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Surface energy and water vapor fluxes observed on a megadune in the Badain Jaran Desert, China
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) 。土壤热流动处于精力平衡起了一个重要作用。吝啬的实际蒸发是 0.41 mm/d，并且累积实际蒸发是约 150 mm/a。水蒸汽将 downwardly 搬运并且作为露水冷凝作用水出现。降水的数量决定了实际蒸发。实际蒸发应当等于 megadune 上的降水，降水是困难的再装地下水。我们的学习能在这个区域为关于陆地空气相互作用的进一步的研究提供一个基础。
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- W3148705509
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- article
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- EN
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- Acta Scientiarum Naturalium Universitatis Sunyatseni
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