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中国沙漠 ›› 1984, Vol. 4 ›› Issue (4): 33-40.

• 中关沙澳科学讨论会论文 • 上一篇    下一篇

中国西北地区的干旱气候及水热资源的调节

陈仲全, 何友松, 严江平   

  1. 西北师范学院地理系
  • 出版日期:1984-12-20 发布日期:1984-12-20

Arid Climate and the Regulation of the Hydrotherma Resources in the Northwest China

Chen Zhongquan, He Yousong, Yan Jiangping   

  1. Geography Department, Northwestern Teachers' University
  • Online:1984-12-20 Published:1984-12-20

摘要: 本文用干燥度(K')和干燥率(D)表征西北干旱气候、干燥程度并进行了干旱气候区划,有助于了解西北干旱气候的的结构与分布。用月干燥度和湿润指数距平百分率(S%)分析年内干湿动态及干旱年变动的韵律性,有利于把握干旱动态的总趋势。为了合理利用西北干旱区水热资源,从调节水热资源的观点提出了计算合理蒸散(E0.4)、合理灌溉深度(g0.4)和合理灌溉定额(Q0.4)的公式,并以西北干旱区为例作了计算与论证。

关键词: 水热资源, 西北干旱区, 中国西北地区, 湿润指数, 距平, 干燥程度, 气候区划, 年平均, 干燥度, 月平均

Abstract: In this paper, the aridity index (K') and the radiational index of dryness (D) are used to show the extent of dryness in the Northwestern part and to make division of arid climate, It is useful to do so for understanding the structure and distribution of the arid climate, in Northwestern The mean monthly aridity index and the anomaly per cent of the moisture index (S%) are used to analysed the dynamics of dry and wet variation in a year and the rhythm revolution of the dry years, It is advantageous to do so for comprehending the total trend of the drought variation. In order to use the hydrothermal resources rationally in the North west arid area, an equation, from the viewpoint of the rational evapotranspiration (E0.4), the depth of the rational irrigation (G0.4) and the standard of the rational irrigation (Q0.4), is presented through the actual evapotranspiration (AE) the Bawen ratio (β) and the net radiation (Rt) from the viewpoint of the regulation of the hydrothermal resources.