Simultaneous Hot and Dry Extreme-Events Increase Wetland Methane Emissions: An Assessment of Compound Extreme-Event Impacts Using Ameriflux and FLUXNET-CH4 Site Data Sets

IF 5.4 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES Global Biogeochemical Cycles Pub Date : 2024-09-14 DOI:10.1029/2024GB008201
T. J. R. Lippmann, Y. van der Velde, K. Naudts, G. Hensgens, J. E. Vonk, H. Dolman
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Abstract

Wetlands are the largest natural source of global atmospheric methane (CH4). Despite advances to our understanding of changes in temperature and precipitation extremes, their impacts on carbon-rich ecosystems such as wetlands, remain significantly understudied. Here, we quantify the impacts of extreme temperature, precipitation, and dry events on wetland CH4 dynamics by investigating the effects of both compound and discrete extreme-events. We use long-term climate data to identify extreme-events and 45 eddy covariance sites data sets sourced from the FLUXNET-CH4 database and Ameriflux project to assess impacts on wetland CH4 emissions. These findings reveal that compound hot + dry extreme-events lead to large increases in daily CH4 emissions. However, per event, discrete dry-only extreme-events cause the largest total decrease in CH4 emissions, due to their long duration. Despite dry-only extreme-events leading to an overall reduction in CH4 emissions, enhanced fluxes are often observed for the first days of dry-only extreme-events. These effects differ depending on wetland type, where marsh sites tend to be sensitive to most types of extreme-events. Lagged impacts are significant for at least the 12 months following several types of extreme-events. These findings have implications for understanding how extreme-event impacts may evolve in the context of climate change, where changes in the frequency and intensity of temperature and precipitation extreme-events are already observed. With increasing occurrences of enhanced CH4 fluxes in response to hot-only extreme-events and hot + wet extreme-events and fewer occurrences of reduced CH4 fluxes during cold-only extreme-events, the impact of wetland CH4 emissions on climate warming may be increasing.

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同时发生的干热极端事件增加了湿地甲烷排放量:利用 Ameriflux 和 FLUXNET-CH4 站点数据集评估复合极端事件的影响
湿地是全球大气中甲烷 (CH4) 的最大天然来源。尽管我们对极端气温和降水变化的理解有所进步,但它们对湿地等富碳生态系统的影响研究仍显不足。在这里,我们通过研究复合极端事件和离散极端事件的影响,量化极端温度、降水和干旱事件对湿地 CH4 动态的影响。我们利用长期气候数据来识别极端事件,并利用来自 FLUXNET-CH4 数据库和 Ameriflux 项目的 45 个涡度协方差站点数据集来评估对湿地 CH4 排放的影响。这些研究结果表明,干热复合极端事件会导致每天的甲烷排放量大幅增加。然而,就每个事件而言,由于持续时间较长,离散的纯干燥极端事件导致的甲烷排放总降幅最大。尽管仅干燥的极端事件会导致 CH4 排放量的总体减少,但在仅干燥的极端事件发生的头几天,往往会观察到通量的增加。这些影响因湿地类型而异,沼泽地往往对大多数类型的极端事件敏感。在几种极端事件发生后的至少 12 个月内,滞后影响都很明显。这些发现对于理解极端事件的影响在气候变化背景下如何演变具有重要意义,因为在气候变化背景下,温度和降水极端事件的频率和强度已经发生了变化。随着仅在炎热极端事件和炎热+潮湿极端事件中CH4通量增加的情况越来越多,而在仅在寒冷极端事件中CH4通量减少的情况越来越少,湿地CH4排放对气候变暖的影响可能会越来越大。
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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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