Autor:	Minato, Shinya
Zdroj:	Journal of Oceanography; June 1983, Vol. 39 Issue: 3 p141-149, 9p
Abstrakt:	Geostrophic response of a two-layer fluid near a straight coast is investigated for a successive disturbance by the use of the inviscid, reduced gravity model. Poincare waves, coastal motion (which is trapped by the coast) and a geostrophic eddy are created. The energy of these motions is obtained. The manner in which the ocean responds is found to depend considerably on the way the disturbance is applied.
Databáze:	Supplemental Index
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