Warming effects of spring rainfall increase methane emissions from thawing permafrost: Site-level data from bog complex I - Water Table Depth 2014-2016

Methane emissions regulate the near-term global warming potential of permafrost thaw, particularly where loss of ice-rich permafrost converts forest and tundra into wetlands. Northern latitudes are expected to get warmer and wetter, and while there is consensus that warming will increase thaw and me...

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Main Authors: Neumann, Rebecca B, Mooreberg, Colby J, Lundquist, Jessica D, Turner, Jesse C, Waldrop, Mark P., McFarland, Jack W., Euskirchen, Eugenie S., Edgar, Colin, Turetsky, Merritt R, Bonanza Creek LTER
Format: Dataset
Language:English
Published: Environmental Data Initiative 2019
Subjects:
Ice
Online Access:https://dx.doi.org/10.6073/pasta/77faf778a5c159ec19693595102651bf
https://portal.edirepository.org/nis/mapbrowse?packageid=knb-lter-bnz.709.3
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spelling ftdatacite:10.6073/pasta/77faf778a5c159ec19693595102651bf 2023-05-15T16:37:21+02:00 Warming effects of spring rainfall increase methane emissions from thawing permafrost: Site-level data from bog complex I - Water Table Depth 2014-2016 Neumann, Rebecca B Mooreberg, Colby J Lundquist, Jessica D Turner, Jesse C Waldrop, Mark P. McFarland, Jack W. Euskirchen, Eugenie S. Edgar, Colin Turetsky, Merritt R Bonanza Creek LTER 2019 https://dx.doi.org/10.6073/pasta/77faf778a5c159ec19693595102651bf https://portal.edirepository.org/nis/mapbrowse?packageid=knb-lter-bnz.709.3 en eng Environmental Data Initiative https://dx.doi.org/10.2172/1573358 Dataset dataPackage dataset 2019 ftdatacite https://doi.org/10.6073/pasta/77faf778a5c159ec19693595102651bf https://doi.org/10.2172/1573358 2022-02-09T11:57:25Z Methane emissions regulate the near-term global warming potential of permafrost thaw, particularly where loss of ice-rich permafrost converts forest and tundra into wetlands. Northern latitudes are expected to get warmer and wetter, and while there is consensus that warming will increase thaw and methane emissions, effects of increased precipitation are uncertain. At a thawing wetland complex in Interior Alaska, we found that interactions between rain and deep soil temperatures controlled methane emissions. In rainy years, recharge from the watershed rapidly altered wetland soil temperatures, warming the top ~80 cm of soil in spring and summer, and cooling it in autumn. When soils were warmed by spring rainfall, methane emissions increased by ~30%. The warm, deep soils early in the growing season likely supported both microbial and plant processes that enhanced emissions. Our study identifies an important and unconsidered role of rain in governing the radiative forcing of thawing permafrost landscapes. All site-level data from the studied bog, eddy covariance and micrometeorological data referenced in the published manuscript are available in the LTER data repository. These data are related to the following data package: Surface carbon, water and energy fluxes measured by eddy covariance at 3 sites within the Alaska Peatlands Experiment and Bonanza Creek Experimental Forest 2013-2016 (http://dx.doi.org/10.6073/pasta/4fabab3846113a1866b06f1b3d6d52a3). Dataset Ice permafrost Tundra Alaska DataCite Metadata Store (German National Library of Science and Technology) Bonanza ENVELOPE(-119.820,-119.820,55.917,55.917)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Methane emissions regulate the near-term global warming potential of permafrost thaw, particularly where loss of ice-rich permafrost converts forest and tundra into wetlands. Northern latitudes are expected to get warmer and wetter, and while there is consensus that warming will increase thaw and methane emissions, effects of increased precipitation are uncertain. At a thawing wetland complex in Interior Alaska, we found that interactions between rain and deep soil temperatures controlled methane emissions. In rainy years, recharge from the watershed rapidly altered wetland soil temperatures, warming the top ~80 cm of soil in spring and summer, and cooling it in autumn. When soils were warmed by spring rainfall, methane emissions increased by ~30%. The warm, deep soils early in the growing season likely supported both microbial and plant processes that enhanced emissions. Our study identifies an important and unconsidered role of rain in governing the radiative forcing of thawing permafrost landscapes. All site-level data from the studied bog, eddy covariance and micrometeorological data referenced in the published manuscript are available in the LTER data repository. These data are related to the following data package: Surface carbon, water and energy fluxes measured by eddy covariance at 3 sites within the Alaska Peatlands Experiment and Bonanza Creek Experimental Forest 2013-2016 (http://dx.doi.org/10.6073/pasta/4fabab3846113a1866b06f1b3d6d52a3).
format Dataset
author Neumann, Rebecca B
Mooreberg, Colby J
Lundquist, Jessica D
Turner, Jesse C
Waldrop, Mark P.
McFarland, Jack W.
Euskirchen, Eugenie S.
Edgar, Colin
Turetsky, Merritt R
Bonanza Creek LTER
spellingShingle Neumann, Rebecca B
Mooreberg, Colby J
Lundquist, Jessica D
Turner, Jesse C
Waldrop, Mark P.
McFarland, Jack W.
Euskirchen, Eugenie S.
Edgar, Colin
Turetsky, Merritt R
Bonanza Creek LTER
Warming effects of spring rainfall increase methane emissions from thawing permafrost: Site-level data from bog complex I - Water Table Depth 2014-2016
author_facet Neumann, Rebecca B
Mooreberg, Colby J
Lundquist, Jessica D
Turner, Jesse C
Waldrop, Mark P.
McFarland, Jack W.
Euskirchen, Eugenie S.
Edgar, Colin
Turetsky, Merritt R
Bonanza Creek LTER
author_sort Neumann, Rebecca B
title Warming effects of spring rainfall increase methane emissions from thawing permafrost: Site-level data from bog complex I - Water Table Depth 2014-2016
title_short Warming effects of spring rainfall increase methane emissions from thawing permafrost: Site-level data from bog complex I - Water Table Depth 2014-2016
title_full Warming effects of spring rainfall increase methane emissions from thawing permafrost: Site-level data from bog complex I - Water Table Depth 2014-2016
title_fullStr Warming effects of spring rainfall increase methane emissions from thawing permafrost: Site-level data from bog complex I - Water Table Depth 2014-2016
title_full_unstemmed Warming effects of spring rainfall increase methane emissions from thawing permafrost: Site-level data from bog complex I - Water Table Depth 2014-2016
title_sort warming effects of spring rainfall increase methane emissions from thawing permafrost: site-level data from bog complex i - water table depth 2014-2016
publisher Environmental Data Initiative
publishDate 2019
url https://dx.doi.org/10.6073/pasta/77faf778a5c159ec19693595102651bf
https://portal.edirepository.org/nis/mapbrowse?packageid=knb-lter-bnz.709.3
long_lat ENVELOPE(-119.820,-119.820,55.917,55.917)
geographic Bonanza
geographic_facet Bonanza
genre Ice
permafrost
Tundra
Alaska
genre_facet Ice
permafrost
Tundra
Alaska
op_relation https://dx.doi.org/10.2172/1573358
op_doi https://doi.org/10.6073/pasta/77faf778a5c159ec19693595102651bf
https://doi.org/10.2172/1573358
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