RSS indicates the square toot of the sum of the variances for all eight. The values are also broken into various oceanic regions. Same as Table 1, but for the Northeast American and the Northwest European shelves. Maps showing the regions of M2 and K1 tidal power input and tidal energy dissipation in the global oceans. Note the primary power input is within 30 degrees of the equator for M2 and away from the equator for K1.
Primary dissipation is in shallow seas for both.
Tidal power flux vectors for M2 and K1 constituents. Note the high convergence into regions of high tidal energy dissipation rates. Load tides computed for M2 and K1 constituents using the correspondig oceanic tides from the global model. Note the regions of large amplification. Table Captions Table 1.