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- W2378192042 abstract "Based on the daily meteorological measurements of 106 meteorological stations in Northeast China from 1951 to 2007,the daily reference evapotranspiration(ET0) and yearly ET0 are estimated using the Penman-Monteith equation.Gridded annual and annual-average ET0 values for the region are produced using the inverse distance weighted interpolation method.The spatiotemporal variability of ET0 is analyzed using the methods of Mexican hat wavelet transform,Mann-Kendall test,the rotated empirical orthogonal function,and the inclination rate.The results show that:(1) a slightly increasing trend(3.89 mm/10a) is detected in the regional-average ET0 time series,and the regional ET0 minimum and maximum are found in 1953 and 1982,respectively;(2) the temporal variability of regional-average ET0 has a quasi-periodicity of 8-16 years experiencing four alternating stages(low-high-low-high),and in which an intensified ET0 oscillation of 8-10 years is observed;(3) the annual-average ET0 ranges from 600 mm to 1160 mm,and appears as obviously spatial difference exhibiting semi-ring-shaped isograms with a gradual ET0 increment from Northeast to Southwest;and(4) the annual-average ET0 shows a increase trend over 72.61% of the region domain based on the analysis of inclination rate,while the opposite result is obtained for the rest of the region;the maximum and minimum values of inclination rate are 30.6 mm/10a at Nenjiang station and-24.4 mm/10a at Yebaishou station,respectively." @default.
- W2378192042 created "2016-06-24" @default.
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- W2378192042 date "2010-01-01" @default.
- W2378192042 modified "2023-09-24" @default.
- W2378192042 title "Spatiotemporal variability of reference evapotranspiration over the Northeast region of China in the last 60 Years" @default.
- W2378192042 hasPublicationYear "2010" @default.
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