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1960-2009年横断山区潜在蒸发量时空变化(英文)
引用本文:朱国锋,何元庆,蒲焘,王旭峰,贾文雄,李宗省,辛惠娟.1960-2009年横断山区潜在蒸发量时空变化(英文)[J].地理学报(英文版),2012,22(1):71-85.
作者姓名:朱国锋  何元庆  蒲焘  王旭峰  贾文雄  李宗省  辛惠娟
作者单位:State Key Laboratory of Cryosphere Sciences, Yulong Snow Mountain Glaciers and Environmental Obser-vation Station, Cold and Arid Regions Environmental and Engineering Research Institute, CAS;Graduate University of Chinese Academy of Sciences;Research School of Arid Environment and Climate Change, Lanzhou University;College of Geography and Environment Science, Northwest Normal University
基金项目:No.2010CB951404,National Natural Science Foundation of China,No.40971019,No.90511007,No.40801028,National Basic Research Program of China
摘    要:Based on the meteorological data of 20 stations in the Hengduan Mountains region during 1961-2009, the annual and seasonal variation of potential evapotranspiration was analyzed in combination with the Penman-Monteith model. With the method of Spline interpolation under ArcGIS, the spatial distribution of potential evapotranspiration was presented to research the regional difference, and the correlation analysis was used to discuss the dominant factor affecting the potential evapotranspiration. The results indicated that the an-nual potential evapotranspiration showed a decreasing tendency since the 1960s, especially from the 1980s to 1990s, while it showed an increasing tendency since 2000. Regional potential evapotranspiration showed a rate of -0.17 mm a?1. Potential evapotranspiration in north, middle and south of the Hengduan Mountains exhibited decreasing trends over the studied period, and its regional trend was on the decline from southwest to northeast.

关 键 词:potential  evapotranspiration  Spline  interpolation  Penman-Monteith  model  spatial  and  temporal  variations  Hengduan  Mountains

Spatial distribution and temporal trends in potential evapotranspiration over Hengduan Mountains region from 1960 to 2009
Guofeng Zhu,Yuanqing He,Tao Pu,Xufeng Wang,Wenxiong Jia,Zongxing Li,Huijuan Xin.Spatial distribution and temporal trends in potential evapotranspiration over Hengduan Mountains region from 1960 to 2009[J].Journal of Geographical Sciences,2012,22(1):71-85.
Authors:Guofeng Zhu  Yuanqing He  Tao Pu  Xufeng Wang  Wenxiong Jia  Zongxing Li  Huijuan Xin
Institution:1,2 1. State Key Laboratory of Cryosphere Sciences, Yulong Snow Mountain Glaciers and Environmental Obser-vation Station, Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou 730000, China; 2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3. Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China; 4. College of Geography and Environment Science, Northwest Normal University, Lanzhou 730070, China
Abstract:Based on the meteorological data of 20 stations in the Hengduan Mountains region during 1961–2009, the annual and seasonal variation of potential evapotranspiration was analyzed in combination with the Penman-Monteith model. With the method of Spline interpolation under ArcGIS, the spatial distribution of potential evapotranspiration was presented to research the regional difference, and the correlation analysis was used to discuss the dominant factor affecting the potential evapotranspiration. The results indicated that the annual potential evapotranspiration showed a decreasing tendency since the 1960s, especially from the 1980s to 1990s, while it showed an increasing tendency since 2000. Regional potential evapotranspiration showed a rate of −0.17 mm a−1. Potential evapotranspiration in north, middle and south of the Hengduan Mountains exhibited decreasing trends over the studied period, and its regional trend was on the decline from southwest to northeast.
Keywords:potential evapotranspiration  Spline interpolation  Penman-Monteith model  spatial and temporal variations  Hengduan Mountains
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