摘要
陆面蒸发量可以根据水量平衡原理用降水量减径流量计算得出,或者在测得或间接算出土壤含水量后用蒸发模式加以计算。本文目的在于探讨不涉及径流和土壤含水量资料,仅用一般气象观测资料来计算陆面蒸发量的方法。
From Bouchet’s complementary relationship,two methods were developed to calculate actual evaporation and were tested by comparing the calculated mean yearly values with that obtained by means of mass budget method.
作者
张志明
Zhang Zhiming(Chengdu University of Science and Technology)
出处
《气象学报》
1988年第4期477-480,共4页
Acta Meteorologica Sinica
