Model Study of the Effects of Climate Change on the Methane Emissions on the Arctic Shelves
Based on a regional ice-ocean model, we simulated the state of the water masses of the Arctic Ocean to analyze the transport of dissolved methane on the Arctic shelves. From 1970 to 2019, we obtained estimates of methane emissions at the Arctic seas due to the degradation of submarine permafrost and...
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2022
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Online Access: | https://doi.org/10.3390/atmos13020274 https://doaj.org/article/f2ca021ee1804d54ab813d03ff01001d |
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ftdoajarticles:oai:doaj.org/article:f2ca021ee1804d54ab813d03ff01001d 2023-05-15T14:34:29+02:00 Model Study of the Effects of Climate Change on the Methane Emissions on the Arctic Shelves Valentina Malakhova Elena Golubeva 2022-02-01T00:00:00Z https://doi.org/10.3390/atmos13020274 https://doaj.org/article/f2ca021ee1804d54ab813d03ff01001d EN eng MDPI AG https://www.mdpi.com/2073-4433/13/2/274 https://doaj.org/toc/2073-4433 doi:10.3390/atmos13020274 2073-4433 https://doaj.org/article/f2ca021ee1804d54ab813d03ff01001d Atmosphere, Vol 13, Iss 274, p 274 (2022) Arctic seas Arctic shelves methane emissions methane concentration ice climate change Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.3390/atmos13020274 2022-12-31T14:44:46Z Based on a regional ice-ocean model, we simulated the state of the water masses of the Arctic Ocean to analyze the transport of dissolved methane on the Arctic shelves. From 1970 to 2019, we obtained estimates of methane emissions at the Arctic seas due to the degradation of submarine permafrost and gas release at the ocean–bottom interface. The calculated annual methane flux from the Arctic shelf seas into the atmosphere did not exceed 2 Tg CH 4 year −1 . We have shown that the East Siberian shelf seas make the main contribution to the total methane emissions of the region. The spatial variability of the methane fluxes into the atmosphere is primarily due to the peculiarities of the water circulation and ice conditions. Only 7% of the dissolved methane originating from sediment enters the atmosphere within the study area. Most of it appears to be transported below the surface and oxidized by microbial activity. We found that increasing periods and areas of ice-free water and decreasing ice concentration have contributed to a steady increase in methane emissions since the middle of the first decade of the current century. Article in Journal/Newspaper Arctic Arctic Ocean Climate change Ice permafrost Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean East Siberian Shelf ENVELOPE(-162.267,-162.267,74.400,74.400) Atmosphere 13 2 274 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic seas Arctic shelves methane emissions methane concentration ice climate change Meteorology. Climatology QC851-999 |
spellingShingle |
Arctic seas Arctic shelves methane emissions methane concentration ice climate change Meteorology. Climatology QC851-999 Valentina Malakhova Elena Golubeva Model Study of the Effects of Climate Change on the Methane Emissions on the Arctic Shelves |
topic_facet |
Arctic seas Arctic shelves methane emissions methane concentration ice climate change Meteorology. Climatology QC851-999 |
description |
Based on a regional ice-ocean model, we simulated the state of the water masses of the Arctic Ocean to analyze the transport of dissolved methane on the Arctic shelves. From 1970 to 2019, we obtained estimates of methane emissions at the Arctic seas due to the degradation of submarine permafrost and gas release at the ocean–bottom interface. The calculated annual methane flux from the Arctic shelf seas into the atmosphere did not exceed 2 Tg CH 4 year −1 . We have shown that the East Siberian shelf seas make the main contribution to the total methane emissions of the region. The spatial variability of the methane fluxes into the atmosphere is primarily due to the peculiarities of the water circulation and ice conditions. Only 7% of the dissolved methane originating from sediment enters the atmosphere within the study area. Most of it appears to be transported below the surface and oxidized by microbial activity. We found that increasing periods and areas of ice-free water and decreasing ice concentration have contributed to a steady increase in methane emissions since the middle of the first decade of the current century. |
format |
Article in Journal/Newspaper |
author |
Valentina Malakhova Elena Golubeva |
author_facet |
Valentina Malakhova Elena Golubeva |
author_sort |
Valentina Malakhova |
title |
Model Study of the Effects of Climate Change on the Methane Emissions on the Arctic Shelves |
title_short |
Model Study of the Effects of Climate Change on the Methane Emissions on the Arctic Shelves |
title_full |
Model Study of the Effects of Climate Change on the Methane Emissions on the Arctic Shelves |
title_fullStr |
Model Study of the Effects of Climate Change on the Methane Emissions on the Arctic Shelves |
title_full_unstemmed |
Model Study of the Effects of Climate Change on the Methane Emissions on the Arctic Shelves |
title_sort |
model study of the effects of climate change on the methane emissions on the arctic shelves |
publisher |
MDPI AG |
publishDate |
2022 |
url |
https://doi.org/10.3390/atmos13020274 https://doaj.org/article/f2ca021ee1804d54ab813d03ff01001d |
long_lat |
ENVELOPE(-162.267,-162.267,74.400,74.400) |
geographic |
Arctic Arctic Ocean East Siberian Shelf |
geographic_facet |
Arctic Arctic Ocean East Siberian Shelf |
genre |
Arctic Arctic Ocean Climate change Ice permafrost |
genre_facet |
Arctic Arctic Ocean Climate change Ice permafrost |
op_source |
Atmosphere, Vol 13, Iss 274, p 274 (2022) |
op_relation |
https://www.mdpi.com/2073-4433/13/2/274 https://doaj.org/toc/2073-4433 doi:10.3390/atmos13020274 2073-4433 https://doaj.org/article/f2ca021ee1804d54ab813d03ff01001d |
op_doi |
https://doi.org/10.3390/atmos13020274 |
container_title |
Atmosphere |
container_volume |
13 |
container_issue |
2 |
container_start_page |
274 |
_version_ |
1766307508424540160 |