Subarctic Gyre in the North Pacific Ocean.
Subarctic Gyre in the North Pacific Ocean.
复制标题
北太平洋的亚北极环流。
DOI：
10.5928/kaiyou.1.75
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发表时间：
1992
期刊：
影响因子：
--
通讯作者：
M. Kashiwai
中科院分区：
文献类型：
--
作者：
Y. Nagata;K. Ohtani;M. Kashiwai
本文讨论了北太平洋副极地环流的环流特征和水团的变化过程。环流路径很好地渗透到白令海内部，一部分水进入鄂霍次克海。水团在这些边缘海及其附近发生了显著变化。该水被证明是由东堪察加海流水和鄂霍次克海水混合而成。鄂霍次克海是中间层中最淡水的海区，对北太平洋中间水的形成起着重要作用。
The circulation nature in the Subarctic Gyre in the North Pacific, and the water mass modification processes found there are discussed. The circulation path penetrates well inside the Bering Sea, and a part of the water enters into the Okhotsk Sea. The water masses are modified significantly in and near these marginal seas. The Oyashio Water is shown to be formed by mixing between the East Kamchatka Current Water and the Okhotsk Sea Water. The freshest water in the intermediate layers is found in the Okhotsk Sea, and appears to play important role in the formation of the North Pacific Intermediate Water.