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A Modelling Stndy of Potential Evapotranspiration and the Estimation of Chinese Soil Moistnre Regimes 被引量:1
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作者 LIU DUOSEN and WANG ZONGSHENG(Instttute of Soil Science, Academia Sinica, P. O. Box 821, Nanjing 210008(China)) 《Pedosphere》 SCIE CAS CSCD 1994年第3期193-200,共8页
Based on the conception of fluid mechanics, the paper propounds a model for monthly potential evapo-transpiration E<sub>Ti</sub> (mm): where i is the number of a month, P<sub>i</sub> the mean... Based on the conception of fluid mechanics, the paper propounds a model for monthly potential evapo-transpiration E<sub>Ti</sub> (mm): where i is the number of a month, P<sub>i</sub> the mean monthly atmospheric pressure (hpa), t<sub>i</sub> the mean monthlyair temperature (° C), d<sub>i</sub> the number of days in the month, U<sub>i</sub> the mean monthly wind velocity measured atheight 10-12 m (m/s), w<sub>oi</sub> the saturated water vapour pressure at t<sub>i</sub>(mmHg, 1 mmHg=133.322 Pa), and h<sub>i</sub>the mean monthly relative humidity. The annual aridity K is:where ra is the mean annual precipitation (mm). Based upon the data of 669 sites in China during 1951-1980, the relations among the soil moisture regime, the vegetation and the value of K may be illustrated asfollows:K Soil moisture regime VegetationK 【 1 Udic Forest Semi-udic Forest, forest-steppe and steppeSemi-aridic Arid steppe Aridic Desert-steppe Very aridic Desert 展开更多
关键词 ARIDITY EVAPOTRANSPIRATION MODELLING moisture regimesscience FOUNDATION of China and the ACADEMIA Sinica.
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