llh[1] = atan2(ecef[1], ecef[0]);
else
llh[1] = 0;
/* If we are close to the pole then convergence is very slow, treat this is a
* special case. */
if (p < WGS84_A * double(1e-16)) {
llh[0] = copysign(M_PI_2, ecef[2]);
llh[2] = fabs(ecef[2]) - WGS84_B;
return;
}
/* Calculate some other constants as defined in the Fukushima paper. */
const double P = p / WGS84_A;
const double e_c = sqrt(1 - WGS84_E*WGS84_E);
const double Z = fabs(ecef[2]) * e_c / WGS84_A;
/* Initial values for S and C correspond to a zero height solution. */
double S = Z;
double C = e_c * P;
/* Neither S nor C can be negative on the first iteration so
* starting prev = -1 will not cause and early exit. */
double prev_C = -1;
double prev_S = -1;
double A_n, B_n, D_n, F_n;
/* Iterate a maximum of 10 times. This should be way more than enough for all
* sane inputs */
for (int i=0; i<10; i++)
{
/* Calculate some intermmediate variables used in the update step based on
* the current state. */
A_n = sqrt(S*S + C*C);
D_n = Z*A_n*A_n*A_n + WGS84_E*WGS84_E*S*S*S;
F_n = P*A_n*A_n*A_n - WGS84_E*WGS84_E*C*C*C;
B_n = double(1.5) * WGS84_E*S*C*C*(A_n*(P*S - Z*C) - WGS84_E*S*C);
/* Update step. */
S = D_n*F_n - B_n*S;
C = F_n*F_n - B_n*C;
/* The original algorithm as presented in the paper by Fukushima has a
* problem with numerical stability. S and C can grow very large or small
* and over or underflow a double. In the paper this is acknowledged and
* the proposed resolution is to non-dimensionalise the equations for S and
* C. However, this does not completely solve the problem. The author caps
* the solution to only a couple of iterations and in this period over or
* underflow is unlikely but as we require a bit more precision and hence
* more iterations so this is still a concern for us.
*
* As the only thing that is important is the ratio T = S/C, my solution is
* to divide both S and C by either S or C. The scaling is chosen such that
* one of S or C is scaled to unity whilst the other is scaled to a value
* less than one. By dividing by the larger of S or C we ensure that we do
* not divide by zero as only one of S or C should ever be zero.
*
* This incurs an extra division each iteration which the author was
* explicityl trying to avoid and it may be that this solution is just
* reverting back to the method of iterating on T directly, perhaps this
* bears more thought?
*/
if (S > C) {
C = C / S;
S = 1;
} else {
S = S / C;
C = 1;
}
/* Check for convergence and exit early if we have converged. */
if (fabs(S - prev_S) < double(1e-16) && fabs(C - prev_C) < double(1e-16)) {
break;
} else {
prev_S = S;
prev_C = C;
}
}
A_n = sqrt(S*S + C*C);
llh[0] = copysign(1.0, ecef[2]) * atan(S / (e_c*C));
llh[2] = (p*e_c*C + fabs(ecef[2])*S - WGS84_A*e_c*A_n) / sqrt(e_c*e_c*C*C + S*S);
}