globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6380066
论文题名:
空中水资源及其降水转化分析
其他题名: Atmospheric water resource and precipitation conversion
作者: 李家叶1; 李铁键2; 王光谦2; 魏加华2; 钟德钰2; 苏洋1; 傅旭东1
刊名: 科学通报
ISSN: 0023-074X
出版年: 2018
卷: 63, 期:26, 页码:605-613
语种: 中文
中文关键词: 空中水资源 ; 白水 ; 降水效率 ; 降水转化率 ; 空地耦合
英文关键词: atmospheric water resource ; white water ; precipitation efficiency ; precipitation conversion ratio ; atmosphericearth surface coupling
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 本文在回顾空中水资源利用的愿景和相关研究成果、分析空中水资源的概念和内涵的基础上,定义了白水,用以代表空中水资源.白水指的是通过地表某处上空的统计意义上具备降水潜力的水物质通量.白水和其他水资源一样,一般表述为年度水量,其本质是水物质的更新通量.将空中水物质的水平运动垂直积分投影到地表二维空间,对于地表任一点,白水的量纲为[L~2 T~(-1)],与地表水资源常用的[L~3 T~(-1)]不同.将某地的降水通量与相应时段的白水的比值定义为白水降水效率,量纲为L~(-1),代表白水每运动单位距离产生的降水量占其自身的比例.将白水概念扩展到地表流域,则可通过沿流域边界积分得到进入某一流域的白水,量纲为[L~3 T~(-1)].将该流域上空全部白水输送路径上的降水效率沿各自路径积分后加权平均,即得到流域的白水降水转化率(无量纲)为流域内的降水占进入该流域的白水的比例,可以采用降水量除以白水与径流量的1/2之差来近似计算.本文采用再分析数据研究了我国大陆附近的白水降水效率的空间分布特征,并选择长江、黄河、珠江、三江源流域开展相关特征参量对比分析.结果表明,白水降水效率是反映气候和地理条件的降水转化能力的公允度量,可直接用于不同地区的对比分析;流域的白水降水转化率可用于分析流域空地水资源循环中的数量关系.研究和评估白水及其降水转化特征,是空地水资源耦合分析及空中水资源开发利用的基础.通过技术手段提高局部地区的白水降水转化率,并与地表水利工程联合调控,有望实现一定规模的空地水资源耦合利用,是水资源开源的新机遇.
英文摘要: The concept of water resources is largely limited only to water in rivers, lakes, underground aquifers, and other sources that can be used by humans directly--blue water. It does not normally include water that directly evaporates from the land surface and transpires from vegetation--green water. Generally speaking, the sum of blue water and green water is equivalent to total precipitation. Considering the global land surface, as much as about 65% of the total precipitation is converted into green water, and only the remaining 35% is converted into blue water. The concept of green water clearly extends the scope of research and management of water resources to the total amount of land precipitation, but the source of terrestrial water resources has not been intensively studied. In terms of a complete water cycle, water resources should refer to the renewal/replenishment of the fluxes of fresh water in different processes in the hydrosphere. The storage of water in the atmosphere is relatively small, but the huge flux of water transport in the atmosphere is the fundamental source of terrestrial water resources. In the contexts of existing water shortages, future water demands (including for ecological protection), and global climate change impacts on water resources, accurate quantitative studies on the formation of terrestrial water resources from the atmosphere are becoming increasingly important. Such studies require a clear definition of the concept of atmospheric water resource and particular focus on its precipitation conversion. Such research can indeed enhance our theoretical knowledge about the functions of water resources systems and further broaden our view of traditional water resources management. Motivated by this, the present paper attempts to improve our understanding of atmospheric water resources. This is done through: (1) a review of the concept of atmospheric water resource; (2) proposing a quantitative estimation method for atmospheric water resource; and (3) quantifying the precipitation conversion characteristics of atmospheric water resources. For a given period of time, we define the atmospheric water resource as the accumulated atmospheric water matter with potential to precipitate, and call it as white water.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/154376
Appears in Collections:气候变化事实与影响

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作者单位: 1.清华大学, 水沙科学与水利水电工程国家重点实验室, 北京 100084, 中国
2.清华大学
3.青海大学
4.三江源协同创新中心, 水沙科学与水利水电工程国家重点实验室
5.三江源生态与高原农牧业国家重点实验室
6.三江源协同创新中心,
7.西宁
8.西宁, 北京
9.100084
10.810016
11.810016, 中国

Recommended Citation:
李家叶,李铁键,王光谦,等. 空中水资源及其降水转化分析[J]. 科学通报,2018-01-01,63(26):605-613
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