The Amur River runoff formation in the Amur liman

被引：0
|
作者：
E. V. Ivanova
V. V. Ivanov
机构：
[1] University of Manchester,Faculty of Life Sciences
[2] Russian Academy of Sciences,Institute of Marine Geology and Geophysics, Far Eastern Branch
来源：
Russian Meteorology and Hydrology | 2012年 / 37卷
关键词：
Level Variation; Brightness Temperature; RUSSIAN Meteorology; Wave Propagation Velocity; Runoff Variation;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
Periodical surface currents with the periods of 46.5, 61, and 91 days detected from the satellite data in the Tatar Strait and Sakhalin Bay are presented as an effect of the Amur River runoff transformation in the estuary. The estuary transforms the flow as a flip-flop directing the Amur runoff by turns to the Sea of Japan or to the Sea of Okhotsk. The flip-flop period is six months. From May 23 to November 10, the Amur River flows into the Sea of Okhotsk and from November 10 to May 25, into the Sea of Japan.
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页码：631 / 639
页数：8
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