Institute of Biology, Biodiversity and Ecological Modeling, Freie Universität Berlin, Altensteinstr. 34, D-14195, Berlin, Germany.
Berlin-Brandenburg Institute of Advanced Biodiversity Research (BBIB), D-14195, Berlin, Germany.
Glob Chang Biol. 2017 Jul;23(7):2743-2754. doi: 10.1111/gcb.13598. Epub 2017 Mar 6.
Drylands occur worldwide and are particularly vulnerable to climate change because 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 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, that is, 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.
干旱地区遍布全球,由于干旱地区生态系统直接依赖于土壤水分的供应,而随着气温升高,土壤水分可能会变得越来越有限,因此它们特别容易受到气候变化的影响。气候变化将直接影响土壤水分的可利用性,并改变植物生物量,从而对土壤湿度产生间接反馈。因此,需要更好地了解直接和间接气候变化对土壤湿度的净影响。我们使用生态水文学模拟模型 SOILWAT,在全球温带干旱地区生态系统的各个站点上,对直接气候效应的贡献以及额外的间接的、由气候变化引起的植被变化对土壤水分可利用性的影响进行了分解。我们模拟了 16 个 GCM 在 RCP4.5 和 RCP8.5 下对本世纪末的当前和未来气候条件的预测。我们确定了由于气候变化本身以及由于气候和植被生长形式和生物量的变化而导致的水可用性的变化。植被变化将主要加剧已经预计将受到气候变化直接影响(两个 RCP 情景给出了类似的定性影响)的地区的低土壤水分可用性。相比之下,在那些由于气候变化本身可能会增加水分可用性的地区,由于截留水分损失增加,植被变化将抵消这些增加。只有在极少数情况下,气候变化引起的植被变化可能会导致水分可用性的净增加。这些结果表明,为了应对气候变化而改变植被可能会加剧干旱条件,并可能减弱由于增加降水而带来的影响,也就是说,尽管某些地区降水增加,但会导致更多的生态干旱。我们的研究结果强调了在评估水资源有限的生态系统未来土壤水分状况时,考虑气候变化对植被的间接影响的重要性。