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- W4313489744 abstract "Abstract Elevation plays a crucial role in modulating the spatiotemporal distributions of climatic variables in mountainous regions, which affects water and energy balances, among which reference evapotranspiration (ET 0 ) is a key hydrological indicator. However, the response of ET 0 to climate change with elevation continues to be poorly understood, especially in the Tibetan Plateau (TP) which has elevation variations of more than 4,000 m. The spatiotemporal variations of ET 0 with elevation were investigated using long‐term (1960–2017) meteorological observations from 82 stations on the TP. The results suggest that the average annual ET 0 showed an insignificant increasing trend. A significant negative correlation between ET 0 and elevation was found ( p < .01). The positive trends of ET 0 decreased with elevation, whereas the negative trends of ET 0 increased significantly with elevation ( p < .05). The magnitude of trends of ET 0 becomes smaller at higher‐elevation stations. Sensitivity analysis indicated that ET 0 was most sensitive to shortwave radiation ( R s ). Moreover, the sensitivities of temperature ( T ) and wind speed ( U ) significantly decreased with elevation, whereas those of R s and vapour pressure deficit (VPD) increased slightly with elevation. The contribution and path analyse indicated that increasing VPD was the dominant contributor to the increase in ET 0 . The effect of elevation on ET 0 variation mainly depended on the tradeoff between the contributions of U and VPD. U was the largest contributing factor for the change in ET 0 below 2,500 m, whereas VPD was the primary contributor to the increase in ET 0 above 2,500 m. This study provides insights into the response of ET 0 to climate change with elevation on the TP, which is of great significance to hydrometeorological processes in high‐altitude regions." @default.
- W4313489744 created "2023-01-06" @default.
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- W4313489744 date "2022-12-27" @default.
- W4313489744 modified "2023-10-17" @default.
- W4313489744 title "Elevation‐dependent changes in the trend of reference evapotranspiration in the Tibetan Plateau during 1960–2017" @default.
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- W4313489744 doi "https://doi.org/10.1002/joc.7964" @default.
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