Permafrost Warming in a Subarctic Peatland – Which Meteorological Controls are Most Important?
Because climate change can affect the carbon balance and hydrology in permafrost peatlands, a better understanding of their sensitivity to changes in temperature and precipitation is needed. In Tavvavuoma, northernmost Sweden, meteorological parameters and ground thermal properties have been monitor...
Published in: | Permafrost and Periglacial Processes |
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Online Access: | https://doi.org/10.1002/ppp.1862 |
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ftrepec:oai:RePEc:wly:perpro:v:27:y:2016:i:2:p:177-188 2023-05-15T17:54:53+02:00 Permafrost Warming in a Subarctic Peatland – Which Meteorological Controls are Most Important? A. Britta K. Sannel Gustaf Hugelius Peter Jansson Peter Kuhry https://doi.org/10.1002/ppp.1862 unknown https://doi.org/10.1002/ppp.1862 article ftrepec https://doi.org/10.1002/ppp.1862 2020-12-04T13:31:25Z Because climate change can affect the carbon balance and hydrology in permafrost peatlands, a better understanding of their sensitivity to changes in temperature and precipitation is needed. In Tavvavuoma, northernmost Sweden, meteorological parameters and ground thermal properties have been monitored in a peat plateau from 2006 to 2013. During this time period, the air temperature record shows no warming trend, and the late‐season thaw depth has been relatively stable at around 55–60 cm. Meanwhile, the mean annual ground temperature at 1 m depth has increased by 0.06 °C/yr and at 2–5 m depth the permafrost is currently warmer than ‐0.3 °C. Statistical analyses suggest that interannual changes in thaw depth and ground temperatures are affected by different meteorological factors. Summer air temperatures and annual thawing degree‐days control thaw depth (p ≤ 0.05), whereas winter precipitation/snow depth affects ground temperatures (p ≤ 0.1). The permafrost in this peat plateau is likely relict and not in equilibrium with current climatic conditions. Since the early 20th century, there has been a regional increase in air temperature and snow depth. If the ongoing permafrost warming in Tavvavuoma is a result of these long‐term trends, short‐term variability in meteorological parameters can still have an impact on the rate of permafrost degradation, but unless pronounced climate cooling occurs, thawing of the peat plateau is inevitable. Copyright © 2015 John Wiley & Sons, Ltd. Article in Journal/Newspaper Peat Peat plateau permafrost Subarctic RePEc (Research Papers in Economics) Tavvavuoma ENVELOPE(20.860,20.860,68.520,68.520) Permafrost and Periglacial Processes 27 2 177 188 |
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Open Polar |
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RePEc (Research Papers in Economics) |
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ftrepec |
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description |
Because climate change can affect the carbon balance and hydrology in permafrost peatlands, a better understanding of their sensitivity to changes in temperature and precipitation is needed. In Tavvavuoma, northernmost Sweden, meteorological parameters and ground thermal properties have been monitored in a peat plateau from 2006 to 2013. During this time period, the air temperature record shows no warming trend, and the late‐season thaw depth has been relatively stable at around 55–60 cm. Meanwhile, the mean annual ground temperature at 1 m depth has increased by 0.06 °C/yr and at 2–5 m depth the permafrost is currently warmer than ‐0.3 °C. Statistical analyses suggest that interannual changes in thaw depth and ground temperatures are affected by different meteorological factors. Summer air temperatures and annual thawing degree‐days control thaw depth (p ≤ 0.05), whereas winter precipitation/snow depth affects ground temperatures (p ≤ 0.1). The permafrost in this peat plateau is likely relict and not in equilibrium with current climatic conditions. Since the early 20th century, there has been a regional increase in air temperature and snow depth. If the ongoing permafrost warming in Tavvavuoma is a result of these long‐term trends, short‐term variability in meteorological parameters can still have an impact on the rate of permafrost degradation, but unless pronounced climate cooling occurs, thawing of the peat plateau is inevitable. Copyright © 2015 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
A. Britta K. Sannel Gustaf Hugelius Peter Jansson Peter Kuhry |
spellingShingle |
A. Britta K. Sannel Gustaf Hugelius Peter Jansson Peter Kuhry Permafrost Warming in a Subarctic Peatland – Which Meteorological Controls are Most Important? |
author_facet |
A. Britta K. Sannel Gustaf Hugelius Peter Jansson Peter Kuhry |
author_sort |
A. Britta K. Sannel |
title |
Permafrost Warming in a Subarctic Peatland – Which Meteorological Controls are Most Important? |
title_short |
Permafrost Warming in a Subarctic Peatland – Which Meteorological Controls are Most Important? |
title_full |
Permafrost Warming in a Subarctic Peatland – Which Meteorological Controls are Most Important? |
title_fullStr |
Permafrost Warming in a Subarctic Peatland – Which Meteorological Controls are Most Important? |
title_full_unstemmed |
Permafrost Warming in a Subarctic Peatland – Which Meteorological Controls are Most Important? |
title_sort |
permafrost warming in a subarctic peatland – which meteorological controls are most important? |
url |
https://doi.org/10.1002/ppp.1862 |
long_lat |
ENVELOPE(20.860,20.860,68.520,68.520) |
geographic |
Tavvavuoma |
geographic_facet |
Tavvavuoma |
genre |
Peat Peat plateau permafrost Subarctic |
genre_facet |
Peat Peat plateau permafrost Subarctic |
op_relation |
https://doi.org/10.1002/ppp.1862 |
op_doi |
https://doi.org/10.1002/ppp.1862 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
27 |
container_issue |
2 |
container_start_page |
177 |
op_container_end_page |
188 |
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1766162744106549248 |