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利用NOAA卫星 1 995年 1月— 1 997年 2月的海洋遥感资料系统地分析和研究了黄、东海陆架区悬浮体向深海输运的时间和空间变化规律 ,并对其动力机制进行了分析和探讨。研究结果表明 ,黄、东海悬浮体在 1 1— 3月份为向外海输运阶段 ,5— 9月份则退向近海为内储阶段 ,4月份为输变退的月份 ,1 0月份则是退变输的月份 ,其中 3月份黄、东海悬浮体向东海深海输运得最远 ,9月份则向岸退得最远 ;黄、东海表面悬浮体向东海的输运范围一般皆位于 1 0 0m等深线以内 ,并很难越过黑潮水系 ,而输向深海的悬浮体又大都在黄海暖流的作用下回输黄海 ,其大部输向韩国西南海域。
The temporal and spatial variation of suspended matter transport to the deep sea in the Yellow Sea and East China Sea shelf areas was systematically analyzed and studied using the ocean remote sensing data from January 1995 to January 1997 by NOAA satellite 1 and its dynamic mechanism was analyzed And explore. The results show that the suspended sediments in the Yellow Sea and the East China Sea are transported to the open sea in January-March and returned to the offshore in September-September, while the month in April is the month in which the transition is reversed. In March, the suspended sediments in the Yellow Sea and East China Sea transported farthest to the deep sea in the East China Sea and the farthest to the shore in September. The transport ranges of the suspended sediments on the Yellow Sea and East China Sea to the East China Sea generally ranged from 100m Isobaths, and it is difficult to cross the Kuroshio water system. Most of the suspended sediments transported to the deep sea are transported back to the Yellow Sea under the action of the Yellow Sea warm current, and most of them are exported to the southwestern South China Sea.