Strong temperature gradients with stable stratification immediately above the surface are typical for radiation cooling, but near-surface temperature inversions (hereinafter referred to as inversions) have hardly been studied. Both phenomena are examined in more detail by means of measurements in the Caspian Sea and Antarctica and compared with measurements made by other authors. For this purpose, tests for decoupling are applied in the first case. In the second case, the inversions can be explained in the context of counter-gradient fluxes and turbulent Prandtl numbers greater than one.

中文翻译：

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稳定分层过程中大气与下垫面之间的解耦

辐射冷却的典型特征是地表正上方具有稳定分层的强温度梯度，但几乎没有研究近地表温度反转（以下简称反转）。通过在里海和南极洲的测量，对这两种现象进行了更详细的研究，并与其他作者的测量结果进行了比较。为此，在第一种情况下应用去耦测试。在第二种情况下，可以在反梯度通量和大于一的湍流普朗特数的背景下解释反演。