长江科学院院报 ›› 2013, Vol. 30 ›› Issue (4): 1-5.DOI: 10.3969/j.issn.1001-5485.2013.04.001

• 水资源与环境 •    下一篇

长江源区水循环机理探讨

陈 进   

  1. 长江科学院 院长办公室,武汉 430010
  • 收稿日期:2012-01-24 修回日期:2013-04-09 出版日期:2013-04-07 发布日期:2013-04-09
  • 作者简介:陈 进(1959-),男,湖北武汉人,教授级高级工程师,博士生导师,主要从事流域水资源研究,(电话)027-82829755(电子信箱)chenjin12342003@yahoo.com.cn。
  • 基金资助:

    “湖北省高端人才引领培养计划第一层次人选”项目资助(2012-2017)

Water Cycle Mechanism in the Source Region of Yangtze River

CHEN Jin   

  1. Yangtze River Scientific Research Institute, Wuhan 430010, China
  • Received:2012-01-24 Revised:2013-04-09 Online:2013-04-07 Published:2013-04-09

摘要:

长江源地区由于特殊的地理和气候环境,其水循环机理具有独特性,根据长江源地区气候、降水、冰川和冻土特点,分析了长江源大汽水、固态水和液态水三水转换机理。研究结果表明:长江源区虽然降水量少,但储存的固态水多,其独特的三水特点及转换机理构建了长江源地区脆弱的生态系统,一旦水循环机理变化,就会显著影响长江源的生态环境。

关键词: 长江源区, 降水, 水循环, 生态系统

Abstract:

Because of special geography and climate environment, the water circulation mechanism in the source of Yangtze River has a distinct characteristic. According to the features of climate, precipitation, glaciers and permafrost in the source region of Yangtze River, the transfer mechanisms among water vapor, solid water and liquid water are analyzed. Results show that despite the lack of rainfall in the source region of Yangtze River, there are huge amounts of solid water storage. Its unique characteristics of water conversion mechanism have constructed a fragile ecological system in the Yangtze River source. Once the water cycle mechanism changes, the ecological environment will be significantly affected.

Key words: the source region of Yangtze River , rainfall , water cycle , eco-system

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