中国北方干旱半干旱地区的气象条件有利于土壤凝结水的形成。
The micro-meteorological conditions are advantageous for forming soil condensate in arid and semiarid regions in north China.
中国的农业重旱省区与气象干旱区不相吻合，雨水较丰的湖南、湖北两省单位耕地面积的多年平均受旱程度亦很严重。
The heavy agricultural drought areas of China do not match with the meteorological drought areas. The average drought degree over years in Hunan and Hubei province of a plenty of rain is also serious.
中国气象学家将近年的干旱解释为气候变化。
Several Chinese meteorologists in recent years have linked drought to climate change.
应用推荐