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Air-Lake Interaction Features Found in Heat and Water Exchanges over Nam Co on the Tibetan Plateau

机译:青藏高原纳木错热与水交换中的气湖相互作用特征

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References(20) Cited-By(15) Supplementary materials(2) The central Tibetan Plateau contains numerous lakes, the largest and deepest of which is Nam Co. Heat and water budgets over Nam Co were estimated throughout the year. Latent and sensible heat fluxes from the lake are very small from spring to summer and larger from fall to early-winter. Although the land surface over the Tibetan Plateau supplies heat energy to the atmosphere during the pre-monsoon and monsoon periods, a deep lake such as Nam Co releases a large amount of heat in the post-monsoon period. Annual evaporation from the lake was 658 mm, much larger than the annual rainfall of 415 mm and also more than two times the annual evaporation from the land surface. The diurnal variation of surface-air temperature difference over the lake showed a reverse phase of that over land in the monsoon period, a condition that likely affects the convective activity over the lake.
机译:参考文献(20)被引用的文献(15)补充材料(2)青藏高原中部包含许多湖泊,其中最大和最深的是南姆湖。全年估算南姆湖的供热和水预算。从春季到夏季,来自湖泊的潜热通量非常小,从秋季到初冬则较大。尽管青藏高原上的陆地表面在季风前和季风期间向大气提供热能,但像纳姆科这样的深湖在季风后时期释放了大量的热量。湖泊的年蒸发量为658毫米,比415毫米的年降雨量大得多,也是陆地表面年蒸发量的两倍以上。季风期间,湖面上的地表空气温度差的日变化显示出与陆地上的温度相反,这种状况可能影响湖上的对流活动。

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