Тип публикации
статья в журнале
Журнал
Izvestiya - Atmospheric and Ocean Physics
ISSN:0001-4338
eSSN:1555-628X
Выходные данные
том
54
выпуск
4
страницы
616-620
Абстракт
Shallow water equations have been used to analyze the final stage of the response of a semi-infinite rotating basin to the wind impulse effect simulating the passage
of a storm in the presence of a coastal current. It has been shown that the most significant effect upon a high storm intensity is that the coastal stream core shifts
several kilometers toward the coast or from the coast, depending on the sign of the Ekman transport. The additional currents arising after the storm passage in the
presence of an alongshore stream differ only quantitatively from the currents arising in its absence.
Ключевые слова
HALLOW WATER EQUATIONS, INERTIAL OSCILLATIONS, COASTAL CURRENTS, WIND IMPULSE
Дата занесения
2018-12-12 15:49:00