Trends in reference evapotranspiration in the humid region of northeast India

被引:228
作者
Jhajharia, Deepak [1 ]
Dinpashoh, Yagob [2 ]
Kahya, Ercan [3 ]
Singh, Vijay P. [4 ,5 ]
Fakheri-Fard, Ahmad [2 ]
机构
[1] N Eastern Reg Inst Sci & Technol, Dept Agr Engn, Itanagar 791109, Arunachal Prade, India
[2] Univ Tabriz, Fac Agr, Dept Water Engn, Tabriz, Iran
[3] Istanbul Tech Univ, Dept Civil Engn, TR-80626 Istanbul, Turkey
[4] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX 77843 USA
[5] Texas A&M Univ, Dept Civil & Environm Engn, College Stn, TX 77843 USA
关键词
reference evapotranspiration; Penman-Monteith method; humid; Northeast India; Mann-Kendall; trend; REFERENCE CROP EVAPOTRANSPIRATION; PAN EVAPORATION TRENDS; POTENTIAL EVAPOTRANSPIRATION; TEMPORAL CHARACTERISTICS; RIVER-BASIN; SENSITIVITY; PRECIPITATION; STREAMFLOW;
D O I
10.1002/hyp.8140
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
In the present study, the trends in the reference evapotranspiration (ETo) estimated through the Penman-Monteith method were investigated over the humid region of northeast (NE) India by using the Mann-Kendall (MK) test after removing the effect of significant lag-1 serial correlation from the time series of ETo by pre-whitening. During the last 22 years, ETo has been found to decrease significantly at annual and seasonal time scales for 6 sites in NE India and NE India as a whole. The seasonal decreases in ETo have, however, been more significant in the pre-monsoon season, indicating the presence of an element of a seasonal cycle. The decreases in ETo are mainly attributed to the net radiation and wind speed, which are also corroborated by the observed trends in these two parameters at almost all the times scales over most of the sites in NE India. The steady decrease in wind speed and decline in net radiation not only balanced the impact of the temperature increases on ETo, but may have actually caused the decreases in ETo over the humid region of northeast India. Copyright (C) 2011 John Wiley & Sons, Ltd.
引用
收藏
页码:421 / 435
页数:15
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