Potential future methane emission hot spots in Greenland
Climate models have been making significant progress encompassing an increasing number of complex feedback mechanisms from natural ecosystems. Permafrost thaw and subsequent induced greenhouse gas emissions, however, remain a challenge for climate models at large. Deducing permafrost conditions and...
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Online Access: | https://doi.org/10.1088/1748-9326/aaf34b https://doaj.org/article/4af0454fcbea4eebaa662f3c7b4453aa |
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ftdoajarticles:oai:doaj.org/article:4af0454fcbea4eebaa662f3c7b4453aa 2023-09-05T13:17:18+02:00 Potential future methane emission hot spots in Greenland Marilena Sophie Geng Jens Hesselbjerg Christensen Torben Røjle Christensen 2019-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/aaf34b https://doaj.org/article/4af0454fcbea4eebaa662f3c7b4453aa EN eng IOP Publishing https://doi.org/10.1088/1748-9326/aaf34b https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aaf34b 1748-9326 https://doaj.org/article/4af0454fcbea4eebaa662f3c7b4453aa Environmental Research Letters, Vol 14, Iss 3, p 035001 (2019) Greenland climate climate change permafrost permafrost thaw methane emissions future emission hot spots Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2019 ftdoajarticles https://doi.org/10.1088/1748-9326/aaf34b 2023-08-13T00:37:31Z Climate models have been making significant progress encompassing an increasing number of complex feedback mechanisms from natural ecosystems. Permafrost thaw and subsequent induced greenhouse gas emissions, however, remain a challenge for climate models at large. Deducing permafrost conditions and associated greenhouse gas emissions from parameters that are simulated in climate models would be a helpful step towards estimating emission budgets from permafrost regions. Here we use a regional climate model with a 5 km horizontal resolution to assess future potential methane (CH _4 ) emissions over presently unglaciated areas in Greenland under an RCP8.5 scenario. A simple frost index is applied to estimate permafrost conditions from the model output. CH _4 flux measurements from two stations in Greenland; Nuuk representing sub-Arctic and Zackenberg high-Arctic climate, are used to establish a relationship between emissions and near surface air temperature. Permafrost conditions in Greenland change drastically by the end of the 21st century in an RCP8.5 climate. Continuous permafrost remains stable only in North Greenland, the north-west coast, the northern tip of Disko Island, and Nuussuaq. Southern Greenland conditions only sustain sporadic permafrost conditions and largely at high elevations, whereas former permafrost in other regions thaws. The increasing thawed soil leads to increasing CH _4 emissions. Especially the area surrounding Kangerlussuaq, Scoresby Land, and the southern coast of Greenland exhibit potentially high emissions during the longer growing season. The constructed maps and budgets combining modelled permafrost conditions with observed CH _4 fluxes from CH _4 promoting sites represent a useful tool to identify areas in need of additional monitoring as they highlight potential CH _4 hot spots. Article in Journal/Newspaper Arctic Climate change Greenland Kangerlussuaq North Greenland Nuuk Nuussuaq permafrost Scoresby land Zackenberg Directory of Open Access Journals: DOAJ Articles Arctic Greenland Kangerlussuaq ENVELOPE(-55.633,-55.633,72.633,72.633) Nuuk ENVELOPE(-52.150,-52.150,68.717,68.717) Nuussuaq ENVELOPE(-51.918,-51.918,66.626,66.626) Scoresby ENVELOPE(162.750,162.750,-66.567,-66.567) Scoresby Land ENVELOPE(-24.500,-24.500,71.750,71.750) Environmental Research Letters 14 3 035001 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Greenland climate climate change permafrost permafrost thaw methane emissions future emission hot spots Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
spellingShingle |
Greenland climate climate change permafrost permafrost thaw methane emissions future emission hot spots Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 Marilena Sophie Geng Jens Hesselbjerg Christensen Torben Røjle Christensen Potential future methane emission hot spots in Greenland |
topic_facet |
Greenland climate climate change permafrost permafrost thaw methane emissions future emission hot spots Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
description |
Climate models have been making significant progress encompassing an increasing number of complex feedback mechanisms from natural ecosystems. Permafrost thaw and subsequent induced greenhouse gas emissions, however, remain a challenge for climate models at large. Deducing permafrost conditions and associated greenhouse gas emissions from parameters that are simulated in climate models would be a helpful step towards estimating emission budgets from permafrost regions. Here we use a regional climate model with a 5 km horizontal resolution to assess future potential methane (CH _4 ) emissions over presently unglaciated areas in Greenland under an RCP8.5 scenario. A simple frost index is applied to estimate permafrost conditions from the model output. CH _4 flux measurements from two stations in Greenland; Nuuk representing sub-Arctic and Zackenberg high-Arctic climate, are used to establish a relationship between emissions and near surface air temperature. Permafrost conditions in Greenland change drastically by the end of the 21st century in an RCP8.5 climate. Continuous permafrost remains stable only in North Greenland, the north-west coast, the northern tip of Disko Island, and Nuussuaq. Southern Greenland conditions only sustain sporadic permafrost conditions and largely at high elevations, whereas former permafrost in other regions thaws. The increasing thawed soil leads to increasing CH _4 emissions. Especially the area surrounding Kangerlussuaq, Scoresby Land, and the southern coast of Greenland exhibit potentially high emissions during the longer growing season. The constructed maps and budgets combining modelled permafrost conditions with observed CH _4 fluxes from CH _4 promoting sites represent a useful tool to identify areas in need of additional monitoring as they highlight potential CH _4 hot spots. |
format |
Article in Journal/Newspaper |
author |
Marilena Sophie Geng Jens Hesselbjerg Christensen Torben Røjle Christensen |
author_facet |
Marilena Sophie Geng Jens Hesselbjerg Christensen Torben Røjle Christensen |
author_sort |
Marilena Sophie Geng |
title |
Potential future methane emission hot spots in Greenland |
title_short |
Potential future methane emission hot spots in Greenland |
title_full |
Potential future methane emission hot spots in Greenland |
title_fullStr |
Potential future methane emission hot spots in Greenland |
title_full_unstemmed |
Potential future methane emission hot spots in Greenland |
title_sort |
potential future methane emission hot spots in greenland |
publisher |
IOP Publishing |
publishDate |
2019 |
url |
https://doi.org/10.1088/1748-9326/aaf34b https://doaj.org/article/4af0454fcbea4eebaa662f3c7b4453aa |
long_lat |
ENVELOPE(-55.633,-55.633,72.633,72.633) ENVELOPE(-52.150,-52.150,68.717,68.717) ENVELOPE(-51.918,-51.918,66.626,66.626) ENVELOPE(162.750,162.750,-66.567,-66.567) ENVELOPE(-24.500,-24.500,71.750,71.750) |
geographic |
Arctic Greenland Kangerlussuaq Nuuk Nuussuaq Scoresby Scoresby Land |
geographic_facet |
Arctic Greenland Kangerlussuaq Nuuk Nuussuaq Scoresby Scoresby Land |
genre |
Arctic Climate change Greenland Kangerlussuaq North Greenland Nuuk Nuussuaq permafrost Scoresby land Zackenberg |
genre_facet |
Arctic Climate change Greenland Kangerlussuaq North Greenland Nuuk Nuussuaq permafrost Scoresby land Zackenberg |
op_source |
Environmental Research Letters, Vol 14, Iss 3, p 035001 (2019) |
op_relation |
https://doi.org/10.1088/1748-9326/aaf34b https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aaf34b 1748-9326 https://doaj.org/article/4af0454fcbea4eebaa662f3c7b4453aa |
op_doi |
https://doi.org/10.1088/1748-9326/aaf34b |
container_title |
Environmental Research Letters |
container_volume |
14 |
container_issue |
3 |
container_start_page |
035001 |
_version_ |
1776198519825104896 |