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Drought and ecosystem carbon cycling

机译:干旱与生态系统碳循环

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摘要

Drought as an intermittent disturbance of the water cycle interacts with the carbon cycle differently than the 'gradual' climate change. During drought plants respond physiologically and structurally to prevent excessive water loss according to species-specific water use strategies. This has consequences for carbon uptake by photosynthesis and release by total ecosystem respiration. After a drought the disturbances in the reservoirs of moisture, organic matter and nutrients in the soil and carbohydrates in plants lead to longer-term effects in plant carbon cycling, and potentially mortality. Direct and carry-over effects, mortality and consequently species competition in response to drought are strongly related to the survival strategies of species. Here we review the state of the art of the understanding of the relation between soil moisture drought and the interactions with the carbon cycle of the terrestrial ecosystems. We argue that plant strategies must be given an adequate role in global vegetation models if the effects of drought on the carbon cycle are to be described in a way that justifies the interacting processes
机译:干旱是水循环的间歇性干扰,与碳循环的相互作用不同于“逐渐”的气候变化。在干旱期间,植物会根据特定物种的用水策略在生理和结构上做出反应,以防止水分过多流失。这对光合作用吸收碳和整个生态系统呼吸释放碳具有影响。干旱后,土壤中水分,有机质和养分以及植物中碳水化合物的储集层紊乱导致植物碳循环的长期影响,并可能导致死亡。直接和残留效应,死亡率以及因此对干旱造成的物种竞争与物种的生存策略密切相关。在这里,我们回顾了对土壤水分干旱与陆地生态系统碳循环相互作用之间关系的理解的最新技术水平。我们认为,如果要以证明相互作用过程合理的方式描述干旱对碳循环的影响,则必须在全球植被模型中赋予植物策略适当的作用。

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