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Spatial distribution and temporal variation of reference evapotranspiration in arid and semi‐arid regions of Iran
Author(s) -
Tabari Hossein,
Aeini Ali,
Talaee P. Hosseinzadeh,
Some'e B. Shifteh
Publication year - 2011
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.8146
Subject(s) - arid , evapotranspiration , trend analysis , environmental science , spatial distribution , aridity index , physical geography , spatial variability , wind speed , seasonality , hydrology (agriculture) , geography , climatology , meteorology , statistics , geology , mathematics , ecology , paleontology , remote sensing , geotechnical engineering , biology
Analysis of spatial and temporal variations of reference evapotranspiration (ET o ) is important in arid and semi‐arid regions where water resources are limited. The main aim of this study was to analyse the spatial distribution and the annual, seasonal and monthly trends of the Penman–Monteith ET o for 21 stations in the arid and semi‐arid regions of Iran. Three statistical tests the Mann‐Kendall, Sen's slope estimator and linear regression were used for the analysis. The analysis revealed that ET o increased from January to July and deceased from July to December at almost all stations. Additionally, higher annual ET o values were found in the southeast of the study region and lower values in the northwest of the region. Although the results showed both positive and negative trends in annual ET o series, ET o generally increased, significantly so in six (∼30%) of the stations. Analysis of the impacts of meteorological variables on the temporal trends of ET o indicated that the increasing trend of ET o was most likely due to a significant increase in minimum air temperature, while decreasing trend of ET o was mainly caused by a significant decrease in wind speed. At the sites where increasing ET o trends were statistically significant, the rate of increase varied from (+)8·36 mm/year at Mashhad station to (+)31·68 mm/year at Iranshahr station. On average, an increasing trend of (+)4·42 mm/year was obtained for the whole study area during the last four decades. Seasonal and monthly ET o have also tended to increase at the majority of the stations. The greatest numbers of significant trends were observed in winter on the seasonal time‐scale and in September on the monthly time‐scale. Copyright © 2011 John Wiley & Sons, Ltd.