Сезонная изменчивость термохалинных характеристик вод эпипелагиали южной части Охотского моря

• Main Authors: Новиков, Ю., Самко, Е.
• Format: Text
• Language: unknown
• Published: Федеральное государственное унитарное предприятие «Тихоокеанский научно-исследовательский рыбохозяйственный центр» 2005
• Subjects: Okhotsk; Pacific; okhotsk sea
• Online Access: http://cyberleninka.ru/article/n/sezonnaya-izmenchivost-termohalinnyh-harakteristik-vod-epipelagiali-yuzhnoy-chasti-ohotskogo-morya; http://cyberleninka.ru/article_covers/9725361.png

В продолжение исследований структуры вод курило-сахалинского района по материалам судовых наблюдений за период 1960-1998 гг. определены основные водные массы южной части Охотского моря, рассмотрены их сезонное распределение и термохалинные характеристики. Climatic fields of water temperature and salinity at the horizons 0, 50, 100, 200 m are calculated for all seasons on the basis of oceanographic data (about 36 thousands stations) collected in the deep part of the Okhotsk Sea southward from 55o N in 1960-1998, averaged in 1-degree squares. The following main surface and subsurface water masses are identified: the Transformed Pacific Water in the eastern part of the region; the Okhotsk Sea Water in the western part of the region; the Soya Current Water near the shores of Hokkaido Island and Kunashir Island (in summer and autumn only); and the Transformed Water that occupies the southern part of the region and is formed by mixing between the Okhotsk Sea Water and Soya Current Water. All water masses have normal seasonal changes of temperature, with a minimum in winter and a maximum in summer at sea surface, and with a minimum in winter and a maximum in autumn in subsurface layer.