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Impact of recent vegetation greening on temperature and precipitation over China

机译:近期植被绿化对中国温度和降水的影响

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Changes in land-use management and natural climate variability has led to significant vegetation greening in China over the past decades, as evidenced by satellite observations. In this study, we used a high-resolution land-atmosphere coupled regional climate model to assess the impacts of recent greening on China's regional summer climate. Our results inferred a country-averged surface cooling of 0.11 degrees C and a precipitation increase of 0.02 mm/d during summer in response to China's widespread greening. We also identified significant regional variability in the climatic responses to vegetation change. The regions of northern China showed significant cooling, including the Northeast China Plain, Loess Plateau, and the eastern areas of the Northern arid and semiarid region; however, no significant temperature changes were simulated in southern China. Summer precipitation decreased in southern China and increased in the Huang-Huai-Hai Plain and the northern Loess Plateau. Variations in moisture flux convergence had a stronger influence on the precipitation patterns relative to evapotranspiration. Furthermore, our results suggested that vegetation greening would influence the occurrence of extreme climate events by decreasing the number of heatwave days (by 1-3 days, particularly in northern China), reducing the number of continuous drought events in northern China, and minimizing the risks of floods in southern China.
机译:土地利用管理和自然气候变化的变化导致了过去几十年来在中国植被绿化,如卫星观测所证明的。在这项研究中,我们使用了一部高分辨率的土地气氛耦合区域气候模型,以评估近期绿化对中国区域夏季气候影响的影响。我们的结果推断出0.11摄氏度的国家平均冷却,夏季夏季降水增加0.02 mm / d,以应对中国广泛的绿化。我们还确定了对植被变化的气候反应中的重大区域变异。中国北方地区表现出显着的冷却,包括东北平原,黄土高原和北干旱和半干旱地区的东部地区;然而,在中国南方没有模拟显着的温度变化。中国南方夏季降水下降,黄淮海平原和黄土高原北部高原增加。水分通量收敛的变化对析出图案相对于蒸发具有更强的影响。此外,我们的结果表明,植被绿化会通过降低热波天数(1-3天,特别是中国北方)来影响极端气候事件的发生,从而减少了中国北部的持续干旱事件的数量,并最大限度地减少了南方洪水风险。

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