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Intraseasonal variation in the salinity of the Yellow and East China Seas in the summers of 2011, 2012, and 2013

机译:2011年,2012年和2013年夏季黄海和东海盐度的季节内变化

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Hydrographic data obtained during eight cruises in the summers of 2011, 2012, and 2013 reveal a substantial intraseasonal variation in the salinity of the Yellow and East China Seas. Salinity variation reflects changes in the water masses in which jellyfish grow from juveniles to adults and changes in the circulation system that can transport jellyfish. The primary change occurred in surface salinity due to inconstant plume pathways caused by the swerve of the offshore current. Distinctive events occurred in the Yellow Sea in 2012, and also occurred in a zone spanning from the mouth of the Changjiang to Jeju Island in 2013. The observations indicated the advancement and recession of the Taiwan Warm Current (TWC), especially its inner branch and the Kuroshio intrusion, induce substantial variations during summer (June, July and August). Atmospheric forcing, the buoyancy input from rivers, Kuroshio transport and a water level discrepancy between the Bashi Channel and the Taiwan Strait that controls the TWC, influence the circulation regime. The changes in all of the aforementioned forcings need to be recorded to understand the mechanism of the dynamic patterns in water masses, temperature and salinity and predict the characteristics of the jellyfish blooming environment.
机译:在2011年,2012年和2013年夏季的八次航行中获得的水文数据表明,黄海和东海的盐度在季节内有很大变化。盐度变化反映了水母从幼体到成年的水团的变化以及可以运输水母的循环系统的变化。最初的变化发生在表面盐度的变化,这是由于近海流转弯引起的羽流路径不固定所致。独特的事件发生在2012年的黄海中,也发生在2013年从长江口到济州岛的区域中。观测结果表明,台湾暖流(TWC)的发展和衰退,特别是其内部分支和黑潮的入侵会在夏季(6月,7月和8月)引起大量变化。大气强迫,河流的浮力输入,黑潮输水以及巴什海峡和控制TWC的台湾海峡之间的水位差异影响了环流状况。需要记录所有上述强迫的变化,以了解水团,温度和盐度中动态模式的机制,并预测水母开花环境的特征。

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