While internal waves generally have a lower frequency than surface waves, they often form as a single wave that breaks into multiple waves as it hits a slope and moves upward.
32.
Specific objectives were to collect data on sea-surface winds, sea-surface temperatures, wave heights, internal waves, atmospheric water, sea ice features and ocean topography.
33.
In physical oceanography, the sublittoral zone refers to coastal regions with significant tidal flows and energy dissipation, including non-linear flows, internal waves, river outflows and oceanic fronts.
34.
In this way, there is a hypothesis that the internal waves accompanied by changes in the salt content, the water temperature, and the hydraulic pressure would obstruct the boat from advancing.
35.
Shanks hypothesized that by clinging to floating debris, crabs can be transported towards shore due to the oceanographic forces of internal waves, which carry floating debris shoreward regardless of the prevailing currents.
36.
Arrival of cool, nutrient-rich water from depths due to internal waves and tidal bores has been linked to growth rates of suspension feeders and benthic algae as well as plankton and larval organisms.
37.
Funayurei are said to possess ships and prevent them from moving, but they have somewhat been given a scientific explanation in the modern era, and have been determined to be a phenomenon of internal waves.
38.
The restoring force for internal waves and tides is still gravity but its effect is reduced because the densities of the 2 layers are relatively similar compared to the large density difference at the air-sea interface.
39.
This occurs when the ship is sailing on a layer of relatively fresh water whose depth is comparable to the ship's draft . This causes a wake of internal waves that dissipates a huge amount of energy.
40.
Whereas the reduced gravity is the key variable describing buoyancy for interfacial internal waves, a different quantity is used to describe buoyancy in continuously stratified fluid whose density varies with height as \ rho _ 0 ( z ).
