Title Wetland emission and atmospheric sink changes explain methane growth in 2020
Authors Peng, Shushi
Lin, Xin
Thompson, Rona L.
Xi, Yi
Liu, Gang
Hauglustaine, Didier
Lan, Xin
Poulter, Benjamin
Ramonet, Michel
Saunois, Marielle
Yin, Yi
Zhang, Zhen
Zheng, Bo
Ciais, Philippe
Affiliation Peking Univ, Coll Urban & Environm Sci, Sino French Inst Earth Syst Sci, Beijing, Peoples R China
Peking Univ, Lab Earth Surface Proc, Beijing, Peoples R China
Peking Univ, Inst Carbon Neutral, Beijing, Peoples R China
Univ Paris Saclay, Lab Sci Climat & Environm, LSCE, IPSL,CEA,CNRS,UVSQ, Gif Sur Yvette, France
Norwegian Inst Air Res NILU, Kjeller, Norway
Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO USA
NOAA, Global Monitoring Lab, Boulder, CO USA
NASA, Goddard Space Flight Ctr, Biospher Sci Lab, Greenbelt, MD USA
CALTECH, Div Geol & Planetary Sci, Pasadena, CA USA
Univ Maryland, Dept Geog Sci, College Pk, MD USA
Tsinghua Univ, Inst Environm & Ecol, Tsinghua Shenzhen Int Grad Sch, Shenzhen, Peoples R China
State Environm Protect Key Lab Sources & Control A, Beijing, Peoples R China
Cyprus Inst, Climate & Atmosphere Res Ctr CARE C, Nicosia, Cyprus
Keywords MODEL DESCRIPTION
CLIMATE-CHANGE
SENSITIVITY
SATELLITE
ORCHIDEE
TRENDS
BUDGET
CH4
CO2
Issue Date 15-Dec-2022
Publisher NATURE
Abstract Atmospheric methane growth reached an exceptionally high rate of 15.1 +/- 0.4 parts per billion per year in 2020 despite a probable decrease in anthropogenic methane emissions during COVID-19 lockdowns(1). Here we quantify changes in methane sources and in its atmospheric sink in 2020 compared with 2019. We find that, globally, total anthropogenic emissions decreased by 1.2 +/- 0.1 teragrams of methane per year (Tg CH(4)yr(-1)), fire emissions decreased by 6.5 +/- 0.1 Tg CH(4)yr(-1) and wetland emissions increased by 6.0 +/- 2.3 Tg CH(4)yr(-1). Tropospheric OH concentration decreased by 1.6 +/- 0.2 per cent relative to 2019, mainly as a result of lower anthropogenic nitrogen oxide (NOx) emissions and associated lower free tropospheric ozone during pandemic lockdowns(2). From atmospheric inversions, we also infer that global net emissions increased by 6.9 +/- 2.1 Tg CH(4)yr(-1) in 2020 relative to 2019, and global methane removal from reaction with OH decreased by 7.5 +/- 0.8 Tg CH(4)yr(-1). Therefore, we attribute the methane growth rate anomaly in 2020 relative to 2019 to lower OH sink (53 +/- 10 per cent) and higher natural emissions (47 +/- 16 per cent), mostly from wetlands. In line with previous findings(3,4), our results imply that wetland methane emissions are sensitive to a warmer and wetter climate and could act as a positive feedback mechanism in the future. Our study also suggests that nitrogen oxide emission trends need to be taken into account when implementing the global anthropogenic methane emissions reduction pledge'.
URI http://hdl.handle.net/20.500.11897/667769
ISSN 0028-0836
DOI 10.1038/s41586-022-05447-w
Indexed SCI(E)
Appears in Collections: 城市与环境学院
地表过程分析与模拟教育部重点实验室

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