Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements

Large changes in the Arctic carbon balance are expected as warming linked to climate change threatens to destabilize ancient permafrost carbon stocks. The eddy covariance (EC) method is an established technique to quantify net losses and gains of carbon between the biosphere and atmosphere at high s...

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Main Authors: Pallandt, Martijn, Kumar, Jitendra, Mauritz, Marguerite, Schuur, Edward, Virkkala, Anna-Maria, Celis, Gerardo, Hoffman, Forrest, Göckede, Mathias
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/bg-2021-133
https://bg.copernicus.org/preprints/bg-2021-133/
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spelling ftcopernicus:oai:publications.copernicus.org:bgd94761 2023-05-15T14:36:51+02:00 Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements Pallandt, Martijn Kumar, Jitendra Mauritz, Marguerite Schuur, Edward Virkkala, Anna-Maria Celis, Gerardo Hoffman, Forrest Göckede, Mathias 2021-07-09 application/pdf https://doi.org/10.5194/bg-2021-133 https://bg.copernicus.org/preprints/bg-2021-133/ eng eng doi:10.5194/bg-2021-133 https://bg.copernicus.org/preprints/bg-2021-133/ eISSN: 1726-4189 Text 2021 ftcopernicus https://doi.org/10.5194/bg-2021-133 2021-07-12T16:22:14Z Large changes in the Arctic carbon balance are expected as warming linked to climate change threatens to destabilize ancient permafrost carbon stocks. The eddy covariance (EC) method is an established technique to quantify net losses and gains of carbon between the biosphere and atmosphere at high spatio-temporal resolution. Over the past decades, a growing network of terrestrial EC tower sites has been established across the Arctic, but a comprehensive assessment of the network’s representativeness within the heterogeneous Arctic region is still lacking. This creates additional uncertainties when integrating flux data across sites, for example when upscaling fluxes to constrain pan-Arctic carbon budgets, and changes therein. This study provides an inventory of Arctic (here >= 60° N) EC sites, which has also been made available online ( https://cosima.nceas.ucsb.edu/carbon-flux-sites/ ). Our database currently comprises 120 EC sites, but only 83 are listed as active, and just 25 of these active sites remain operational throughout the winter. To map the representativeness of this EC network, based on 18 bioclimatic and edaphic variables, we evaluated the similarity between environmental conditions observed at the tower locations and those within the larger Arctic study domain. With the majority of sites located in Fennoscandia and Alaska, these regions were assigned the highest level of network representativeness, while large parts of Siberia and patches of Canada were classified as under-represented. This division between regions is further emphasized for wintertime and methane flux data coverage. Across the Arctic, particularly mountainous regions were poorly represented by the current EC observation network. We tested three different strategies to identify new site locations, or upgrades of existing sites, that optimally enhance the representativeness of the current EC network. While 15 new sites can improve the representativeness of the pan-Arctic network by 20 percent, upgrading as few as 10 existing sites to capture methane fluxes, or remain active during wintertime, can improve their respective network coverage by 28 to 33 percent. This targeted network improvement could be shown to be clearly superior to an unguided selection of new sites, therefore leading to substantial improvements in network coverage based on relatively small investments. Text Arctic Climate change Fennoscandia permafrost Alaska Siberia Copernicus Publications: E-Journals Arctic Canada
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Large changes in the Arctic carbon balance are expected as warming linked to climate change threatens to destabilize ancient permafrost carbon stocks. The eddy covariance (EC) method is an established technique to quantify net losses and gains of carbon between the biosphere and atmosphere at high spatio-temporal resolution. Over the past decades, a growing network of terrestrial EC tower sites has been established across the Arctic, but a comprehensive assessment of the network’s representativeness within the heterogeneous Arctic region is still lacking. This creates additional uncertainties when integrating flux data across sites, for example when upscaling fluxes to constrain pan-Arctic carbon budgets, and changes therein. This study provides an inventory of Arctic (here >= 60° N) EC sites, which has also been made available online ( https://cosima.nceas.ucsb.edu/carbon-flux-sites/ ). Our database currently comprises 120 EC sites, but only 83 are listed as active, and just 25 of these active sites remain operational throughout the winter. To map the representativeness of this EC network, based on 18 bioclimatic and edaphic variables, we evaluated the similarity between environmental conditions observed at the tower locations and those within the larger Arctic study domain. With the majority of sites located in Fennoscandia and Alaska, these regions were assigned the highest level of network representativeness, while large parts of Siberia and patches of Canada were classified as under-represented. This division between regions is further emphasized for wintertime and methane flux data coverage. Across the Arctic, particularly mountainous regions were poorly represented by the current EC observation network. We tested three different strategies to identify new site locations, or upgrades of existing sites, that optimally enhance the representativeness of the current EC network. While 15 new sites can improve the representativeness of the pan-Arctic network by 20 percent, upgrading as few as 10 existing sites to capture methane fluxes, or remain active during wintertime, can improve their respective network coverage by 28 to 33 percent. This targeted network improvement could be shown to be clearly superior to an unguided selection of new sites, therefore leading to substantial improvements in network coverage based on relatively small investments.
format Text
author Pallandt, Martijn
Kumar, Jitendra
Mauritz, Marguerite
Schuur, Edward
Virkkala, Anna-Maria
Celis, Gerardo
Hoffman, Forrest
Göckede, Mathias
spellingShingle Pallandt, Martijn
Kumar, Jitendra
Mauritz, Marguerite
Schuur, Edward
Virkkala, Anna-Maria
Celis, Gerardo
Hoffman, Forrest
Göckede, Mathias
Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements
author_facet Pallandt, Martijn
Kumar, Jitendra
Mauritz, Marguerite
Schuur, Edward
Virkkala, Anna-Maria
Celis, Gerardo
Hoffman, Forrest
Göckede, Mathias
author_sort Pallandt, Martijn
title Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements
title_short Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements
title_full Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements
title_fullStr Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements
title_full_unstemmed Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements
title_sort representativeness assessment of the pan-arctic eddy-covariance site network, and optimized future enhancements
publishDate 2021
url https://doi.org/10.5194/bg-2021-133
https://bg.copernicus.org/preprints/bg-2021-133/
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Climate change
Fennoscandia
permafrost
Alaska
Siberia
genre_facet Arctic
Climate change
Fennoscandia
permafrost
Alaska
Siberia
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-2021-133
https://bg.copernicus.org/preprints/bg-2021-133/
op_doi https://doi.org/10.5194/bg-2021-133
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