干燥裸地边界层内的逆湿现象是由于下垫面非均匀的湿度场与中尺度平流的共同作用的结果。
A phenomenon called humidity inversion is caused by the joint of the heterogeneous humidity Pattern and mesoscale advection over the underlying surface.
计算结果表明此系统可进行大气边界层和平流层探测。
It is shown from the calculated results that the system can be used for atmospheric boundary layer and stratosphere sounding.
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