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1)  aridification
干暖化
1.
Preliminary analysis of aridification impact on irrigation water consumption in Ningmeng irrigation area of the upper Yellow river;
干暖化对黄河上游宁蒙灌区灌溉耗水量影响初析
2)  Warm-dry and warm-wet tendency
暖干(湿)化
3)  warming-drying trend
暖干化
1.
From 1990s,the features of climatic warming-drying trend was very remarkable on the whole in Guanzhong Plain,it was the same to the east and west.
20世纪90年代以来,关中平原整体上气候暖干化特征显著,东西部地区也呈现暖干化,中部近年来呈现暖湿化,同时关中暖春、暖冬化,春旱、秋旱等也愈加显著。
2.
The results show that the annual temperature and seasonal temperature were obviously increased in recent 51 years,the annual and summer precipitations were significantly decreased,aridity was also decreased gradually,warming-drying trend was obvious,and the aridity was abruptly changed in 1989.
结果表明:51年来额济纳旗年、季平均气温均明显上升,年降水量及夏季降水量呈明显下降趋势,干燥度亦呈逐渐下降趋势,气候暖干化趋势明显,干燥度在1989年发生了突变。
4)  warming and drying trend
暖干化趋势
1.
Overall,the climate condition on Hulunbeier sandy land had a warming and drying trend.
结果表明:呼伦贝尔沙地总体气候暖干化趋势显著;气温逐年升高、降水量减少、蒸发量增加和极端气候事件增多,使流动沙地面积不断增加,植被盖度下降。
5)  drying and warming of climatic
气候干暖化
6)  drier and warmer characteristics
暖干化特征
补充资料:公理化方法(见公理化和形式化)


公理化方法(见公理化和形式化)
axiomatical method

  gongllbuafangfa公理化方法化和形式化。(axiomatieal method)见公理
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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