function [E, N, U] = cart2utm(X, Y, Z, zone) %CART2UTM Transformation of (X,Y,Z) to (N,E,U) in UTM, zone 'zone'. % %[E, N, U] = cart2utm(X, Y, Z, zone); % % Inputs: % X,Y,Z - Cartesian coordinates. Coordinates are referenced % with respect to the International Terrestrial Reference % Frame 1996 (ITRF96) % zone - UTM zone of the given position % % Outputs: % E, N, U - UTM coordinates (Easting, Northing, Uping) %Kai Borre -11-1994 %Copyright (c) by Kai Borre % % CVS record: % $Id: cart2utm.m,v 1.1.1.1.2.6 2007/01/30 09:45:12 dpl Exp $ %This implementation is based upon %O. Andersson & K. Poder (1981) Koordinattransformationer % ved Geod\ae{}tisk Institut. Landinspekt\oe{}ren % Vol. 30: 552--571 and Vol. 31: 76 % %An excellent, general reference (KW) is %R. Koenig & K.H. Weise (1951) Mathematische Grundlagen der % h\"oheren Geod\"asie und Kartographie. % Erster Band, Springer Verlag % Explanation of variables used: % f flattening of ellipsoid % a semi major axis in m % m0 1 - scale at central meridian; for UTM 0.0004 % Q_n normalized meridian quadrant % E0 Easting of central meridian % L0 Longitude of central meridian % bg constants for ellipsoidal geogr. to spherical geogr. % gb constants for spherical geogr. to ellipsoidal geogr. % gtu constants for ellipsoidal N, E to spherical N, E % utg constants for spherical N, E to ellipoidal N, E % tolutm tolerance for utm, 1.2E-10*meridian quadrant % tolgeo tolerance for geographical, 0.00040 second of arc % B, L refer to latitude and longitude. Southern latitude is negative % International ellipsoid of 1924, valid for ED50 a = 6378388; f = 1/297; ex2 = (2-f)*f / ((1-f)^2); c = a * sqrt(1+ex2); vec = [X; Y; Z-4.5]; alpha = .756e-6; R = [ 1 -alpha 0; alpha 1 0; 0 0 1]; trans = [89.5; 93.8; 127.6]; scale = 0.9999988; v = scale*R*vec + trans; % coordinate vector in ED50 L = atan2(v(2), v(1)); N1 = 6395000; % preliminary value B = atan2(v(3)/((1-f)^2*N1), norm(v(1:2))/N1); % preliminary value U = 0.1; oldU = 0; iterations = 0; while abs(U-oldU) > 1.e-4 oldU = U; N1 = c/sqrt(1+ex2*(cos(B))^2); B = atan2(v(3)/((1-f)^2*N1+U), norm(v(1:2))/(N1+U) ); U = norm(v(1:2))/cos(B)-N1; iterations = iterations + 1; if iterations > 100 fprintf('Failed to approximate U with desired precision. U-oldU: %e.\n', U-oldU); break; end end %Normalized meridian quadrant, KW p. 50 (96), p. 19 (38b), p. 5 (21) m0 = 0.0004; n = f / (2-f); m = n^2 * (1/4 + n*n/64); w = (a*(-n-m0+m*(1-m0))) / (1+n); Q_n = a + w; %Easting and longitude of central meridian E0 = 500000; L0 = (zone-30)*6 - 3; %Check tolerance for reverse transformation tolutm = pi/2 * 1.2e-10 * Q_n; tolgeo = 0.000040; %Coefficients of trigonometric series %ellipsoidal to spherical geographical, KW p. 186--187, (51)-(52) % bg[1] = n*(-2 + n*(2/3 + n*(4/3 + n*(-82/45)))); % bg[2] = n^2*(5/3 + n*(-16/15 + n*(-13/9))); % bg[3] = n^3*(-26/15 + n*34/21); % bg[4] = n^4*1237/630; %spherical to ellipsoidal geographical, KW p. 190--191, (61)-(62) % gb[1] = n*(2 + n*(-2/3 + n*(-2 + n*116/45))); % gb[2] = n^2*(7/3 + n*(-8/5 + n*(-227/45))); % gb[3] = n^3*(56/15 + n*(-136/35)); % gb[4] = n^4*4279/630; %spherical to ellipsoidal N, E, KW p. 196, (69) % gtu[1] = n*(1/2 + n*(-2/3 + n*(5/16 + n*41/180))); % gtu[2] = n^2*(13/48 + n*(-3/5 + n*557/1440)); % gtu[3] = n^3*(61/240 + n*(-103/140)); % gtu[4] = n^4*49561/161280; %ellipsoidal to spherical N, E, KW p. 194, (65) % utg[1] = n*(-1/2 + n*(2/3 + n*(-37/96 + n*1/360))); % utg[2] = n^2*(-1/48 + n*(-1/15 + n*437/1440)); % utg[3] = n^3*(-17/480 + n*37/840); % utg[4] = n^4*(-4397/161280); %With f = 1/297 we get bg = [-3.37077907e-3; 4.73444769e-6; -8.29914570e-9; 1.58785330e-11]; gb = [ 3.37077588e-3; 6.62769080e-6; 1.78718601e-8; 5.49266312e-11]; gtu = [ 8.41275991e-4; 7.67306686e-7; 1.21291230e-9; 2.48508228e-12]; utg = [-8.41276339e-4; -5.95619298e-8; -1.69485209e-10; -2.20473896e-13]; %Ellipsoidal latitude, longitude to spherical latitude, longitude neg_geo = 'FALSE'; if B < 0 neg_geo = 'TRUE '; end Bg_r = abs(B); [res_clensin] = clsin(bg, 4, 2*Bg_r); Bg_r = Bg_r + res_clensin; L0 = L0*pi / 180; Lg_r = L - L0; %Spherical latitude, longitude to complementary spherical latitude % i.e. spherical N, E cos_BN = cos(Bg_r); Np = atan2(sin(Bg_r), cos(Lg_r)*cos_BN); Ep = atanh(sin(Lg_r) * cos_BN); %Spherical normalized N, E to ellipsoidal N, E Np = 2 * Np; Ep = 2 * Ep; [dN, dE] = clksin(gtu, 4, Np, Ep); Np = Np/2; Ep = Ep/2; Np = Np + dN; Ep = Ep + dE; N = Q_n * Np; E = Q_n*Ep + E0; if neg_geo == 'TRUE ' N = -N + 20000000; end; %%%%%%%%%%%%%%%%%%%% end cart2utm.m %%%%%%%%%%%%%%%%%%%%