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云的含水量及其水循环
引用本文:张学文.云的含水量及其水循环[J].水科学进展,2002,13(1):83-86.
作者姓名:张学文
作者单位:新疆气象科学研究所, 新疆, 乌鲁木齐, 830002
摘    要:通过分析云的含水量表明:①全球的云中含水量约为90×109t,与大气中气体状态的水汽比,不足其1%,在计算大气总含水量时可以忽略;②积雨云含水分丰富,但是计算显示它持有的水分也少于3mm。③由于云的含水量很小,而每年有1000mm的雨雪从云中降落,所以云中的水分循环很快,从成云到致雨(雪)不足2h。

关 键 词:    含水量    水分循环
文章编号:1001-6791(2002)01-0083-04
收稿时间:2000-12-27
修稿时间:2000年12月27

Water content of cloud and its water circulation
ZHANG Xue-wen.Water content of cloud and its water circulation[J].Advances in Water Science,2002,13(1):83-86.
Authors:ZHANG Xue-wen
Institution:Xinjiang Institute of Meteorology, Wulumuqi 830002, China
Abstract:The calculation and analysis indicte that:(1)The total water content of global cloud is nearly 90×109 t,which is less than 1% comparing with the global vapor.So when calculating the amount of globe atmospheric water,the cloud water content can be ignored;(2)Cumulonimbus is abundant of water,but calculation shows that its precipitable water is less than 3 mm;and(3)There are 1 000 mm water precipitated from the cloud every year,but the precipitable water of cloud is exiguity,so water circulation is very quickly.The duration of a water element from the beginning of cloud to landing as rain is less than 2 hours.
Keywords:cloud  water content  water circulation  
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