Summer evapotranspiration in western Siberia: A comparison between eddy covariance and Penman method formulations

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題名:	Summer evapotranspiration in western Siberia: A comparison between eddy covariance and Penman method formulations
作者:	柯奧圖;Fleischer, Elisa;Bölter, Jana;Klemm, Otto
貢獻者:	地球科學學院大氣科學學系
關鍵詞:	actual evapotranspiration;approximation formula;Climate;climate change;cold;Covariance;Eddies;eddy covariance;environmental factors;equations;Estimates;Evapotranspiration;forests;Formulations;Marine;Mathematical analysis;meteorological data;Penman method;potential evapotranspiration;Siberia;soil;steppes;surfaces;water stress;western Siberia
日期:	2015-09-30
上傳時間:	2026-04-21 14:07:41 (UTC+8)
出版者:	John Wiley and Sons Ltd;Chichester: Blackwell Publishing Ltd
摘要:	摘要： Evapotranspiration is difficult to quantify because of the many factors and complex processes that influence it. Several empirical methods have been developed over the years to estimate potential evapotranspiration based on easily available parameters. Directly measured data of actual evapotranspiration have been rather sparse in the past and still need to be improved in particular regions like western Siberia. The transition zone between the warm temperate and cold temperate continental climates is very sensitive to climate change, and water stress is an increasingly important issue in these regions with a highly dynamic agricultural activity. So there is a growing need to estimate actual evapotranspiration. Widely usable approximations are needed. In this study, the values of potential evapotranspiration computed with the original version, and eight modifications of the Penman formulation were compared and related to the actual evapotranspiration measured by eddy covariance over a grassland area in western Siberia. The original 1948 and 1963 Penman formulations are best for estimating potential evapotranspiration in the transition zone between the forest steppes and the pre‐taiga. A nearly linear relationship between the potential and actual evapotranspiration was found. A simple modification of the Penman equation (i.e. the multiplication of the result by a factor of 0.47) is suggested for approximating the actual evapotranspiration based on standard meteorological data for the region. The original Penman formulation is most robust and will provide the widest applicability in the future under changing climate and environmental conditions. In this context, it is further recommended not to neglect the ventilation term of the Penman equation, which is often assumed to be negligibly small. A detailed correlation analysis showed that under dry soil conditions, the vegetation largely contributed to the actual evapotranspiration and, in contrast to widely held expectations, that the Penman equation is best adapted to vegetated surfaces. Copyright © 2015 John Wiley & Sons, Ltd. 其他題名： Hydrol. Process 出版者： Chichester: Blackwell Publishing Ltd 出版日期： 2015-09-30 出處： Hydrological processes, 2015-09, Vol.29 (20), p.4498-4513 資源來源： Wiley Online Library All Journals 版權： Copyright © 2015 John Wiley & Sons, Ltd. 識別號： ISSN: 0885-6087 識別號： EISSN: 1099-1085 識別號： DOI: 10.1002/hyp.10517
顯示於類別:	[大氣科學學系] 期刊論文

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