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Modelling and attributing evapotranspiration changes on China's Loess Plateau with Budyko framework considering vegetation dynamics and climate seasonality

机译:考虑植被动力学和气候季节性的Budyko框架对中国黄土高原的建模和归因于中国黄土高原的变化

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摘要

The Grain for Green Project in China's Loess Plateau has significantly increased the vegetation coverage (M) since it was implemented in 1999. Accurately modelling evapotranspiration (ET) and attributing its changes are important for assessing the hydrological effects of revegetation in this area. Budyko-based models have been widely used to estimate ET whereby the controlling parameter (omega) captures the effects of land surface conditions and climate seasonality. Although the effects of climate seasonality on ET variation have been theoretically discussed, its important role in omega remains further investigation. An improved climate seasonality and asynchrony index (SAI) was thus used to reflect the seasonality and asynchrony of water and energy distribution in this study. Then omega was extended to M and SAI at grid scale to model annual ET by linking Fu equation in China's Loess Plateau for the period 1981-2012. Further, the whole study period was split into two sub-periods at the year of 1999, and then the complementary method was used to quantify the contributions of precipitation (P), potential evapotranspiration (E-0), M and SAI changes to ET variation between the two sub-periods. The results showed that ET increased by 5.1 mm/yr after 1999. ET is most sensitive to changes in P, followed by M, E-0, and SAI. However, increasing M dominated the overall increase in ET, outweighing the effects of decreasing P and increasing SAI. Because SAI accounted for almost a third of total ET change, the impacts of climate seasonality cannot be ignored in ET simulation and attribution analysis.
机译:中国黄土高原绿化项目的谷物大大增加了植被覆盖率(M),因为它于1999年实施。蒸散(ET)准确地建模并归因于其变化对于评估该地区的再灌注植物的水文影响是重要的。基于Budyko的模型已被广泛用于估算ET,其中控制参数(OMEGA)捕获了土地表面条件和气候季节性的影响。虽然气候季节性对ET变异的影响已经过理论上讨论,但其在欧米茄中的重要作用仍然进一步调查。因此,使用改善的气候季节性和异步指数(SAI),以反映本研究中的水和能源分配的季节性和异步。然后,欧米茄延伸到M和Sai,以富士方程在1981 - 2012年中国黄土高原中的傅方程连接到M和Sai。此外,整个研究时期被分为1999年的两个子周期,然后使用互补方法来量化沉淀(P),潜在的蒸散(E-0),M和SAI变化的贡献两个子周期之间的变化。结果表明,1999年后ET增加了5.1毫米/年.ET对P的变化最敏感,其次是M,E-0和SAI。然而,增加M占据了ET的总体增加,超过了降低P和增加SAI的影响。由于SAI占Total ET的近三分之一,因此在ET模拟和归因分析中不能忽视气候季节性的影响。

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    Chinese Acad Sci Northwest Inst Ecoenvironm & Resources Key Lab Ecohydrol Inland River Basin Lanzhou 730000 Peoples R China;

    Northwest A&F Univ State Key Lab Soil Eros & Dryland Farming Loess P Yangling 712100 Shaanxi Peoples R China;

    Northwest A&F Univ State Key Lab Soil Eros & Dryland Farming Loess P Yangling 712100 Shaanxi Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm & Resources Key Lab Ecohydrol Inland River Basin Lanzhou 730000 Peoples R China;

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  • 正文语种 eng
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  • 关键词

    Evapotranspiration; Budyko method; Climate seasonality; Vegetation;

    机译:蒸散;Budyko方法;气候季节性;植被;

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