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金沙江河谷灌溉需水转折趋势分析

顾世祥,  何大明,  李远华,  崔远来,  李靖5

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文章导航 > 水科学进展  > 2008 >  19(3): 352-360
顾世祥, 何大明, 李远华, 崔远来, 李靖5. 金沙江河谷灌溉需水转折趋势分析[J]. 水科学进展, 2008, 19(3): 352-360.
引用本文: 顾世祥, 何大明, 李远华, 崔远来, 李靖5. 金沙江河谷灌溉需水转折趋势分析[J]. 水科学进展, 2008, 19(3): 352-360.
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GU Shi-xiang, HE Da-ming, LI Yuan-hua, CUI Yuan-lai, LI Jing. Agriculture irrigation water requirements change and R/S analysis of Jinshajiang dry-arid valley in recent 40 years[J]. Advances in Water Science, 2008, 19(3): 352-360.
Citation: GU Shi-xiang, HE Da-ming, LI Yuan-hua, CUI Yuan-lai, LI Jing. Agriculture irrigation water requirements change and R/S analysis of Jinshajiang dry-arid valley in recent 40 years[J]. Advances in Water Science, 2008, 19(3): 352-360.
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金沙江河谷灌溉需水转折趋势分析

  • 1.

    武汉大学水资源与水电工程科学国家重点实验室, 湖北, 武汉, 430072;

  • 2.

    云南省水利水电勘测设计研究院, 云南, 昆明, 650021;

  • 3.

    云南大学亚洲国际河流中心, 云南, 昆明, 650091;

  • 4.

    水利部农村水利司, 北京市, 100053;

  • 5.

    云南农业大学水利水电与建筑学院, 云南, 昆明, 650201

基金项目: 国家重点基础研究发展计划(973)资助项目(2003CB415105);云南省水资源综合规划专题研究(YSZY-2003-01,07)
详细信息
    作者简介:

    顾世祥(1972- ),男(彝族),云南镇雄人,高级工程师,博士,主要从事农业节水灌溉和水资源开发利用规划研究.E-mail:gushxang@public.km.yn.cn;gushxang@qq.com

  • 中图分类号: P467;S161

Agriculture irrigation water requirements change and R/S analysis of Jinshajiang dry-arid valley in recent 40 years

  • 1.

    State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan 430072, China;

  • 2.

    YunNan Institute of Water Resources and Hydropower Engineering Investigation, Design and Research, Kunming 650021, China;

  • 3.

    YunNan University, Kunming 650091, China;

  • 4.

    Department of Irrigation, Drainage and Rural Water Supply, MWR, Beijing 100053, China;

  • 5.

    YunNan Agriculture University, Kunming 650201, China

Funds: The study is financially supported by the National Basic Research Program of China(No.2003CB415105).

  • 摘要: 基于元谋、宾川、东川、祥云、楚雄及昆明等6个站1960-2000年的逐月气象数据及作物种植、农业耕作等资料,采用Mann-Kendall法和R/S分析法研究了金沙江干热河谷近40多年来的干湿变化及农业灌溉需水量转折变化趋势。结果表明,整个河谷内降水量增加、日照时数减少,气温却出现升高和降低两种趋势,气温在干热河谷内为下降,但在龙川江、鱼泡江、普渡河等支流的上游地区呈升高趋势,但ET0都显著降低,干湿指数、水稻及农业综合灌溉需水定额也都呈普遍下降的趋势;金沙江河谷及支流上游的气象因子、ET0、干湿指数、水稻灌溉及农业综合灌溉定额系列的转折变化集中在20世纪70年代末~80年代初、80年代末~90年代初两个时段,在降水量最小的宾川站,对气候变化的响应更为敏感。
    Abstract: Based on the monthly climate records of Yuanmou,Binchan,Dongchuan,Xiangyun,Chuxiong,and Kunming stations in the period 1960-2000,as well as crop pattern and cultivate data in 2000,the Mann-Kendall trend and the Rescaled Range Analysis(abbr.R/S)method are adopted to research the tendency in aridity-humidity and irrigation water requirements in Jinshajiang dryarid valley in the last 40 years. The results show that the precipitation and the temperature decrease,and sunshine hours increase in the valley. But the temperature increases in the branch upstream of Longchuanjiang,Yupaojiang, Puduhe,etc,thus,results in ET0 decreases remarkable in Jinshajiang basin. Furthermore,the aridity-humidity index,paddy irrigation quota and total agriculture irrigation quota also decreases. The turn point of climate factors,ET0,aridity-humidity index,paddy irrigation quota and total agriculture irrigation quota in Jinshajiang valley are focused the late 1970s-1980s and the late 1980s the early 1990s,and Binchuan station which occurs minimum precipitation is most sensitivity to climates change.
  • [1] 秦大河,罗勇,陈振林,等.气候变化科学的最新进展:IPCC第四次评估综合报告解析[J].气候变化研究进展,2007,3(6):311-314.(QIN Da-he,LUO Yong,CHEN Zhen-lin,et al.Latest advances in climate change sciences:Interpretation of the synthesis report of the IPCC fourth assessment report[J].Adv Clim Change Res,2007,3(6):311-314.(in Chinese))
    [2] 丁一汇,任国玉,石广玉,等.气候变化国家评估报告(Ⅰ):中国气候变化的历史和未来趋势[J].气候变化研究进展,2006,2(1):3-8.(DING Yi-hui,REN Guo-yu,SHI Guang-yu,et al.National assessment report of climate change (I):Climate change in China and its future trend[J].Adv Clim Change Res,2006,2 (1):3-8.(in Chinese))
    [3] 林而达,许吟隆,蒋金荷,等.气候变化国家评估报告(Ⅱ):气候变化的影响与适应[J].气候变化研究进展,2006,2(2):51-56.(LIN Er-da,XU Ying-long,JIANG Jin-he,et al.National assessment report of climate change (Ⅱ):Climate change impacts and adaptation[J].Adv Clim Change Res,2006,2(2):51-56.(in Chinese))
    [4] 王绍武,罗勇,闻新宇,等.近千年全球温度变化研究的新进展[J].气候变化研究进展,2007,3(1):14-19.(WANG Shao-wu,LUO Yong,WEN Xin-yu,et al.Latest advances in studies of the global temperature variations for the last millennium[J].Adv Clim Change Res,2007,3(1):14-19.(in Chinese))
    [5] 马柱国,符淙斌.20世纪下半叶全球干旱化的事实及其大尺度背景的联系[J].中国科学D辑,2007,37(2):222-214.(MA Zhu-guo,FU Zong-bin.Evidences of drying trend in the global during the later half of 20th Century and their relationship with large-scale climate background[J].Science in China Series D,2007,50 (5):776-788.(in Chinese))
    [6] 马柱国,符宗斌.1951-2004年中国北方干旱化的基本事实[J].科学通报,2006,51(20):2 429-2 439.(MA Zhu-guo,FU Cong-bin.Some evidence of drying trend over northern China from 1951 to 2004[J].Chinese Science Bulletin,2006,51 (23):2 913-2 925.(in Chinese))
    [7] 马柱国,任小波.1951-2006年中国区域干旱化特征[J].气候变化研究进展,2007,3(4):195-201.(MA Zhu-guo,REN Xiao-bo.Drying trend over China from 1951 to 2006[J].Adv Clim Change Res,2007,3 (4):195-201.(in Chinese))
    [8] 施晓辉,徐祥德.中国大陆冬夏气候型年代际转折的区域结构特征[J].科学通报,2006,51(17):2 075-2 084.(SHI Xiao-hui,XU Xiang-de.Regional characteristics of the interdecadal turning of winter/summer climate modes in Chinese mainland[J].Chinese Science Bulletin,2007,52 (1):101-112.(in Chinese))
    [9] 张磊,廖启龙.青藏高原近40年来的降水变化特征[J].干旱区地理,2007,30(2):240-246.(ZHANG Lei,LIAO Qi-long.Precipitation changes in the Tibetan plateau during the last four decades[J].Arid Land Geography,2007,30(2):240-246.(in Chinese))
    [10] 张建云,章四龙,王金星,等.近50年来中国六大流域年际径流变化趋势研究[J].水科学进展,2007,18(2):230-234.(ZHANG Jian-yun,ZHANG Si-long,WANG Jin-xing,et al.Study on runoff trends of the six larger basins in China over the past 50 years[J].Advances in Water Science,2007,18(2):230-234.(in Chinese))
    [11] 姜彤,苏布达,王艳君,等.四十年来长江流域气温降水及径流变化趋势[J].气候变化研究进展,2005,1(2):65-68.(JIANG Tong,SU Bu-da,WANG Yan-jun,et al.Trends of temperature,precipitation and runoff in the Yangtze River basin from 1961 to 2000[J].Adv Clim Change Res,2005,1(2):65-68.(in Chinese))
    [12] 刘晓冉,李国平,范广洲,等.我国西南地区1960-2000年降水资源变化的时空特征[J].自然资源学报,2007,22(5):76-87.(LIU Xiao-ran,LI Guo-ping,FAN Guang-zhou,et al.Spatial and temporal characteristics of precipitation resources in southwest China during 1961-2000[J].Journal of Natural Resources,2007,22(5):76-87.(in Chinese))
    [13] 刘晓英,林而达.气候变化对华北地区主要作物需水量的影响[J].水利学报,2004,35(2):77-83.(LIU Xiao-ying,LIN Er-da.Impact of climate change on water requirement of main crops in North China[J].Journal of Hydraulic Engineering,2004,35(2):77-83.(in Chinese))
    [14] 徐长春,陈亚宁,李卫红,等.塔里木河流域近50年气候变化及其水文过程响应[J].科学通报,2006,51(增刊1):21-30.(XU Chang-chun,CHEN Ya-ning,LI Wei-hong,et al.Climate change and hydrologic process response in the Tarim river basin over the past 50 years[J].Chinese Science Bulletin,2006,51(SupplementⅠ):25-36.(in Chinese))
    [15] 丁永建,叶柏生,韩添丁,等.过去50年中国西部气候和径流变化的区域差异[J].中国科学D辑,2007,37(2):206-233.(DING Yong-jian,YE Bo-sheng,HAN Tian-ding,et al.Regional difference of annual precipitation and discharge variation over west China during the last 50 years[J].Science in China Ser,D Earth Sciences,2007,50 (6):936-945.(in Chinese))
    [16] 王国杰,姜彤,陈桂亚.长江干流径流的时序结构与长期记忆[J].地理学报,2006,61(1):47-56.(WANG Guo-jie,JIANG Tong,CHEN Gui-ya.Structure and long-term memory of discharge series in Yangtze River[J].Acta Geographica Sinica,2006,61(1):47-56.(in Chinese))
    [17] 吴益,程维明,任立良,等.新疆和田河流域河川径流的时序特征分析[J].自然资源学报,2006,21(3):375-381.(WU Yi,CHENG Wei-ming,REN Li-liang,et al.Analysis on the characteristics of annual runoff in Hotan catchment[J].Journal of Natural Resources,2006,21(3):375-381.(in Chinese))
    [18] YUE S,PILON P,PHINNEY B,et al.Power of the Mann-Kendall and Spearman's rho tests for detecting monotonic trends in hydrological series[J].Journal of Hydrology,2002,259:254-271.
    [19] 赵晶,王乃昂.近50年来兰州城市气候变化的R/S分析[J].干旱区地理,2002,25(1):90-94.(ZHAO Jin,WANG Nai-ang.R/S analysis of urbanization effect on climate in Lanzhou[J].Arid Land Geography,2002,25(1):90-94.(in Chinese))
    [20] 王孝礼,胡宝清,夏军.水文时序趋势与变异点的R/S分析[J].武汉大学学报(工学版),2002,35(2):10-12.(WANG Xian-Li,HU Bao-qing,XIA Jun.R/S analysis method of trend and aberrance point on hydrological time series[J].Journal of Wuhan University (Engineering Science Edition),2002,35(2):10-12.(in Chinese))
    [21] 张荣祖.横断山区干旱河谷[M].北京:科学出版社,1996.145-157.(ZHANG Rong-gzu.Arid valley in Hengduan Mountainous plateau[M].Beijing:Science Press,1996.145-157.(in Chinese))
    [22] 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.(HE Yong-bin,LU Pei-ze,ZHU Tong.Causes for the formation of dry-hot valleys in Hengduan Mountain-Yunnan plateau[J].Journal of Resources Science,2000,22(5):69-72.(in Chinese))
    [23] FENG Y,HE D M.Research progress on international rivers in Asia[J].Journal of Geographical Sciences,2006,16(3):271-276.
    [24] 何大明,吴绍洪,欧晓昆,等.纵向岭谷区生态系统变化及西南跨境生态安全研究进展[J].地理学报,2007,62(1):93-100.(HE Da-ming,WU Shao-hong,OU Xiao-kun,et al.Acta Geographica Sinica.Research progress in the Longitudinal Range-Gorge Region (LRGR) ecosystem changes and trans-boundary ecological safety in southwest China[J].Acta Geographica Sinica,2007,62(1):93-100.(in Chinese))
    [25] ALLEN R G,PEREIRA L S,RAES D,et al.Crop evapotranspiration:guideline for computing crop requirement[M].FAO Irrigation and Drainage Paper No 56,Rome,Italy,1998.51-202.
    [26] CLARKE D.Crop wat for Windows:User Guide[M].England:University of Southampton,1998.1-40.
    [27] 刘钰,PEREIRA L S,TEIXEIRA J L,等.参照腾发量的新定义及计算方法对比[J].水利学报,1997,28(6):27-33.(LIU Yu,Pereira L S,TEIXEIRA J L,et al.Update definition and computation of reference evapotranspiration comparison with former method[J].Journal of Hydraulic Engineering,1997,28(6):27-33.(in Chinese))
    [28] 郭元裕主编.农田水利学(第三版)[M].北京:中国水利水电出版社,1998.18-74.(GUO Yuan-yu.Irrigation and Drainage Engineering[M].Beijing:China WaterPower Press,1998.18-74.(in Chinese))
    [29] 顾世祥,傅骅,高嵩,等.低纬度高原区农业灌溉需水规律研究[J].灌溉排水学报,2004,23(4):71-74.(GU Shi-xiang,FU Hua,GAO Song,et al.Research on low latitude plateau irrigation district agriculture irrigation water rule[J].Journal of Irrigation and Drainage.2004,23(4):71-74.(in Chinese))
    [30] 张万诚,万云霞,肖子牛.中国西南纵向岭谷区近百年来降水的时空变化特征[J].自然资源学报,2006,21(5):802-809.(ZHANG Wan-cheng,WAN Yun-xia,XIAO Zi-niu.The spatio-temporal variations of the longitudinal range-gorge region (LRGR) precipitation in recent 100 years in southwest China[J].Journal of Natural Resources,2006,21(5):802-809.(in Chinese))
    [31] 尤卫红,段长春,何大明,等.纵向岭谷作用下的干湿气候差异及其对跨境河川径流量的影响[J].科学通报,2006,51(增刊2):56-65.(YOU Wei-hong,DUAN Chang-chun,HE Da-ming,et al.Climatic difference in dry and wet season under effect of the longitudinal range-gorge and its influence on transboundary river runoff[J].Chinese Science Bulletin,2006,51(Supplement Ⅱ):69-79.(in Chinese))
    [32] 吴绍洪,尹云鹤,郑度,等.近30年中国陆地表层干湿状况研究[J].中国科学D辑,2005,35(3):276-283.(WU Shao-hong,YIN Yun-he,ZHENG Du,et al.Aridity/ humidity status of land surface in China during the last three decades[J].Science in China Ser.D Earth Sciences,2005,48(9):1 510-1 518.(in Chinese))
    [33] 顾世祥,何大明,崔远来,等.纵向岭谷区灌溉需水空间变异性及其与"通道-阻隔"作用的关系[J].科学通报,2007,52(增刊Ⅱ):29-36.(GU Shi-xiang,HE Da-ming,CUI Yuan-lai,et al.Spatial variability of irrigation factors and their relationships with "corridor-barrier" functions in the longitudinal range-gorge region[J].Chinese Science Bulletin,2007,52(Supplement Ⅱ):33-41.(in Chinese))
    [34] 王顺久.全球气候变化对水文水资源的影响[J].气候变化研究进展,2006,2(5):223-227.(WANG Shun-jiu.Impacts of global climate change on hydrology and water Resources[J].Adv Clim Change Res,2006,2(5):223-227.(in Chinese))
    [35] 丛振涛,倪广恒,杨大文,等."蒸发悖论"在中国的规律分析[J].水科学进展,2008,19(2):147-152.(CONG Zhen-tao,NI Guang-heng,YANG Da-wen,et al.Evaporation paradox in China[J].Advances in Water Science,2008,19(2):147-152.(in Chinese))
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    [14] 黄永基, 陈晓军.  我国水资源需求管理现状及发展趋势分析 . 水科学进展, 2000, 11(2): 215-220.
    [15] 张世法.  对“对‘径流的趋势分析和概率预测’一文的商榷”的答复 . 水科学进展, 1997, 8(4): 389-389.
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    [19] 张世法, 崔新文.  径流的趋势分析和概率预测 . 水科学进展, 1995, 6(1): 22-28.
    [20] 李远华.  水稻需水量预报研究 . 水科学进展, 1991, 2(2): 127-132.
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  • 收稿日期:  2007-11-15
  • 刊出日期:  2008-05-25

金沙江河谷灌溉需水转折趋势分析

  • 1. 武汉大学水资源与水电工程科学国家重点实验室, 湖北, 武汉, 430072;
  • 2. 云南省水利水电勘测设计研究院, 云南, 昆明, 650021;
  • 3. 云南大学亚洲国际河流中心, 云南, 昆明, 650091;
  • 4. 水利部农村水利司, 北京市, 100053;
  • 5. 云南农业大学水利水电与建筑学院, 云南, 昆明, 650201
    • 基金项目:  国家重点基础研究发展计划(973)资助项目(2003CB415105);云南省水资源综合规划专题研究(YSZY-2003-01,07)
    作者简介:

    顾世祥(1972- ),男(彝族),云南镇雄人,高级工程师,博士,主要从事农业节水灌溉和水资源开发利用规划研究.E-mail:gushxang@public.km.yn.cn;gushxang@qq.com

  • 收稿日期: 2007-11-15
  • 刊出日期: 2008-05-25

  • 中图分类号: P467;S161

摘要: 基于元谋、宾川、东川、祥云、楚雄及昆明等6个站1960-2000年的逐月气象数据及作物种植、农业耕作等资料,采用Mann-Kendall法和R/S分析法研究了金沙江干热河谷近40多年来的干湿变化及农业灌溉需水量转折变化趋势。结果表明,整个河谷内降水量增加、日照时数减少,气温却出现升高和降低两种趋势,气温在干热河谷内为下降,但在龙川江、鱼泡江、普渡河等支流的上游地区呈升高趋势,但ET0都显著降低,干湿指数、水稻及农业综合灌溉需水定额也都呈普遍下降的趋势;金沙江河谷及支流上游的气象因子、ET0、干湿指数、水稻灌溉及农业综合灌溉定额系列的转折变化集中在20世纪70年代末~80年代初、80年代末~90年代初两个时段,在降水量最小的宾川站,对气候变化的响应更为敏感。

English Abstract

顾世祥, 何大明, 李远华, 崔远来, 李靖5. 金沙江河谷灌溉需水转折趋势分析[J]. 水科学进展, 2008, 19(3): 352-360.
引用本文: 顾世祥, 何大明, 李远华, 崔远来, 李靖5. 金沙江河谷灌溉需水转折趋势分析[J]. 水科学进展, 2008, 19(3): 352-360.
shu
GU Shi-xiang, HE Da-ming, LI Yuan-hua, CUI Yuan-lai, LI Jing. Agriculture irrigation water requirements change and R/S analysis of Jinshajiang dry-arid valley in recent 40 years[J]. Advances in Water Science, 2008, 19(3): 352-360.
Citation: GU Shi-xiang, HE Da-ming, LI Yuan-hua, CUI Yuan-lai, LI Jing. Agriculture irrigation water requirements change and R/S analysis of Jinshajiang dry-arid valley in recent 40 years[J]. Advances in Water Science, 2008, 19(3): 352-360.
shu

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