Water temperature variations off the Sakhalin coast from the data of instrumental observations

被引:1
|
作者
Shevchenko, G. V. [1 ]
Kirillov, K. V. [1 ]
机构
[1] Russian Acad Sci, Far Eastern Branch, Inst Marine Geol & Geophys, Ul Nauki 1B, Yuzhno Sakhalinsk 693022, Russia
关键词
Water temperature; bottom station; wind speed; oceanological section; coastal upwelling;
D O I
10.3103/S1068373917030062
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The data of instrumental observations of water temperature at autonomous bottom stations in the coastal zone of Sakhalin Island (the depth is 3-17 m) mainly along the southeastern coast are analyzed. The cases of sharp (by 15A degrees C per day) temperature drop are detected. They are caused by the strengthening of southern and southwestern winds typtcal of summer and betng the offshore winds which favor the lift of cold water to the surface. This phenomenon is observed every year but its intensity varies depending on the frequency of offshore winds. Along the southwestern coast of Sakhalin, where the offshore effect is induced by northern, northeastern, and eastern winds characterized by the low frequency of occurrence, water temperature drops are rarer and shorter (3-5 days) but rather sharp. The occurrence of cold water (its temperature is sometimes negative) in the shallow coastal zone may lead to the mass mortality of juvenile salmon after its downstream migration in spawning rivers, may impede the approaches of humpback salmon and negatively affect its catch.
引用
收藏
页码:189 / 197
页数:9
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