A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen)
Most permafrost is located in the Arctic, where frozen organic carbon makes it an important component of the global climate system. Despite the fact that the Arctic climate changes more rapidly than the rest of the globe, observational data density in the region is low. Permafrost thaw and carbon re...
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ftoslouniv:oai:www.duo.uio.no:10852/71510 2023-05-15T14:28:02+02:00 A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen) Boike, Julia Juszak, Inge Lange, Stephan Chadburn, Sarah Burke, Eleanor Paul Overduin, Pier Roth, Kurt Ippisch, Olaf Bornemann, Niko Stern, Lielle Gouttevin, Isabelle Hauber, Ernst Westermann, Sebastian 2018-07-24T12:38:02Z http://hdl.handle.net/10852/71510 http://urn.nb.no/URN:NBN:no-74660 https://doi.org/10.5194/essd-10-355-2018 EN eng http://urn.nb.no/URN:NBN:no-74660 Boike, Julia Juszak, Inge Lange, Stephan Chadburn, Sarah Burke, Eleanor Paul Overduin, Pier Roth, Kurt Ippisch, Olaf Bornemann, Niko Stern, Lielle Gouttevin, Isabelle Hauber, Ernst Westermann, Sebastian . A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen). Earth System Science Data. 2018, 10(1), 355-390 http://hdl.handle.net/10852/71510 1598478 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Earth System Science Data&rft.volume=10&rft.spage=355&rft.date=2018 Earth System Science Data 10 1 355 390 https://doi.org/10.5194/essd-10-355-2018 URN:NBN:no-74660 Fulltext https://www.duo.uio.no/bitstream/handle/10852/71510/2/essd-10-355-2018.pdf Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ CC-BY 1866-3508 Journal article Tidsskriftartikkel Peer reviewed PublishedVersion 2018 ftoslouniv https://doi.org/10.5194/essd-10-355-2018 2020-06-21T08:52:52Z Most permafrost is located in the Arctic, where frozen organic carbon makes it an important component of the global climate system. Despite the fact that the Arctic climate changes more rapidly than the rest of the globe, observational data density in the region is low. Permafrost thaw and carbon release to the atmosphere are a positive feedback mechanism that can exacerbate global warming. This positive feedback functions via changing land–atmosphere energy and mass exchanges. There is thus a great need to understand links between the energy balance, which can vary rapidly over hourly to annual timescales, and permafrost, which changes slowly over long time periods. This understanding thus mandates long-term observational data sets. Such a data set is available from the Bayelva site at Ny-Ålesund, Svalbard, where meteorology, energy balance components and subsurface observations have been made for the last 20 years. Additional data include a high-resolution digital elevation model (DEM) that can be used together with the snow physical information for snowpack modeling and a panchromatic image. This paper presents the data set produced so far, explains instrumentation, calibration, processing and data quality control, as well as the sources for various resulting data sets. The resulting data set is unique in the Arctic and serves as a baseline for future studies. The mean permafrost temperature is −2.8 °C, with a zero-amplitude depth at 5.5 m (2009–2017). Since the data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as snow depth and soil moisture content, they are suitable for use in integrating, calibrating and testing permafrost as a component in earth system models. Article in Journal/Newspaper Arctic Arctic Global warming Ny Ålesund Ny-Ålesund permafrost Svalbard Spitsbergen Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Arctic Bayelva ENVELOPE(11.898,11.898,78.933,78.933) Ny-Ålesund Svalbard Earth System Science Data 10 1 355 390 |
institution |
Open Polar |
collection |
Universitet i Oslo: Digitale utgivelser ved UiO (DUO) |
op_collection_id |
ftoslouniv |
language |
English |
description |
Most permafrost is located in the Arctic, where frozen organic carbon makes it an important component of the global climate system. Despite the fact that the Arctic climate changes more rapidly than the rest of the globe, observational data density in the region is low. Permafrost thaw and carbon release to the atmosphere are a positive feedback mechanism that can exacerbate global warming. This positive feedback functions via changing land–atmosphere energy and mass exchanges. There is thus a great need to understand links between the energy balance, which can vary rapidly over hourly to annual timescales, and permafrost, which changes slowly over long time periods. This understanding thus mandates long-term observational data sets. Such a data set is available from the Bayelva site at Ny-Ålesund, Svalbard, where meteorology, energy balance components and subsurface observations have been made for the last 20 years. Additional data include a high-resolution digital elevation model (DEM) that can be used together with the snow physical information for snowpack modeling and a panchromatic image. This paper presents the data set produced so far, explains instrumentation, calibration, processing and data quality control, as well as the sources for various resulting data sets. The resulting data set is unique in the Arctic and serves as a baseline for future studies. The mean permafrost temperature is −2.8 °C, with a zero-amplitude depth at 5.5 m (2009–2017). Since the data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as snow depth and soil moisture content, they are suitable for use in integrating, calibrating and testing permafrost as a component in earth system models. |
format |
Article in Journal/Newspaper |
author |
Boike, Julia Juszak, Inge Lange, Stephan Chadburn, Sarah Burke, Eleanor Paul Overduin, Pier Roth, Kurt Ippisch, Olaf Bornemann, Niko Stern, Lielle Gouttevin, Isabelle Hauber, Ernst Westermann, Sebastian |
spellingShingle |
Boike, Julia Juszak, Inge Lange, Stephan Chadburn, Sarah Burke, Eleanor Paul Overduin, Pier Roth, Kurt Ippisch, Olaf Bornemann, Niko Stern, Lielle Gouttevin, Isabelle Hauber, Ernst Westermann, Sebastian A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen) |
author_facet |
Boike, Julia Juszak, Inge Lange, Stephan Chadburn, Sarah Burke, Eleanor Paul Overduin, Pier Roth, Kurt Ippisch, Olaf Bornemann, Niko Stern, Lielle Gouttevin, Isabelle Hauber, Ernst Westermann, Sebastian |
author_sort |
Boike, Julia |
title |
A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen) |
title_short |
A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen) |
title_full |
A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen) |
title_fullStr |
A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen) |
title_full_unstemmed |
A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen) |
title_sort |
20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high arctic permafrost research site (bayelva, spitsbergen) |
publishDate |
2018 |
url |
http://hdl.handle.net/10852/71510 http://urn.nb.no/URN:NBN:no-74660 https://doi.org/10.5194/essd-10-355-2018 |
long_lat |
ENVELOPE(11.898,11.898,78.933,78.933) |
geographic |
Arctic Bayelva Ny-Ålesund Svalbard |
geographic_facet |
Arctic Bayelva Ny-Ålesund Svalbard |
genre |
Arctic Arctic Global warming Ny Ålesund Ny-Ålesund permafrost Svalbard Spitsbergen |
genre_facet |
Arctic Arctic Global warming Ny Ålesund Ny-Ålesund permafrost Svalbard Spitsbergen |
op_source |
1866-3508 |
op_relation |
http://urn.nb.no/URN:NBN:no-74660 Boike, Julia Juszak, Inge Lange, Stephan Chadburn, Sarah Burke, Eleanor Paul Overduin, Pier Roth, Kurt Ippisch, Olaf Bornemann, Niko Stern, Lielle Gouttevin, Isabelle Hauber, Ernst Westermann, Sebastian . A 20-year record (1998–2017) of permafrost, active layer and meteorological conditions at a high Arctic permafrost research site (Bayelva, Spitsbergen). Earth System Science Data. 2018, 10(1), 355-390 http://hdl.handle.net/10852/71510 1598478 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Earth System Science Data&rft.volume=10&rft.spage=355&rft.date=2018 Earth System Science Data 10 1 355 390 https://doi.org/10.5194/essd-10-355-2018 URN:NBN:no-74660 Fulltext https://www.duo.uio.no/bitstream/handle/10852/71510/2/essd-10-355-2018.pdf |
op_rights |
Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/essd-10-355-2018 |
container_title |
Earth System Science Data |
container_volume |
10 |
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1 |
container_start_page |
355 |
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390 |
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1766302156954009600 |