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 ；
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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