Has the upper portion of the Japan Sea Proper Water formation really been enhancing?
Has the upper portion of the Japan Sea Proper Water formation really been enhancing?
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DOI：
10.1007/s10872-012-0115-y
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发表时间：
2012-08-01
影响因子：
2.3
通讯作者：
Senjyu, Tomoharu
中科院分区：
文献类型：
--
作者：
Cui, Yanlin;Senjyu, Tomoharu
根据1970年至2004年的溶解氧浓度和潜在温度，检测到日本海上部固有水形成的减弱，与以前的研究表明，自20世纪70年代以来，它已经增强。所揭示的变暖和整个水柱中溶解氧浓度的下降趋势表明，在日本海的输送带系统仍然放缓，即使在中间层，虽然相对活跃的溶解氧供应到中间层的建议。这一事实使我们修改了以前关于水团形成的概念;虽然中间水团形成相对活跃，但深水层并未被中间水团形成所抵消，自20世纪70年代以来，整个日本海固有水形成一直处于停滞状态。
Weakening of the upper portion of the Japan Sea Proper Water formation was detected based on the dissolved oxygen concentration and potential temperature from 1970 to 2004, unlike the suggestion of previous studies that it has been enhanced since the 1970s. The revealed warming and decreasing trends in DO concentration throughout the water column indicate that the conveyor belt system in the Japan Sea is still slowing down even in the intermediate layers, though a relatively active dissolved oxygen supply into the intermediate layers is suggested. This fact leads us to modify the previous concept about the water mass formation; though a relatively active formation of the intermediate water mass occurs, the deep water formation is not counterbalanced by the intermediate water formation, and the overall Japan Sea Proper Water formation has been stagnating since the 1970s.