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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Simulated effects of soil moisture on oasis self-maintenance in a surrounding desert environment in Northwest China
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Simulated effects of soil moisture on oasis self-maintenance in a surrounding desert environment in Northwest China

机译:西北沙漠环境下土壤水分对绿洲自维持的模拟影响

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摘要

Irrigation is the only method to sustain oasis agriculture in northwest China. In this study, the effects of soil moisture perturbations on the oasis self-maintenance mechanism were investigated using the mesoscale model MM5 with satellite observations of land-surface parameters from MODIS data. Twelve simulations were performed, among which CTL (default simulation) and MOD (with parameters replaced with MODIS data) were used to evaluate the model results. Another 10 simulations with soil moisture perturbations (DRY and WET) assessed the influence of soil moisture on the oasis self-maintenance mechanism. Independent of the initial soil moisture content, all simulations showed dramatic reductions of soil moisture in the initial several days of the simulation, due to the strong evapotranspiration in this arid environment. Both the DRY and WET perturbations led to substantial changes in surface heat flux partitioning and the oasis 'cold-wet' effect, which were also verified by an analysis of the secondary circulation and moisture-inversion level. Drying tends to have more influence than wetting, which indicates that irrigation should be performed more frequently than intensively to protect the oasis self-maintenance mechanism.
机译:灌溉是中国西北地区维持绿洲农业的唯一方法。在这项研究中,使用中尺度模型MM5和MODIS数据对卫星地表参数的卫星观测,研究了土壤水分扰动对绿洲自维持机制的影响。进行了十二次仿真,其中使用CTL(默认仿真)和MOD(参数替换为MODIS数据)来评估模型结果。通过土壤水分扰动(DRY和WET)进行的另外10个模拟评估了土壤水分对绿洲自我维持机制的影响。与最初的土壤水分含量无关,所有模拟结果都显示在模拟的最初几天中,土壤水分显着减少,这是由于在这种干旱环境中强烈的蒸散作用。 DRY和WET扰动都会导致表面热通量分配和绿洲“冷湿”效应发生实质性变化,这也通过对二次循环和水分转化水平的分析得到了证实。干燥往往比润湿具有更大的影响力,这表明灌溉应比集约灌溉更频繁,以保护绿洲的自我维持机制。

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