Greatly increased influence of the deep water masses in the western Pacific during the last glacial maximum
Greatly increased influence of the deep water masses in the western Pacific during the last glacial maximum
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发表时间：
1996
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通讯作者：
翦知湣
中科院分区：
文献类型：
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作者：
翦知湣
在现代海洋中，深水主要产于大西洋，流向太平洋。但在冰川时期，太平洋可能产生了深水，然后均匀地反向流向大西洋。然而，“北太平洋深水(NPDW)”还是“中间水”真的产生于冰川时期的太平洋吗？这是一个有争议的问题，需要用实际材料来解决。南海中国海域是寻找答案的中心海域。作为边缘海，南海提供了
In the modern ocean, deep water is mainly produeed in the Atlantic and flows to thePacific. But during glacials deep water could have been produeed in the Pacific and eveninversely flown to the Atlantic. However, is 'the North Pacific Deep Water (NPDW)'or ouly the 'Intermediate Water' really produced in the Pacific during glacials? This isa disputable question to be solved by actual materials. The South China Sea (SCS) is justone of the areas where to search for the answer. Being a marginal sea, the SCS provides