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- W2363438211 abstract "Based on the daily data of 23 meteorological stations from 1959 to 2010,the potential evaporation(ET0) was calculated using the Food and Agriculture Organization(FAO) Penman-Monteith model,and then the humid index in the Wei river basin was reconstructed from the ET0.With the method of spline interpolation,climatic trend rate,normalized ratio and correlation analysis,etc,the temporal and spatial variations of humid index and extreme arid and wet event,as well as its influential factors were discussed.The results indicated that the humid index decreased in the last 52 years,drought phenomenon increased gradually from south to North,with the driest condition in the loess hilly gully region and the wettest condition in Guanzhong Region and Qin Mountain.The inter annual fluctuations of humid index was very significant and change trend of extreme points presented a antiphase relation corresponding to the potential evaporation.Jing River and North Luo River had the similar dry-wet condition to Wei River Basin.Drying rate was larger for the Hua Mountain and Baoji,Guanzhong Region presented a trend of becoming wet.There was a positive correlation with precipitation and relative humidity,and negative correlation with sunshine duration,potential evaporation and wind speed." @default.
- W2363438211 created "2016-06-24" @default.
- W2363438211 creator A5078275961 @default.
- W2363438211 date "2013-01-01" @default.
- W2363438211 modified "2023-09-22" @default.
- W2363438211 title "Effect of climate change on net primary productivity(NPP) of natural vegetation in Wei river basin(I).Temporal and spatial characteristics of dry-wet condition" @default.
- W2363438211 hasPublicationYear "2013" @default.
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