在离岸较远的深水区，影响POC垂直分布的主要因素是大洋海水的性质。
Otherwise, in the shelf break of the East China Sea, the vertical distribution of POC was controlled by the characteristics of the deep ocean water.
特纳说，“危险的是，这种越来越温暖的海水会进入这些冰架底层，导致冰流越来越快地向大洋输送冰块。”
danger is that this warmer water will get under these ice shelvesand cause the ice streams to get faster and feed ice out into theocean, " said Turner.
低潮过后大洋的海水回来的特别快。
The low tide was over and the ocean water came back very quick.
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