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首页> 外文期刊>Oceanology >Study of the heat flux at the water-bottom sediments in Amurskiy Bay in the Sea of Japan in the winter season
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Study of the heat flux at the water-bottom sediments in Amurskiy Bay in the Sea of Japan in the winter season

机译:冬季日本海阿穆尔斯基湾水底沉积物热通量研究

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摘要

The results of the temperature profiles and heat flux field studies in the upper layer of the bottom sediments of Amurskiy Bay in the Sea of Japan are presented. These studies were carried out from November 22 to March 25, 2010. The obtained values of the heat flux from the sediments to the water layer can explain the formation of the warm water layer with high salinity near the bottom in Amurskiy Bay during the winter season.
机译:介绍了日本海Amurskiy湾底部沉积物上层的温度剖面和热通量场研究的结果。这些研究是在2010年11月22日至3月25日进行的。从沉积物到水层的热通量的获得值可以解释冬季冬季阿穆尔斯基湾底部附近盐分高的温水层的形成。 。

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