Barrow, Alaska Concentrations, Thaw Depth, Temperature, and Water Content 2005 - 2007 Biocomplexity Experiment South/Biocomplexity Experiment Central (BES/BEC) Towers and Soil Probes

The rates, processes, and controls on Arctic cold period soil carbon loss are still poorly understood. To understand one component of winter carbon dioxide (CO2) loss to the atmosphere, continuous measurements of soil CO2 concentration, [CO2], were made and compared to ecosystem scale CO2 fluxes. Me...

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Main Author: Eric Wilkman
Format: Dataset
Language:unknown
Published: Arctic Data Center 2021
Subjects:
Online Access:https://doi.org/10.18739/A20P0WR91
id dataone:doi:10.18739/A20P0WR91
record_format openpolar
spelling dataone:doi:10.18739/A20P0WR91 2024-06-03T18:46:38+00:00 Barrow, Alaska Concentrations, Thaw Depth, Temperature, and Water Content 2005 - 2007 Biocomplexity Experiment South/Biocomplexity Experiment Central (BES/BEC) Towers and Soil Probes Eric Wilkman Barrow, Alaska BEC and BES Tower ENVELOPE(-156.5965,-156.5965,71.2809,71.2809) BEGINDATE: 2005-01-01T00:00:00Z ENDDATE: 2007-01-01T00:00:00Z 2021-01-01T00:00:00Z https://doi.org/10.18739/A20P0WR91 unknown Arctic Data Center Carbon cycle Shoulder season non-growing season diffusive flux Dataset 2021 dataone:urn:node:ARCTIC https://doi.org/10.18739/A20P0WR91 2024-06-03T18:17:19Z The rates, processes, and controls on Arctic cold period soil carbon loss are still poorly understood. To understand one component of winter carbon dioxide (CO2) loss to the atmosphere, continuous measurements of soil CO2 concentration, [CO2], were made and compared to ecosystem scale CO2 fluxes. Measurements of soil [CO2] were made near Utqiaġvik, Alaska from the beginning of soil thaw in summer 2005 until spring 2007. In the summer, soil [CO2] rose with increased soil temperature, reaching values orders of magnitude higher than atmospheric [CO2]. Soil [CO2] initially decreased at the end of summer and beginning of fall but then increased subsequent to soil freezing. Due to complex changes in biological activity, storage, and transport processes, soil [CO2] was then approximately double that observed in the summer. After reaching peak concentrations in November, soil [CO2] steeply decreased over a couple of weeks, suggesting a substantial release of CO2 into the atmosphere and movement within the soil column. Eddy covariance measurements showed variable but continued emissions of CO2 to the atmosphere during freeze-up. The disconnect between soil [CO2] and landscape level fluxes may be attributed to the spatio-temporal heterogeneity in releases of high concentrations of soil [CO2] to the atmosphere during the fall; and when integrated over the area of the eddy covariance tower footprint, do not frequently result in detectable emission events. Continued monitoring of fall and winter soil [CO2] and ecosystem fluxes will be vital to further understanding the variability of inter-annual Arctic CO2 emissions. Dataset Arctic Barrow Alaska Arctic Data Center (via DataONE) Arctic ENVELOPE(-156.5965,-156.5965,71.2809,71.2809)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic Carbon cycle
Shoulder season
non-growing season
diffusive flux
spellingShingle Carbon cycle
Shoulder season
non-growing season
diffusive flux
Eric Wilkman
Barrow, Alaska Concentrations, Thaw Depth, Temperature, and Water Content 2005 - 2007 Biocomplexity Experiment South/Biocomplexity Experiment Central (BES/BEC) Towers and Soil Probes
topic_facet Carbon cycle
Shoulder season
non-growing season
diffusive flux
description The rates, processes, and controls on Arctic cold period soil carbon loss are still poorly understood. To understand one component of winter carbon dioxide (CO2) loss to the atmosphere, continuous measurements of soil CO2 concentration, [CO2], were made and compared to ecosystem scale CO2 fluxes. Measurements of soil [CO2] were made near Utqiaġvik, Alaska from the beginning of soil thaw in summer 2005 until spring 2007. In the summer, soil [CO2] rose with increased soil temperature, reaching values orders of magnitude higher than atmospheric [CO2]. Soil [CO2] initially decreased at the end of summer and beginning of fall but then increased subsequent to soil freezing. Due to complex changes in biological activity, storage, and transport processes, soil [CO2] was then approximately double that observed in the summer. After reaching peak concentrations in November, soil [CO2] steeply decreased over a couple of weeks, suggesting a substantial release of CO2 into the atmosphere and movement within the soil column. Eddy covariance measurements showed variable but continued emissions of CO2 to the atmosphere during freeze-up. The disconnect between soil [CO2] and landscape level fluxes may be attributed to the spatio-temporal heterogeneity in releases of high concentrations of soil [CO2] to the atmosphere during the fall; and when integrated over the area of the eddy covariance tower footprint, do not frequently result in detectable emission events. Continued monitoring of fall and winter soil [CO2] and ecosystem fluxes will be vital to further understanding the variability of inter-annual Arctic CO2 emissions.
format Dataset
author Eric Wilkman
author_facet Eric Wilkman
author_sort Eric Wilkman
title Barrow, Alaska Concentrations, Thaw Depth, Temperature, and Water Content 2005 - 2007 Biocomplexity Experiment South/Biocomplexity Experiment Central (BES/BEC) Towers and Soil Probes
title_short Barrow, Alaska Concentrations, Thaw Depth, Temperature, and Water Content 2005 - 2007 Biocomplexity Experiment South/Biocomplexity Experiment Central (BES/BEC) Towers and Soil Probes
title_full Barrow, Alaska Concentrations, Thaw Depth, Temperature, and Water Content 2005 - 2007 Biocomplexity Experiment South/Biocomplexity Experiment Central (BES/BEC) Towers and Soil Probes
title_fullStr Barrow, Alaska Concentrations, Thaw Depth, Temperature, and Water Content 2005 - 2007 Biocomplexity Experiment South/Biocomplexity Experiment Central (BES/BEC) Towers and Soil Probes
title_full_unstemmed Barrow, Alaska Concentrations, Thaw Depth, Temperature, and Water Content 2005 - 2007 Biocomplexity Experiment South/Biocomplexity Experiment Central (BES/BEC) Towers and Soil Probes
title_sort barrow, alaska concentrations, thaw depth, temperature, and water content 2005 - 2007 biocomplexity experiment south/biocomplexity experiment central (bes/bec) towers and soil probes
publisher Arctic Data Center
publishDate 2021
url https://doi.org/10.18739/A20P0WR91
op_coverage Barrow, Alaska BEC and BES Tower
ENVELOPE(-156.5965,-156.5965,71.2809,71.2809)
BEGINDATE: 2005-01-01T00:00:00Z ENDDATE: 2007-01-01T00:00:00Z
long_lat ENVELOPE(-156.5965,-156.5965,71.2809,71.2809)
geographic Arctic
geographic_facet Arctic
genre Arctic
Barrow
Alaska
genre_facet Arctic
Barrow
Alaska
op_doi https://doi.org/10.18739/A20P0WR91
_version_ 1800869045660024832