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首页> 外文期刊>Wiley Interdisciplinary Reviews: Water >Arctic wetland system dynamics under climate warming
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Arctic wetland system dynamics under climate warming

机译:气候变暖下的北极湿地系统动力学

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摘要

Abstract Warming and hydrological changes have already affected and shifted environments in the Arctic. Arctic wetlands are complex systems of coupled hydrological, ecological, and permafrost‐related processes, vulnerable to such environmental changes. This review uses a systems perspective approach to synthesize and elucidate the various interlinked responses and feedbacks of Arctic wetlands to hydroclimatic changes. Starting from increased air temperatures, subsequent permafrost thaw and concurrent hydrological changes are identified as key factors for both shrinkage and expansion of wetland area. Other diverse factors further interact with warming, hydrological changes, and permafrost thaw in altering the Arctic wetland systems. Surface albedo shifts driven by land cover alterations are powerful in reinforcing Arctic warming, while vegetation‐related factors can balance and decelerate permafrost thaw, causing negative feedback loops. With the vast amounts of carbon stored in Arctic wetlands, their changes in turn affect the global carbon cycle. Overall, the systems perspectives outlined and highlighted in this review can be useful in structuring and elucidating the interactions of wetlands with climate, hydrological, and other environmental changes in the Arctic, including the essential permafrost‐carbon feedback. This article is categorized under: Water and Life > Nature of Freshwater Ecosystems Water and Life > Stresses and Pressures on Ecosystems Science of Water > Water and Environmental Change
机译:抽象的变暖和水文变化已经影响和转移北极环境。北极湿地是耦合的水文,生态和多年冻土相关过程的复杂系统,容易受到这种环境变化的影响。这篇综述采用了系统透视方法来综合和阐明北极湿地的各种相互关联的反应和反馈对氢化气候变化。从升高的空气温度开始,随后的多年冻结融化和同时的水文变化被确定为湿地区域收缩和扩张的关键因素。其他各种因素在改变北极湿地系统时进一步与变暖,水文变化和永久冻结融化相互作用。由土地覆盖改变驱动的表面反照率转移在增强北极变暖方面具有强大的功能,而与植被相关的因素可以平衡和减速永久冻结融化,从而导致负反馈回路。随着大量碳存储在北极湿地中,它们的变化反过来影响了全球碳循环。总体而言,本综述中概述和强调的系统观点可用于构建和阐明湿地与北极气候,水文和其他环境变化的相互作用,包括必需的多年冻土 - 碳反馈。本文分类为:水与生命>淡水生态系统的性质水和生命>对水科学的压力和压力>水与环境变化

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