Countergradient heat flux in the surface layer in South Pole is analyzed based on the data obtained from the field experiments near China Zhongshan Observatory in South Pole.

根据南极中山站观测结果，分析了南极地区近地层热量逆梯度输送的现象。

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The analyses show that the countergradient heat flux often occurs in the stable atmospheric surface layer even when the inversion strength is fairly strong.

结果表明南极地区在近地层逆温较明显时 ，常会出现热量逆梯度输送的现象 ；

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