结果表明：黄土高原核桃林地土壤蒸发量与月均温呈正相关关系。
The results showed that soil evaporative capacity of walnut forest land was positive correlation to average temperature of month.
5干热河谷典型的干热气候致使自由水面蒸发量是饱和土壤蒸发量3.35倍。
The amount of the water surface evaporation was approximately 3.35 times that of the saturated soil evaporation.
随着气温升高，干旱的危险也会增加：即使降雨量不减少，蒸发量增加也能使土壤干燥。
Drought risk also increases with warming: even where rainfall does not decline, increased evaporation dries out the soils.
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