Effects of fire on CO2, CH4, and N2O exchange in a well‐drained Arctic heath ecosystem. (27th May 2022)
- Record Type:
- Journal Article
- Title:
- Effects of fire on CO2, CH4, and N2O exchange in a well‐drained Arctic heath ecosystem. (27th May 2022)
- Main Title:
- Effects of fire on CO2, CH4, and N2O exchange in a well‐drained Arctic heath ecosystem
- Authors:
- Hermesdorf, Lena
Elberling, Bo
D'Imperio, Ludovica
Xu, Wenyi
Lambæk, Anders
Ambus, Per L. - Abstract:
- 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 (CO2 ), methane (CH4 ), and nitrous oxide (N2 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 CO2 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 CO2, measurements suggest that the overall sink capacity of atmospheric CH4, as well as net N2 O emissions, were not affected by fire in the short term, but only immediately after the fire. The minor effects on CH4 and N2 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 theAbstract: 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 (CO2 ), methane (CH4 ), and nitrous oxide (N2 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 CO2 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 CO2, measurements suggest that the overall sink capacity of atmospheric CH4, as well as net N2 O emissions, were not affected by fire in the short term, but only immediately after the fire. The minor effects on CH4 and N2 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 CO2 . Additional investigations are needed to assess the consequences of more severe fires. Abstract : We investigated the effects of an experimental fire on carbon dioxide (CO2 ), methane (CH4 ), and nitrous oxide (N2 O) surface fluxes in an Arctic upland ecosystem with and without summer warming. Overall, this study highlights that wildfires in a typical tundra ecosystem in Greenland may not lead to markedly increased net GHG emissions other than CO2 . … (more)
- Is Part Of:
- Global change biology. Volume 28:Number 16(2022)
- Journal:
- Global change biology
- Issue:
- Volume 28:Number 16(2022)
- Issue Display:
- Volume 28, Issue 16 (2022)
- Year:
- 2022
- Volume:
- 28
- Issue:
- 16
- Issue Sort Value:
- 2022-0028-0016-0000
- Page Start:
- 4882
- Page End:
- 4899
- Publication Date:
- 2022-05-27
- Subjects:
- carbon dioxide -- GHG balance -- Greenland -- methane -- NEE -- nitrous oxide -- tundra
Climatic changes -- Environmental aspects -- Periodicals
Troposphere -- Environmental aspects -- Periodicals
Biodiversity conservation -- Periodicals
Eutrophication -- Periodicals
551.5 - Journal URLs:
- http://www.blackwell-synergy.com/member/institutions/issuelist.asp?journal=gcb ↗
http://onlinelibrary.wiley.com/ ↗ - DOI:
- 10.1111/gcb.16222 ↗
- Languages:
- English
- ISSNs:
- 1354-1013
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 4195.358330
British Library DSC - BLDSS-3PM
British Library HMNTS - ELD Digital store - Ingest File:
- 22593.xml