Effects of fire on CO 2 , CH 4 , and N 2 O exchange in a well‐drained Arctic heath ecosystem

Abstract Wildfire frequency and expanse in the Arctic have increased in recent years and are projected to increase further with changes in climatic conditions due to warmer and drier summers. Yet, there is a lack of knowledge about the impacts such events may have on the net greenhouse gas (GHG) bal...

Full description

Bibliographic Details
Published in:Global Change Biology
Main Authors: Hermesdorf, Lena, Elberling, Bo, D'Imperio, Ludovica, Xu, Wenyi, Lambæk, Anders, Ambus, Per L.
Other Authors: Danmarks Grundforskningsfond
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2022
Subjects:
Online Access:http://dx.doi.org/10.1111/gcb.16222
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16222
https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.16222
id crwiley:10.1111/gcb.16222
record_format openpolar
spelling crwiley:10.1111/gcb.16222 2024-06-23T07:50:01+00:00 Effects of fire on CO 2 , CH 4 , and N 2 O exchange in a well‐drained Arctic heath ecosystem Hermesdorf, Lena Elberling, Bo D'Imperio, Ludovica Xu, Wenyi Lambæk, Anders Ambus, Per L. Danmarks Grundforskningsfond 2022 http://dx.doi.org/10.1111/gcb.16222 https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16222 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.16222 en eng Wiley http://creativecommons.org/licenses/by-nc-nd/4.0/ Global Change Biology volume 28, issue 16, page 4882-4899 ISSN 1354-1013 1365-2486 journal-article 2022 crwiley https://doi.org/10.1111/gcb.16222 2024-06-13T04:25:44Z Abstract Wildfire frequency and expanse in the Arctic have increased in recent years and are projected to increase further with changes in climatic conditions due to warmer and drier summers. Yet, there is a lack of knowledge about the impacts such events may have on the net greenhouse gas (GHG) balances in Arctic ecosystems. We investigated in situ effects of an experimental fire in 2017 on carbon dioxide (CO 2 ), methane (CH 4 ), and nitrous oxide (N 2 O) surface fluxes in the most abundant tundra ecosystem in West Greenland in ambient and warmer conditions. Measurements from the growing seasons 2017 to 2019 showed that burnt areas became significant net CO 2 sources for the entire study period, driven by increased ecosystem respiration (ER) immediately after the fire and decreased gross ecosystem production (GEP). Warming by open‐top chambers significantly increased both ER and GEP in control, but not in burnt plots. In contrast to CO 2 , measurements suggest that the overall sink capacity of atmospheric CH 4 , as well as net N 2 O emissions, were not affected by fire in the short term, but only immediately after the fire. The minor effects on CH 4 and N 2 O, which was surprising given the significantly higher nitrate availability observed in burnt plots. However, the minor effects are aligned with the lack of significant effects of fire on soil moisture and soil temperature. Net uptake and emissions of all three GHG from burnt soils were less temperature‐sensitive than in the undisturbed control plots. Overall, this study highlights that wildfires in a typical tundra ecosystem in Greenland may not lead to markedly increased net GHG emissions other than CO 2 . Additional investigations are needed to assess the consequences of more severe fires. Article in Journal/Newspaper Arctic Greenland Tundra Wiley Online Library Arctic Greenland Global Change Biology 28 16 4882 4899
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Wildfire frequency and expanse in the Arctic have increased in recent years and are projected to increase further with changes in climatic conditions due to warmer and drier summers. Yet, there is a lack of knowledge about the impacts such events may have on the net greenhouse gas (GHG) balances in Arctic ecosystems. We investigated in situ effects of an experimental fire in 2017 on carbon dioxide (CO 2 ), methane (CH 4 ), and nitrous oxide (N 2 O) surface fluxes in the most abundant tundra ecosystem in West Greenland in ambient and warmer conditions. Measurements from the growing seasons 2017 to 2019 showed that burnt areas became significant net CO 2 sources for the entire study period, driven by increased ecosystem respiration (ER) immediately after the fire and decreased gross ecosystem production (GEP). Warming by open‐top chambers significantly increased both ER and GEP in control, but not in burnt plots. In contrast to CO 2 , measurements suggest that the overall sink capacity of atmospheric CH 4 , as well as net N 2 O emissions, were not affected by fire in the short term, but only immediately after the fire. The minor effects on CH 4 and N 2 O, which was surprising given the significantly higher nitrate availability observed in burnt plots. However, the minor effects are aligned with the lack of significant effects of fire on soil moisture and soil temperature. Net uptake and emissions of all three GHG from burnt soils were less temperature‐sensitive than in the undisturbed control plots. Overall, this study highlights that wildfires in a typical tundra ecosystem in Greenland may not lead to markedly increased net GHG emissions other than CO 2 . Additional investigations are needed to assess the consequences of more severe fires.
author2 Danmarks Grundforskningsfond
format Article in Journal/Newspaper
author Hermesdorf, Lena
Elberling, Bo
D'Imperio, Ludovica
Xu, Wenyi
Lambæk, Anders
Ambus, Per L.
spellingShingle Hermesdorf, Lena
Elberling, Bo
D'Imperio, Ludovica
Xu, Wenyi
Lambæk, Anders
Ambus, Per L.
Effects of fire on CO 2 , CH 4 , and N 2 O exchange in a well‐drained Arctic heath ecosystem
author_facet Hermesdorf, Lena
Elberling, Bo
D'Imperio, Ludovica
Xu, Wenyi
Lambæk, Anders
Ambus, Per L.
author_sort Hermesdorf, Lena
title Effects of fire on CO 2 , CH 4 , and N 2 O exchange in a well‐drained Arctic heath ecosystem
title_short Effects of fire on CO 2 , CH 4 , and N 2 O exchange in a well‐drained Arctic heath ecosystem
title_full Effects of fire on CO 2 , CH 4 , and N 2 O exchange in a well‐drained Arctic heath ecosystem
title_fullStr Effects of fire on CO 2 , CH 4 , and N 2 O exchange in a well‐drained Arctic heath ecosystem
title_full_unstemmed Effects of fire on CO 2 , CH 4 , and N 2 O exchange in a well‐drained Arctic heath ecosystem
title_sort effects of fire on co 2 , ch 4 , and n 2 o exchange in a well‐drained arctic heath ecosystem
publisher Wiley
publishDate 2022
url http://dx.doi.org/10.1111/gcb.16222
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16222
https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.16222
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Greenland
Tundra
genre_facet Arctic
Greenland
Tundra
op_source Global Change Biology
volume 28, issue 16, page 4882-4899
ISSN 1354-1013 1365-2486
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1111/gcb.16222
container_title Global Change Biology
container_volume 28
container_issue 16
container_start_page 4882
op_container_end_page 4899
_version_ 1802640770994274304