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Climate change-induced vegetation shifts lead to more ecological droughts despite projected rainfall increases in many global temperate drylands

机译:气候变化引起的植被变化

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摘要

Drylands occur world-wide and are particularly vulnerable to climate change since dryland ecosystems depend directly on soil water availability that may become increasingly limited as temperatures rise. Climate change will both directly impact soil water availability, and also change plant biomass, with resulting indirect feedbacks on soil moisture. Thus, the net impact of direct and indirect climate change effects on soil moisture requires better understanding. We used the ecohydrological simulation model SOILWAT at sites from temperate dryland ecosystems around the globe to disentangle the contributions of direct climate change effects and of additional indirect, climate change-induced changes in vegetation on soil water availability. We simulated current and future climate conditions projected by 16 GCMs under RCP 4.5 and RCP 8.5 for the end of the century. We determined shifts in water availability due to climate change alone and due to combined changes of climate and the growth form and biomass of vegetation. Vegetation change will mostly exacerbate low soil water availability in regions already expected to suffer from negative direct impacts of climate change (with the two RCP scenarios giving us qualitatively similar effects). By contrast, in regions that will likely experience increased water availability due to climate change alone, vegetation changes will counteract these increases due to increased water losses by interception. In only a small minority of locations, climate change induced vegetation changes may lead to a net increase in water availability. These results suggest that changes in vegetation in response to climate change may exacerbate drought conditions and may dampen the effects of increased precipitation, i.e. leading to more ecological droughts despite higher precipitation in some regions. Our results underscore the value of considering indirect effects of climate change on vegetation when assessing future soil moisture conditions in water-limited ecosystems. This article is protected by copyright. All rights reserved.
机译:干旱地区遍布世界各地,特别容易受到气候变化的影响,因为干旱地区的生态系统直接依赖于土壤水的可利用性,随着温度的升高,土壤的可利用性将越来越有限。气候变化不仅会直接影响土壤水分的供应,还会改变植物的生物量,从而间接反馈土壤水分。因此,直接和间接的气候变化影响对土壤水分的净影响需要更好地理解。我们在来自全球温带旱地生态系统的地点使用了生态水文模拟模型SOILWAT,以弄清直接的气候变化影响以及其他间接的,由气候变化引起的植被变化对土壤水分利用的贡献。我们模拟了本世纪末16个GCM在RCP 4.5和RCP 8.5下预测的当前和未来气候条件。我们确定了仅由于气候变化以及由于气候变化以及植被的生长形式和生物量的综合变化而导致的水利用量变化。在预期已经遭受气候变化负面直接影响的地区,植被变化将在大多数情况下加剧土壤低水供应(两种RCP情景在质量上都具有相似的影响)。相比之下,在仅因气候变化而可能会增加水利用量的地区,由于拦截造成的水损失增加,植被变化将抵消这些增加。在极少数地区,气候变化引起的植被变化可能导致水资源净增加。这些结果表明,响应气候变化的植被变化可能加剧干旱条件,并可能抑制降水增加的影响,即尽管某些地区降水增加,但仍导致更多的生态干旱。我们的结果强调了在评估缺水生态系统中未来土壤水分状况时考虑气候变化对植被的间接影响的价值。本文受版权保护。版权所有。

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