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Numerical simulation of water circulation in the central part of the Sea of Japan and study of its long-term variability in 1958–2006статья
Информация о цитировании статьи получена из
Web of Science,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 18 марта 2016 г.
- Авторы: Stepanov D.V., Diansky N.A., Novotryasov V.V.
- Журнал: Izvestiya - Atmospheric and Oceanic Physics
- Том: 50
- Номер: 1
- Год издания: 2014
- Издательство: Pleiades Publishing, Ltd
- Местоположение издательства: Road Town, United Kingdom
- Первая страница: 73
- Последняя страница: 84
- DOI: 10.1134/S0001433813050149
- Аннотация: The response of circulation in the Sea of Japan (SJ) to the CORE-calculated real atmospheric forcing for 1958–2006 is reconstructed using the general ocean circulation model developed at the Institute of Computational Mathematics, Russian Academy of Sciences (ICM RAS). Features of the interannual variability of the circulation in the intermediate and deep layers of the central part of SJ are studied from the numerical simulation results. For this, the spatiotemporal variability of the relative vorticity is calculated. Frequency spectra of this variability are calculated at depths of 500 and 800 m and the layer-average between these levels. The spectra have a quasi-discrete structure with maxima in vicinities of 4–5, 7, and 10-year periods. Coincidence is ascertained between frequencies corresponding to these periods and earlier determined frequencies of the inter-annual variability of the temperature field observed in the intermediate layer of the SJ in the second half of the 20th century.
- Добавил в систему: Дианский Николай Ардальянович