Thermal water structure in the North-West Pacific and role of wind forcing and advection in its forming
Two basic types of vertical thermal structure are defined in the North-West Pacific on the data obtained in CTD survey conducted from May 29 to July 9, 2013 . One of them prevailed in the coastal areas of the Bering Sea and at East Kamchatka where the depth of winter convection was 160-200 m and eve...
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| Формат: | Стаття |
| Мова: | Russian |
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Transactions of the Pacific Research Institute of Fisheries and Oceanography
2017-09-01
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| Серія: | Известия ТИНРО |
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| Онлайн доступ: | https://izvestiya.tinro-center.ru/jour/article/view/323 |