Temporal and Spatial Change Analysis of the Sensitivity of Potential Evapotranspiration to Meteorological Influencing Factors in China

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  • 1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
    2. College of Resources and Environment, Beijing Normal University, Beijing 100875, China;
    3. Graduate University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2011-03-16

  Revised date: 2011-04-06

  Online published: 2011-05-20

Supported by

National Natural Science Foundation of China, No.40971023; National Basic Research Program of China, No.2010CB428406

Abstract

Potential evapotranspiration (E0), as an estimate of the evaporative demand of the atmosphere, has been widely discussed in researches on irrigation management, crop water demand and predictions in ungauged basins (PUBs). Analysis of the sensitivity of E0 to meteorological factors is the basic research on the impact of climate change on water resources, and also is important to the optimal allocation of agricultural water resources. In this study, the calculation method of global radiation in Penman-Monteith formula was improved by optimazation, and the sensitivities of Penman-Monteith potential evapotranspiration to the daily maximum temperature (STmax), daily minimum temperature (STmin), wind speed (SU2), global radiation (SRs) and vapor pressure (SVP) were calculated and analyzed based on the long-term meteorological data at 653 meteorological stations in China during the period 1961-2000. The results are obtained as follows. (1) The multiple correlation coefficient between E0 and pan evaporation increased from 0.61 to 0.75 using the improved Penman-Monteith formula. Trend analysis shows that E0 had the decreasing trends in eight basins of China, which indicates that "pan evaporation paradox" common existed in China from 1960 to 2007. (2) Spatially, Tmax was the most sensitive variable in the Haihe River, Yellow River, Huaihe River, Yangtze River, Pearl River and river basins in southeastern China, and VP was the most sensitive variable in the Songhua River Basin, Liaohe River Basin and river basins in Northwest China, while Rs was the most sensitive variable in river basins of Southwest China. For the national average, the most sensitive variable was VP, followed by Tmax, Rs, U2 and Tmin. In addition, the changes in sensitivity coefficients had certain correlation with elevation. (3) Temporally, the maximum values of STmax and SRs occurred in July, while the maximum values of STmin, SVP and SU2 occurred in January. Moreover, trend analysis indicates that STmax had decreasing trends, while STmin, SU2, SRs and SVP had increasing trends.

Cite this article

LIU Changming, ZHANG Dan . Temporal and Spatial Change Analysis of the Sensitivity of Potential Evapotranspiration to Meteorological Influencing Factors in China[J]. Acta Geographica Sinica, 2011 , 66(5) : 579 -588 . DOI: 10.11821/xb201105001

References

[1] Allen R G, Pereira L S, Raes D et al. Crop evapotranspiration-guidelines for computing crop water requirements. FAOIrrigation and Drainage Paper 56. FAO, 1998.



[2] Liu C M, Zhang X Y, Zhang Y Q. Determination of daily evaporation and evapotranspiration of winter wheat and maize bylarge-scale weighing lysimeter and micro-lysimeter. Agricultural and Forest Meteorology, 2002, 111: 109-120.



[3] Guo S L, Guo J, Zhang J et al. VIC distributed hydrological model to predict climate change impact in the Hanjiang Basin.Science China: Series E, 2009, 52(11): 3234-3239.



[4] Liu Changming; Sun Rui. Ecological aspects of water cycle: Advances in soil vegetation atmosphere of energy and waterfluxes. Advances in Water Science, 1999, 10(3): 23-28. [刘昌明, 孙睿. 水循环的生态学方面: 土壤—植被—大气系统水分能量平衡研究进展. 水科学进展, 1999, 10(3): 23-28.]



[5] Peterson T C, Golubev V S, Groisman PY. Evaporation losing its strength. Nature, 1995, 377: 687-688.



[6] Liu Changming, Zeng Yan. Changes of pan evaporation in the recent 40 years in the Yellow River Basin. WaterInternational, 2004, 29(4): 510-516.



[7] BrutsaertW, Parlange M B. Hydrologic cycle explains the evaporation paradox. Nature, 1998, 396: 30.



[8] Saxton K E. Sensitivity analysis of the combination evapotranspiration equation. Agricultural and Meteorology, 1975, 15(3): 343-353.



[9] Hupet F, Vanclooster M. Effect of the sampling frequency of meteorological variables on the estimation of the referenceevapotranspiration. Journal of Hydrology, 2001, 243: 192-204.



[10] Gong L B, Xu C Y, Chen D L et al. Sensitivity of the Penman-Monteith reference evapotranspiration to key climaticvariables in Changjiang (Yangtze River) Basin. Journal of Hydrology, 2006, 329: 620-629.



[11] Liu Xiaomang, Zheng Hongxing, Liu Changming et al. Sensitivity of the potential evapotranspiration to key climaticvariables in the Haihe River Basin. Resources Science, 2009, 31(9): 1470-1476. [刘小莽, 郑红星, 刘昌明等. 海河流域潜在蒸散发的气候敏感性分析. 资源科学, 2009, 31(9): 1470-1476.]



[12] Chen D, Gao G., Xu C Y et al. Comparison of Thornthwaite method and pan data with the standard Penman-Monteithestimates of potential evapotranspiration for China. Climate Research, 2005, 28: 123-132.



[13] Zeng Yan, Qiu Xinfa, Pan Aoda et al. Distributed modeling of global solar radiation over rugged terrain of the YellowRiver Basin. Advances in Earth Science, 2008, 23(11): 1185-1193. [曾燕, 邱新法, 潘敖大等. 地形对黄河流域太阳辐射影响的分析研究. 地球科学进展, 2008, 23(11): 1185-1193.]



[14] Qian T, Dai A, Trenberth K E et al. Simulation of global land surface conditions from 1948-2004 (Part I): Forcing data andevaluation. Hydrometeorology, 2006, 7(5): 953-975.



[15] Roderick M L, Rotstayn L D, Farquhar G D et al. On the attribution of changing pan evaporation. Geophysical ResearchLetters, 2007, 34, L17403, doi: 10.1029/2007GL031166.



[16] Zheng H, Liu X, Liu C et al. Assessing contributions to panevaporation trends in Haihe River Basin, China. Geophys. Res.2009, 114: D24105, doi: 10.1029/2009JD012203.



[17] McCuen R H. A sensitivity and error analysis of procedures used for estimating evaporation. Water Resource Bulletin,1974, 10(3): 486-498.



[18] Shi Neng, Chen Jiaqi, Tu Qipu. 4-phase climate change features in the last 100 years over China. Acta MeteorologicaSinica, 1995, 53(4): 431- 439. [施能, 陈家其, 屠其璞. 中国近100 年来4 个年代际的气候变化特征. 气象学报, 1995, 53 (4): 431- 439.]



[19] Sun Peng, Zhang Qiang, Chen Xiaohong et al. Spatio-temporal patterns of sediment and runoff changes in the PoyangLake Basin and underlying causes. Acta Geographica Sinica, 2010, 65(7): 828-840. [孙鹏, 张强, 陈晓宏等. 鄱阳湖流域水沙时空演变特征及其机理. 地理学报, 2010, 65(7): 828-840.]



[20] Gao G, Chen D, Xu C Y et al. Trend of estimated actural evapotranspiration over China during 1960-2002. Journal ofGeophysical Research, 2007, 112, D11120, doi: 10.1029/2006JD008010.



[21] Cong Zhentao, Zhao Jingjing, Yang Dawen et al. Understanding the hydrological trends of river basins in China. Journalof Hydrology, 2010, 388: 350-356.



[22] Gifford R M, Farquhar G D, Nicholls N et al. Workshop summary on pan evaporation: An example of the detection andattribution of climate change variables. Australia Academy of Sciences, 2005: 22-23.
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