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Combined effects of precipitation and air temperature on soil moisture in different land covers in a humid basin

机译:降水和气温对湿润盆地不同土地覆盖下土壤水分的综合影响

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Soil moisture is a key variable in hydrological processes. Although the combined effects of multiple climatic factors in different land cover conditions are highly valuable for water resource management, a complete understanding of these effects remains unclear. This study used a cluster analysis approach to investigate the combined effects of precipitation and air temperature, rather than a single factor, in different land covers for an area over the Poyang Lake Basin in China from 2003 to 2009. Specifically, monthly soil moisture was classified into eight clusters according to the change in precipitation and air temperature; the clusters describe a range of climates from the extreme of wet-hot to that of dry-cold. For an individual climate factor, our results showed that the contribution of air temperature to soil moisture is greater than that of precipitation, and the effect of air temperature is more sensitive in different land covers. When considering the combined effects of precipitation and air temperature, soil moisture varies with land cover; however, the variation in a normal climate cluster is greater than in an extreme climate cluster. This indicated that land cover is the dominant factor in soil moisture variation in normal climatic conditions, whereas climate is the dominant factor in extreme conditions. As climate shifts from the wet-hot to the dry-cold cluster, soil moisture decreases for all land covers, with the minimum rate occurring in forest conditions. Meanwhile, soil moisture deficit and saturation are more likely to occur in grassland and forest areas, indicating that forest cover might mitigate drought. The results of this study provide an effective approach to investigate the combined effects of climate factors on soil moisture for various land covers in humid areas. This study also supports the management of water resources in changing climates. (C) 2015 Elsevier B.V. All rights reserved.
机译:土壤水分是水文过程中的关键变量。尽管在不同的土地覆盖条件下多种气候因素的综合影响对于水资源管理非常有价值,但对这些影响的完整理解仍不清楚。这项研究使用聚类分析方法研究了2003年至2009年中国the阳湖盆地上空不同土地覆被下降水和气温的综合影响,而不是单一因素。根据降水量和气温的变化分为八类;这些集群描述了从湿热到干冷的各种气候。对于单个气候因素,我们的结果表明,气温对土壤水分的贡献大于降水的贡献,并且气温在不同土地覆盖下的影响更加敏感。当考虑降水和气温的综合影响时,土壤湿度随土地覆盖而变化。然而,正常气候群的变化要大于极端气候群的变化。这表明,在正常气候条件下,土地覆盖是土壤水分变化的主要因素,而在极端条件下,气候是主要因素。随着气候从湿热向干冷转变,所有土地覆盖的土壤水分都在减少,在森林条件下发生的速率最小。同时,草地和森林地区更容易发生土壤水分亏缺和饱和,表明森林覆盖可能减轻干旱。这项研究的结果为研究气候因素对潮湿地区各种土地覆盖的土壤水分的综合影响提供了有效的方法。这项研究还支持气候变化中的水资源管理。 (C)2015 Elsevier B.V.保留所有权利。

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