Agricultural influences on evaporation paradox in China

被引:0
|
作者
Han S. [1 ,2 ]
Wang S. [1 ,2 ]
Yang D. [3 ]
机构
[1] Department of Irrigation and Drainage, China Institute of Water Resources and Hydropower Research
[2] National Center of Efficient Irrigation Engineering and Technology Research
[3] State Key Laboratory of Hydro-Science and Engineering, Department of Hydraulic Engineering, Tsinghua University
关键词
Agricultural influence; Air temperature; Climate change; Evaporation paradox; Pan evaporation;
D O I
10.3969/j.issn.1002-6819.2010.10.001
中图分类号
学科分类号
摘要
The air temperature increased and the pan evaporation decreased from 1960 to 2001 in China, and the evaporation paradox exist. Using the data from 251 meteorological stations in regions without significant agricultural influences and from 165 meteorological stations in regions with significant agricultural influences divided by land use, the trends of pan evaporations and air temperature changes from 1960 to 2001 were evaluated contrastively. The differences of evaporation paradox in regions with different agricultural influences in China were analyzed. The increasing trends of air temperature over meteorological stations in regions with significant agricultural influences were weaker than that in regions without significant agricultural influences, while the pan evaporation appeared decreasing trends, and the differences were more obvious in arid or semi-arid areas in North China. The differences of evaporation paradox over different agricultural regions were influenced by agricultural activities such as irrigation, and should be taken into account.
引用
收藏
页码:1 / 8
页数:7
相关论文
共 36 条
  • [1] Climate Change 2007, (2007)
  • [2] Peterson T., Golubev V., Groisman P., Evaporation losing its strength, Nature, 393, pp. 687-688, (1995)
  • [3] Roderick M.L., Farquhar G.D., Changes in Australian pan evaporation from 1970 to 2002, International Journal of Climatology, 24, 9, pp. 1077-1090, (2004)
  • [4] Chattopadhyay N., Hulme M., Evaporation and potential evapotranspiration in India under conditions of recent and future climate change, Agricultural and Forest Meteorology, 87, 1, pp. 55-73, (1997)
  • [5] Roderick M.L., Farquhar G.D., The cause of decreased pan evaporation over the past 50 years, Science, 298, pp. 1410-1411, (2002)
  • [6] Xu J., Shigenori H., Kazuyuki S., Et al., Surface heat balance and pan evaporation trends in Eastern Asia in the period 1971-2000, Hydrological Processes, 19, 11, pp. 2161-2186, (2005)
  • [7] Brutsaert W., Hydrologic M., Cycle explains the evaporation paradox, Nature, 396, (1998)
  • [8] Cohen S., Ianetz A., Stanhill G., Evaporative climate changes at Bet Dagan, Israel, 1964-1998, Agricultural and Forest Meteorology, 111, 2, pp. 83-91, (2002)
  • [9] Ren G., Guo J., Change in pan evapration and the influential factors over China: 1956-2000, Journal of Natural Resources, 21, 1, pp. 31-44, (2006)
  • [10] Han S., Hu H., Yang D., Et al., Differences in changes of potential evaporation in the mountainous and oasis regions of the Tarim basin, northwest China, Science in China Series E: Technological Sciences, 52, 7, pp. 1981-1989, (2009)