甲烷
温室气体
表(数据库)
环境科学
水生生态系统
大气(单位)
气候变化
全球变暖
温室效应
水生植物
化石燃料
甲烷排放
大气科学
生态学
气象学
地理
生物
地质学
水生植物
计算机科学
数据挖掘
作者
Sarian Kosten,Pascal Bodmer
标识
DOI:10.1016/j.aquabot.2024.103775
摘要
Methane (CH4) is a potent greenhouse gas (GHG) - CH4 of non-fossil origin has a global warming potential (GWP) of 27.0 on a 100-year time scale -and strongly contributes to climate change (Table 7.15 in Forster et al. 2021). Approximately half of the CH4 emitted to the atmosphere originates from aquatic systems (Rosentreter et al.2021). While the estimate of aquatic CH4 commissions comes with large uncertainties, this applies even more for the contribution of CH4 emissions from vegetated aquatic areas. This is related to uncertainties in both the emission intensities as well as the areal extent of vegetated aquatic areas (Bodmer et al. 2021).
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