Current and Future Global Lake Methane Emissions: A Process–Based Modeling Analysis

Freshwater ecosystem contributions to the global methane budget remains the most uncertain among natural sources. With warming and accompanying carbon release from thawed permafrost and thermokarst lake expansion, the increase of methane emissions could be large. However, the impact and relative imp...

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Published in:Journal of Geophysical Research: Biogeosciences
Main Authors: Zhuang, Qianlai, Guo, Mingyang, Melack, John M., Lan, Xin, Tan, Zeli, Oh, Youmi, Leung, L. Ruby
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1971991
https://www.osti.gov/biblio/1971991
https://doi.org/10.1029/2022jg007137
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spelling ftosti:oai:osti.gov:1971991 2023-07-30T04:06:17+02:00 Current and Future Global Lake Methane Emissions: A Process–Based Modeling Analysis Zhuang, Qianlai Guo, Mingyang Melack, John M. Lan, Xin Tan, Zeli Oh, Youmi Leung, L. Ruby 2023-05-08 application/pdf http://www.osti.gov/servlets/purl/1971991 https://www.osti.gov/biblio/1971991 https://doi.org/10.1029/2022jg007137 unknown http://www.osti.gov/servlets/purl/1971991 https://www.osti.gov/biblio/1971991 https://doi.org/10.1029/2022jg007137 doi:10.1029/2022jg007137 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1029/2022jg007137 2023-07-11T10:26:52Z Freshwater ecosystem contributions to the global methane budget remains the most uncertain among natural sources. With warming and accompanying carbon release from thawed permafrost and thermokarst lake expansion, the increase of methane emissions could be large. However, the impact and relative importance of various factors related to warming remain uncertain. Based on diverse lake characteristics incorporated in modeling and observational data, we calibrate and verify a lake biogeochemistry model. The model is then applied to estimate global lake methane emissions and examine the impacts of temperature increase, permafrost thaw, and thermokarst lake area changes for the first and the last decades of the 21st century under different climate scenarios. We find that current emissions are 24.0 ± 8.4 Tg CH 4 yr -1 from lakes larger than 0.1 km 2 , accounting for 11% of the global total natural source as estimated based on atmospheric inversion. Future projections under the RCP8.5 scenario suggest a 57-86% growth in emissions from lakes. While more active methanogenesis and additional carbon substrates from thawing permafrost will enhance methane production under warming, methane oxidation in lake water can be an effective sink to reduce the release from lakes. Other/Unknown Material permafrost Thermokarst SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Journal of Geophysical Research: Biogeosciences 128 3
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Zhuang, Qianlai
Guo, Mingyang
Melack, John M.
Lan, Xin
Tan, Zeli
Oh, Youmi
Leung, L. Ruby
Current and Future Global Lake Methane Emissions: A Process–Based Modeling Analysis
topic_facet 54 ENVIRONMENTAL SCIENCES
description Freshwater ecosystem contributions to the global methane budget remains the most uncertain among natural sources. With warming and accompanying carbon release from thawed permafrost and thermokarst lake expansion, the increase of methane emissions could be large. However, the impact and relative importance of various factors related to warming remain uncertain. Based on diverse lake characteristics incorporated in modeling and observational data, we calibrate and verify a lake biogeochemistry model. The model is then applied to estimate global lake methane emissions and examine the impacts of temperature increase, permafrost thaw, and thermokarst lake area changes for the first and the last decades of the 21st century under different climate scenarios. We find that current emissions are 24.0 ± 8.4 Tg CH 4 yr -1 from lakes larger than 0.1 km 2 , accounting for 11% of the global total natural source as estimated based on atmospheric inversion. Future projections under the RCP8.5 scenario suggest a 57-86% growth in emissions from lakes. While more active methanogenesis and additional carbon substrates from thawing permafrost will enhance methane production under warming, methane oxidation in lake water can be an effective sink to reduce the release from lakes.
author Zhuang, Qianlai
Guo, Mingyang
Melack, John M.
Lan, Xin
Tan, Zeli
Oh, Youmi
Leung, L. Ruby
author_facet Zhuang, Qianlai
Guo, Mingyang
Melack, John M.
Lan, Xin
Tan, Zeli
Oh, Youmi
Leung, L. Ruby
author_sort Zhuang, Qianlai
title Current and Future Global Lake Methane Emissions: A Process–Based Modeling Analysis
title_short Current and Future Global Lake Methane Emissions: A Process–Based Modeling Analysis
title_full Current and Future Global Lake Methane Emissions: A Process–Based Modeling Analysis
title_fullStr Current and Future Global Lake Methane Emissions: A Process–Based Modeling Analysis
title_full_unstemmed Current and Future Global Lake Methane Emissions: A Process–Based Modeling Analysis
title_sort current and future global lake methane emissions: a process–based modeling analysis
publishDate 2023
url http://www.osti.gov/servlets/purl/1971991
https://www.osti.gov/biblio/1971991
https://doi.org/10.1029/2022jg007137
genre permafrost
Thermokarst
genre_facet permafrost
Thermokarst
op_relation http://www.osti.gov/servlets/purl/1971991
https://www.osti.gov/biblio/1971991
https://doi.org/10.1029/2022jg007137
doi:10.1029/2022jg007137
op_doi https://doi.org/10.1029/2022jg007137
container_title Journal of Geophysical Research: Biogeosciences
container_volume 128
container_issue 3
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