Salinity maxima associated with some sub-surface water masses in the upper layers of the Bay of Bengal
Salinity maxima associated with some sub-surface water masses in the upper layers of the Bay of Bengal
复制标题
与孟加拉湾上层一些地下水团相关的盐度最大值
DOI：
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复制
发表时间：
1968
期刊：
影响因子：
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通讯作者：
C. Reddy
中科院分区：
文献类型：
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作者：
V. Varadachari;C. Murty;C. Reddy
介绍了西南季风期间孟加拉西部湾部分地下水团的分布情况。根据最大盐度和西格玛值，可以确定波斯湾和红海起源水域的存在。研究表明，波斯湾和红海海水分别在约200 m和400 m的深度进入海湾，并遵循各自进入深度的环流模式。指示了可能的进入路径。这些水域进入海湾后会下沉到不同的深度。波斯湾海水可追溯到约350 m 的深度，而红海水可追溯到900 m 的深度。
The distribution of some sub-surface water masses in the western bay of Bengal during the south-west monsoon period is presented. Based on the salinity maxima and sigma t values the existence of waters of Persian Gulf and Red Sea origin could be established. The studies show that the Persian Gulf and Red Sea waters enter the Bay at depths of about 200 m and 400 m respectively, and follow the circulation pattern at the respective depths of entry. The probable paths of entry are indicated. These waters sink to different depths subsequent to their entry into the Bay. The Persian Gulf water could be traced down to a depth of about 350 m while the Red Sea water could be traced down to 900 m depth.