# From Madzak et al # "High frequency-Earth rotation variations deduced from altimetry based ocean models", J. Geodesy., 90:1237 # X Y UT1 LOD # gamma l l0 F D Omega Doodson Period Sin Cos Sin Cos Sin Cos Sin Cos SQ1 1 -2 0 -2 0 -2 125.755 28.0062 0.7 4.8 -4.8 0.7 0.9 -0.3 -1.7 -4.6 sig1 1 0 0 -2 -2 -2 127.555 27.8484 0.9 5.7 -5.7 0.9 1.0 -0.4 -2.1 -5.4 - 1 -1 0 -2 0 -1 135.645 26.8728 1.9 5.8 -5.8 1.9 0.8 -0.5 -2.7 -4.7 Q1 1 -1 0 -2 0 -2 135.655 26.8684 10.3 30.5 -30.5 10.3 4.4 -2.5 -14.2 -24.6 rho1 1 1 0 -2 -2 -2 137.455 26.7231 2.0 5.6 -5.6 2 0.8 -0.5 -2.7 -4.4 - 1 0 0 -2 0 -1 145.545 25.8234 12.2 27.4 -27.4 12.2 2.9 -2.5 -14.5 -16.8 O1 1 0 0 -2 0 -2 145.555 25.8193 65.1 146.1 -146.1 65.1 15.3 -13.3 -77.6 -89.5 - 1 1 0 -2 0 -2 155.455 24.8492 -1.4 -3.8 3.8 -1.4 -0.4 0.3 1.8 2.2 M1 1 -1 0 0 0 0 155.655 24.8332 -4.0 -10.5 10.5 -4.0 -1.0 0.9 5.3 6.3 pi1 1 0 -1 -2 2 -2 162.556 24.1321 1.9 3.3 -3.3 1.9 0.3 -0.2 -1.4 -1.9 P1 1 0 0 -2 2 -2 163.555 24.0659 28.1 40.3 -40.3 28.1 4.6 -2.9 -18.2 -29.0 - 1 0 0 0 0 1 165.545 23.938 2.2 3.1 -3.1 2.2 0.3 -0.2 -1.3 -1.9 K1 1 0 0 0 0 0 165.555 23.9345 -113.0 -158.0 158.0 -113.0 -15.3 9.7 61.4 96.5 - 1 0 0 0 0 -1 165.565 23.931 -15.3 -21.4 21.4 -15.3 -2.1 1.3 8.3 13.1 J1 1 1 0 0 0 0 175.455 23.0985 -11.9 -6.4 6.4 -11.9 -0.7 0.1 0.6 4.3 OO1 1 0 0 2 0 2 185.555 22.3061 -11.2 -1.9 1.9 -11.2 -0.2 -0.3 -1.7 1.7 - 1 0 0 2 0 1 185.565 22.303 -7.2 -1.2 1.2 -7.2 -0.2 -0.2 -1.1 1.1 2N2 2 -2 0 -2 0 -2 235.755 12.9054 -6.6 -0.9 1.1 4.0 -0.4 -0.4 -5.0 5.2 mu2 2 0 0 -2 -2 -2 237.555 12.8718 -8.0 -1.1 1.2 4.8 -0.5 -0.5 -5.9 6.3 N2 2 -1 0 -2 0 -2 245.655 12.6583 -49.4 -10.3 4.3 32.5 -2.7 -2.1 -24.9 32.1 nu2 2 1 0 -2 -2 -2 247.455 12.626 -9.6 -1.8 1.0 6.1 -0.5 -0.4 -4.7 6.4 - 2 0 0 -2 0 -1 255.545 12.4215 10.6 0.9 -1.6 -6.5 0.6 0.3 3.5 -7.4 M2 2 0 0 -2 0 -2 255.555 12.4206 -282.1 -24.6 43.6 174.0 -16.5 -8.0 -96.7 200.3 L2 2 1 0 -2 0 -2 265.455 12.1916 8.4 -1.1 -2.3 -5.3 0.4 0.3 3.1 -4.5 T2 2 0 -1 -2 2 -2 272.556 12.0164 -8.2 2.4 3.1 4.7 -0.4 -0.2 -2.1 5.4 S2 2 0 0 -2 2 -2 273.555 12 -132.3 53.1 56.1 84.3 -8.7 -1.8 -22.2 109.9 K2 2 0 0 0 0 0 275.555 11.9672 -38.0 12.7 15.5 21.4 -2.2 -0.6 -7.2 27.7 - 2 0 0 0 0 -1 275.565 11.9664 -11.4 3.8 4.6 6.3 -0.7 -0.2 -2.2 8.3