| 多年平均陆面蒸发量的计算 |
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| 引用本文： | 杨远东. 多年平均陆面蒸发量的计算[J]. 地理研究, 1987, 6(4): 62-69. DOI: 10.11821/yj1987040007 |
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| 作者姓名： | 杨远东 |
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| 作者单位： | 长江流域规划办公室水文局 |
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| 摘 要： | 作者建议用公式E/r=thD(E0/r)来计算陆面蒸发量,并从数学上及气候物理概念上对此公式作了分析论证,认为是合理的可行的,又用国内外大量资料检验,符合精度要求。
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| 关 键 词： | 陆面蒸发量 |
| 收稿时间： | 1981-12-17 |
| 修稿时间： | 1987-05-03 |
A COMPUTATION OF LONGTERM AVERAGE LAND EVAPORATION |
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| Yang Yuandong. A COMPUTATION OF LONGTERM AVERAGE LAND EVAPORATION[J]. Geographical Research, 1987, 6(4): 62-69. DOI: 10.11821/yj1987040007 |
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| Authors: | Yang Yuandong |
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| Affiliation: | Hydrology Brucan, Yangtze Valley Planning Office |
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| Abstract: | The mothod for computing the longtcrm land evaporation in China is classified into three kinds in this peper. The first one belongs to a constant relationship. The second one gives a formula in which some parameters represent the effects of geography and climate.The thrid one can only be used in some special regions. Thus, the formula E/r = thD (E/r) is suggested to compute the longterm average evaporation in this paper.The suggested formula has been analysed and demonstrated in mathematics and in the concepts of climate and physics, and it is considered to be rational and feasible.This it, checked by a large amount of data in China and other countries meeting the heed of the precision. An analysis on some special climalical and geographical conditions and hydrolog ical effects is made for the parameter D which represents the affecting factor of various climates and underlying surfaces. |
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| Keywords: | land evaporation |
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