丰水年,土壤水分收支正平衡,但入渗雨量的大部分(>80%)为强烈蒸发蒸腾所消耗。
In rainy year, soil water storage increased, but most infiltrated rainfall (more than 80%) was consumed by intensive evapotranspiration.
同时计算了江淮地区地面的降水量、蒸发量和地面余水量,分析了地面的水分收支和水分盈亏。
The rainfall, evaporation and remaining water on the ground were also calculated, and its water budget and water excess (deficit) were analyzed.
同时计算了江淮地区地面的降水量、蒸发量和地面余水量,分析了地面的水分收支和水分盈亏。
The rainfall, evaporation and remaining water on the ground were also calculated, and its water budget and water excess (deficit) were analyzed.
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