The tomographic inversion of the surface layer velocity model with the first break is the important base of the tomographic static correction.
初至波表层速度模型层析反演是层析静校正的重要基础。
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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