期刊文献+

变化环境下的元谋干热河谷区水热响应分析 被引量:5

A Hydrothermal Analysis of Environment of Yuanmou Dry-hot River Valley in Jinsha River,Upper Yangtze River,China
下载PDF
导出
摘要 以变化环境影响下的脆弱区金沙江元谋干热河谷为研究对象,通过多种验证方法,研究气温、极端最高气温、极端最低气温、降水量、日降水量大于0.1 mm的日数和最大日降水量等水热指标对变化环境的响应规律。结果表明:从年际来看,自1956年以来,年均气温、极端最高气温均呈降低趋势,而极端最低气温则微弱升高,降水量、日降水量大于0.1 mm的日数和最大日降水量均为升高趋势;从年内来看,平均气温四季均为降低趋势,春季最显著,秋季最不明显,降水量四季均表现为增加趋势,其中春季最显著,冬季最不显著;从未来趋势来看,平均气温维持降低趋势的概率比升高的大,年降水量维持增加趋势的概率较转向降低趋势的概率要大,干热河谷有可能转为干暖或干温河谷。 Taking the Yuanmou dry-hot river valley of Jinsha River as the subject,which is a vulnerable area and affected by the environment.By a variety of methods,the discipline that the hydrothermal exponent response to the changing environment are studied.The hydrothermal exponent includes the annual temperature,extreme maximum temperature,extreme minimum temperature,precipitation,daily precipitation more than 0.1 mm and daily maximum precipitation.The results show that: Firstly,since 1956,annual average temperature and extreme maximum temperature showed a decreasing trend,while the extreme minimum temperature showed a slightly increasing trend,precipitation,daily precipitation more than 0.1 mm and the daily maximum precipitation are increasing trends;Secondly,average temperature in spring,summer,autumn and winter decreased,which is most significant in spring,and autumn is the least significant,rainfall in the four seasons showed an increasing trend,and the most significant was in spring,but winter was the least significant.Thirdly,for the future trend,the probability of maintaining the decreasing trend of the average annual temperature is better than the trend of increase,for the annual rainfall,the probability of maintaining an upward trend is more than the trend of reducing,which means that the dry-hot valley may become a warm and cool valley.
出处 《中国农村水利水电》 北大核心 2011年第2期39-42,共4页 China Rural Water and Hydropower
基金 国家自然科学基金-云南省人民政府联合基金重点资助项目(U0933604) 云南省自然科学基金资助项目(2009CD053)
关键词 水热响应 全球变化 气温 降水 元谋干热河谷 hydrothermal response global change temperature rainfall Yuanmou dry-hot river valley
  • 相关文献

参考文献8

  • 1明庆忠,史正涛.三江并流区干热河谷成因新探析[J].中国沙漠,2007,27(1):99-104. 被引量:54
  • 2ZHANG Jian ping, YANG Zhong, WANG Dao-jie, et al. Cli- mate change and causes in the Yuanmou dry--hot valley of Yun- nan, China [J ]. Journal of Arid Environments, 2002,51 (1) : 153 -162.
  • 3Andrew N Parsons, J E Barrett, Diana H Wall, et al. Soil carbon dioxide flux in antarctic dry valley ecosystems[J]. Ecosystems, 2004, (7): 286-295.
  • 4IPCC. IPCC Fourth Assessment Report (AR4)[M]. Cambridge: Cambridge University Press, 2007 : 2- 5.
  • 5气候变化国家评估报告编委会.气候变化国家评估报告[M].北京:科学出版社.2007.
  • 6Mandelbrot B B, Wallis J R. Some long-run properties of geographys- ical records[J]. Water Resource Research, 1969a, 5(2):321-340.
  • 7Mandelbrot B B, Wallis J R. Robustness of the rescaled range R/ S in the measurement of noncyclic long-run statistical dependence [J]. Water Resource Research, 1969b, 5 (4): 967-988.
  • 8Hurst H E, Black R P, Simaka Y M. Long-term Storage: An Experimental Study[M]. London, 1965:40-45.

二级参考文献8

  • 1明庆忠,史正涛,张虎才.三江并流区地貌与环境演化研究[J].热带地理,2006,26(2):119-122. 被引量:11
  • 2张荣祖,郑度,杨勤业,等.横断山干旱河谷[M].北京:科学出版社,1997:1—216.
  • 3杨勤业 郑度.横断山区干旱河谷的自然特点及其开发利用[J].干旱区资源与环境,1988,2(2):17-17.
  • 4Schwein U. The easten marches of high asia and river gorge country[C]//Trooll C. Landschaftsoekologie, der Hoehgebrige, Ewrasiens. Wiesbasen Erdwiss, Forschg, IV, 1972 : 276-287.
  • 5Liu Dongsheng, Geological and Ecological of Qinghai-Tibet Plateau[ M]. Beijing: Science Press: 1981.
  • 6文传甲.横断山区降水的时空分布特征[C]//高生淮,郑远昌,主编.横断山研究文集.成都:四川科学技术出版社,1989.
  • 7李吉均,方小敏.青藏高原隆起与环境变化研究[J].科学通报,1998,43(15):1568-1574. 被引量:377
  • 8何永彬,卢培泽,朱彤.横断山——云南高原干热河谷形成原因研究[J].资源科学,2000,22(5):69-72. 被引量:93

共引文献59

同被引文献79

引证文献5

二级引证文献75

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部