The Arctic Carbon Cycle and Its Response to Changing Climate

Abstract Purpose of Review The Arctic has experienced the most rapid change in climate of anywhere on Earth, and these changes are certain to drive changes in the carbon budget of the Arctic as vegetation changes, soils warm, fires become more frequent, and wetlands evolve as permafrost thaws. In th...

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Published in:Current Climate Change Reports
Main Authors: Bruhwiler, Lori, Parmentier, Frans-Jan W., Crill, Patrick, Leonard, Mark, Palmer, Paul I.
Other Authors: NOAA Research, Natural Environment Research Council, Norwegian Research Council, Swedish Research Council
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2021
Subjects:
Online Access:http://dx.doi.org/10.1007/s40641-020-00169-5
http://link.springer.com/content/pdf/10.1007/s40641-020-00169-5.pdf
http://link.springer.com/article/10.1007/s40641-020-00169-5/fulltext.html
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spelling crspringernat:10.1007/s40641-020-00169-5 2023-05-15T14:33:57+02:00 The Arctic Carbon Cycle and Its Response to Changing Climate Bruhwiler, Lori Parmentier, Frans-Jan W. Crill, Patrick Leonard, Mark Palmer, Paul I. NOAA Research Natural Environment Research Council Norwegian Research Council Swedish Research Council 2021 http://dx.doi.org/10.1007/s40641-020-00169-5 http://link.springer.com/content/pdf/10.1007/s40641-020-00169-5.pdf http://link.springer.com/article/10.1007/s40641-020-00169-5/fulltext.html en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Current Climate Change Reports volume 7, issue 1, page 14-34 ISSN 2198-6061 Atmospheric Science Global and Planetary Change journal-article 2021 crspringernat https://doi.org/10.1007/s40641-020-00169-5 2022-01-04T08:04:22Z Abstract Purpose of Review The Arctic has experienced the most rapid change in climate of anywhere on Earth, and these changes are certain to drive changes in the carbon budget of the Arctic as vegetation changes, soils warm, fires become more frequent, and wetlands evolve as permafrost thaws. In this study, we review the extensive evidence for Arctic climate change and effects on the carbon cycle. In addition, we re-evaluate some of the observational evidence for changing Arctic carbon budgets. Recent Findings Observations suggest a more active CO2 cycle in high northern latitude ecosystems. Evidence points to increased uptake by boreal forests and Arctic ecosystems, as well as increasing respiration, especially in autumn. However, there is currently no strong evidence of increased CH4 emissions. Summary Long-term observations using both bottom-up (e.g., flux) and top-down (atmospheric abundance) approaches are essential for understanding changing carbon cycle budgets. Consideration of atmospheric transport is critical for interpretation of top-down observations of atmospheric carbon. Article in Journal/Newspaper Arctic Climate change permafrost Springer Nature (via Crossref) Arctic Current Climate Change Reports 7 1 14 34
institution Open Polar
collection Springer Nature (via Crossref)
op_collection_id crspringernat
language English
topic Atmospheric Science
Global and Planetary Change
spellingShingle Atmospheric Science
Global and Planetary Change
Bruhwiler, Lori
Parmentier, Frans-Jan W.
Crill, Patrick
Leonard, Mark
Palmer, Paul I.
The Arctic Carbon Cycle and Its Response to Changing Climate
topic_facet Atmospheric Science
Global and Planetary Change
description Abstract Purpose of Review The Arctic has experienced the most rapid change in climate of anywhere on Earth, and these changes are certain to drive changes in the carbon budget of the Arctic as vegetation changes, soils warm, fires become more frequent, and wetlands evolve as permafrost thaws. In this study, we review the extensive evidence for Arctic climate change and effects on the carbon cycle. In addition, we re-evaluate some of the observational evidence for changing Arctic carbon budgets. Recent Findings Observations suggest a more active CO2 cycle in high northern latitude ecosystems. Evidence points to increased uptake by boreal forests and Arctic ecosystems, as well as increasing respiration, especially in autumn. However, there is currently no strong evidence of increased CH4 emissions. Summary Long-term observations using both bottom-up (e.g., flux) and top-down (atmospheric abundance) approaches are essential for understanding changing carbon cycle budgets. Consideration of atmospheric transport is critical for interpretation of top-down observations of atmospheric carbon.
author2 NOAA Research
Natural Environment Research Council
Norwegian Research Council
Swedish Research Council
format Article in Journal/Newspaper
author Bruhwiler, Lori
Parmentier, Frans-Jan W.
Crill, Patrick
Leonard, Mark
Palmer, Paul I.
author_facet Bruhwiler, Lori
Parmentier, Frans-Jan W.
Crill, Patrick
Leonard, Mark
Palmer, Paul I.
author_sort Bruhwiler, Lori
title The Arctic Carbon Cycle and Its Response to Changing Climate
title_short The Arctic Carbon Cycle and Its Response to Changing Climate
title_full The Arctic Carbon Cycle and Its Response to Changing Climate
title_fullStr The Arctic Carbon Cycle and Its Response to Changing Climate
title_full_unstemmed The Arctic Carbon Cycle and Its Response to Changing Climate
title_sort arctic carbon cycle and its response to changing climate
publisher Springer Science and Business Media LLC
publishDate 2021
url http://dx.doi.org/10.1007/s40641-020-00169-5
http://link.springer.com/content/pdf/10.1007/s40641-020-00169-5.pdf
http://link.springer.com/article/10.1007/s40641-020-00169-5/fulltext.html
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
permafrost
genre_facet Arctic
Climate change
permafrost
op_source Current Climate Change Reports
volume 7, issue 1, page 14-34
ISSN 2198-6061
op_rights https://creativecommons.org/licenses/by/4.0
https://creativecommons.org/licenses/by/4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1007/s40641-020-00169-5
container_title Current Climate Change Reports
container_volume 7
container_issue 1
container_start_page 14
op_container_end_page 34
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