U Seiler, Periodic changes of the angular momentum budget due to the tides of the world ocean, J. Geophys. Res., 96, 10287, 1991.
This model of the ocean tides is a purely numerical one; no tidal observations were used in its solution. Seiler solved Laplace's tidal equations on a global finite-difference grid using time-stepping methods. Dissipation was effected by quadratic bottom drag and a turbulent eddy viscosity.
These angular momentum data are extracted directly from the above reference. Amplitude and Greenwich phase lag are given for major tidal constituents. The (x,y,z) Cartesian components of angular momentum refer to the (Greenwich, 90°E, North) axes. Momentum components are decomposed into those due to tidal oceanic heights, which perturb the inertia tensor, and tidal currents, which effect relative momentum exchanges between ocean and mantle.
Units of momentum amplitude are 1025 kg m2/s. Units of phase are degrees.
X Y Z Tides amp pha amp pha amp pha M2 Heights 0.824 327.8 0.264 300.8 0.824 96.5 M2 Currents 1.241 201.1 2.139 149.5 3.056 311.9 S2 Heights 0.282 26.5 0.402 328.9 0.792 130.3 S2 Currents 1.085 274.5 1.545 188.7 1.866 338.2 N2 Heights 0.189 307.0 0.045 94.7 0.019 67.5 N2 Currents 0.098 167.0 0.274 158.3 0.543 320.0 K1 Heights 0.637 358.2 1.134 221.4 0.076 124.9 K1 Currents 0.182 234.2 0.380 201.6 0.653 143.3 O1 Heights 0.489 13.6 1.533 217.1 0.516 106.6 O1 Currents 0.204 262.2 0.185 111.7 0.851 114.2 P1 Heights 0.251 351.1 0.371 228.3 0.047 183.0 P1 Currents 0.037 275.2 0.169 213.3 0.240 144.7
The following long-period constituents are in the same format, except the amplitude units are 1024 kg m2/s.
X Y Z Tides amp pha amp pha amp pha Mf Heights 0.093 118.3 0.112 24.5 3.324 15.8 Mf Currents 0.127 332.8 0.092 0.0 0.286 97.7 Mm Heights 0.043 58.2 0.059 339.5 1.945 10.7 Mm Currents 0.062 315.3 0.037 326.0 0.074 91.3 Ssa Heights 0.026 6.2 0.012 258.6 1.851 2.0 Ssa Currents 0.011 278.3 0.007 279.9 0.009 88.9(The Ssa components refer only to the gravitational component, not the larger meteorologically driven component.)