Water stable isotope record of ice core WAIS divide
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Changes in atmospheric circulation over the past five decades have enhanced the wind-driven inflow of warm ocean water onto the Antarctic continental shelf, where it melts ice...
近五十年来，大气环流的变化增强了风驱动的暖海水向南极大陆架的涌流，在此区域内暖海水会消融海冰……
