Distributions of the Temperature and Salinity in Kamak Bay
Distributions of the Temperature and Salinity in Kamak Bay
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卡马克湾温度和盐度的分布
DOI：
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发表时间：
1990
期刊：
影响因子：
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通讯作者：
Cho Kyu
中科院分区：
文献类型：
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作者：
Lee Kyu;Cho Kyu
本文利用1988年5月至1989年2月四季的详细水文资料，研究了具有两个水道和三个海底地形区的卡马克湾的温、盐度分布。1989.卡马克湾温盐特征分布的总体格局基本上是由海湾的地形和海水运动所形成的。这些分布的季节变化主要来自于海面的加热和冷却以及径流量的增加。海湾有三个显著的水团，其一般特征如下：内湾水具有受内陆和西北部海底凹陷影响的停滞特征，Yosu港水具有由东北部Somjin河和Yon布鲁克莱特径流引起的低盐度河口特征，而外湾水具有外海特征，因为它位于海湾南部的大口附近。由于流态的不同，潮涨潮落时水团的分布呈现出不同的特征，而且杭大里附近海域的海况日变化较大，可能影响到海湾生物的生活和生产。
The distributions of the temperature and salinity in Kamak bay which has two channels and three sea bottom topographic parts were studied by taking the detailed hydrographic data at the ebb and flood during four seasons from May, 1988 to Feb., 1989. The general pattern of the distributions of characteristics which the temperature and salinity has in Kamak bay is basically formed by the topography and sea water movement of the bay. The changes of these distributions by seasons mainly come from the heating and cooling of the sea surface and the increase of the run-off. The bay has three remarkable water masses and the their general characteristics are follows: the inner bay water has a stagnation character influenced by the inland and the concave of the sea bottom in the north west, Yosu harbor water has an estuary character of the low salinity caused by the run-off of Somjin river and Yon Tung brooklet in the north east, and the outer bay water has an out-sea character, as it is located near by the big mouth in the south of the bay. The distributions of those water masses at the ebb and flood show some different features due to the flow patterns, and the daily changes of oceanic conditions at the vicinity of Hangdae-ri are so big that it may influence the habitation and production of the living things in the bay.