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蒸发（升华）作用对我国大陆型冰川的消融具有重要意义。随着冰川分布的海拔升高，其发育的气候条件更加寒冷干燥，蒸发量在消融中所占比例呈增加趋势。大陆型冰川的消融与其表面的气温、湿度及风速密切相关，其融化耗热与蒸发耗热之比值（ＭＥ）为表征其消融的重要参数；随着ＭＥ比值减小，它对消融的影响增大且蒸发量在消融中的比重增加。依大陆型冰川的ＭＥ比值可将其消融划分为融化型、融化蒸发过渡型和蒸发型。该划分亦可延伸至海洋型及极地型山地冰川
Evaporation (sublimation) effect on the ablation of continental glaciers in our country is of great significance. As the elevation of glacier distribution increases, the climatic conditions of its development are more cold and dry, and the evaporation proportion increases in ablation. The ablation of the continental glaciers is closely related to the surface temperature, humidity and wind speed. The ratio of melting and evaporating heat (ME) is an important parameter for the ablation. As the ME ratio decreases, the effect on the ablation increases Large and evaporation in the proportion of ablation increased. According to the continental-type glacier ME ratio can be divided into melt-thaw melting, thawing and evaporative transition and evaporation. The division can also extend to marine and polar mountain glaciers