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On the relation between residual currents and the wind field in the German Bightстатья
Информация о цитировании статьи получена из
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Дата последнего поиска статьи во внешних источниках: 28 мая 2015 г.
- Авторы: Koltermann K.P., Lange W.
- Журнал: Deutsche Hydrographische Zeitschrift
- Том: 28
- Номер: 5
- Год издания: 1975
- Первая страница: 193
- Последняя страница: 206
- DOI: 10.1007/BF02232570
- Аннотация: The long-period part (T>25 h) of currents measured at close spacing in the German Bight in June 1968 is investigated. The north component of the bottom current is shown to be highly correlated with the east component of the wind in this area, the wind-generated changes of the mass-field giving rise to a quasi-geostrophic current near the bottom. This current responds without perceptible delay to the variations of wind fields with periods considerably longer than those of the seiches of the North Sea. The accelerations linked to such long periods are so small as to be negligable and the residual currents can be regarded as quasi-stationary. © 1975 Deutsches Hydrographisches Institut.
- Добавил в систему: Koltermann Klaus Peter