海面蒸发
- 网络sea surface evaporation
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由海面蒸发波导预报平流海雾的方法
The way to forecast sea advection fog from evaporation duct
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海面蒸发量测量工具的改进
Improvement of Measurement Tools of Sea-Surface Evaporation
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海面蒸发是海气相互作用的重要途径之一,是地球上热能交换的重要因子,海面蒸发量的测量对海气通量交换的研究具有十分重要的意义;
Evaporation from sea surface is one of the important approaches of mutual relationship between sea and the atmosphere , it is also an important factor of heat energy exchange on the earth .
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利用1951&1990年南海船舶报资料,用直接计算法,采用1°×1°网格,计算了南海海域的月平均感热通量和海面(蒸发)潜热通量。
The data from ship reports in South China Sea from 1951 to 1990 are used . Monthly mean values of sensible heat fluxes and latent heat fluxes of the sea surface ( evaporated ) are calculated in 1 °× 1 ° grids of South China Sea area .
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海洋混合层的影响是直接的,主要通过海面感热和蒸发量的变化影响低层大气。
The inclusion of the ocean mixing layer has directs effects on SST , mainly through the changes of the sensible heat flux and the evaporation amount .
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这一气温变化看似微小,但是,举个例子说,渐增的温差可能会加剧海面水汽的蒸发,从而使暴风雨愈演愈烈。
Though such a change appears small , incremental differences can , for example , add to the ferocity of storms by evaporating more steam off the ocean .