Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale

Anthropogenic climate change threatens northern permafrost environments. This compromises the existence of permafrost landforms, such as palsas and peat plateaus, which have been assessed to be critically endangered habitats. In this study, we integrated geospatial datasets and statistical methods t...

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Published in:The Cryosphere
Main Authors: Leppiniemi, Oona, Karjalainen, Olli, Aalto, Juha, Luoto, Miska, Hjort, Jan
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-3157-2023
https://tc.copernicus.org/articles/17/3157/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc104907 2023-09-05T13:22:23+02:00 Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale Leppiniemi, Oona Karjalainen, Olli Aalto, Juha Luoto, Miska Hjort, Jan 2023-08-08 application/pdf https://doi.org/10.5194/tc-17-3157-2023 https://tc.copernicus.org/articles/17/3157/2023/ eng eng doi:10.5194/tc-17-3157-2023 https://tc.copernicus.org/articles/17/3157/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-3157-2023 2023-08-14T16:24:22Z Anthropogenic climate change threatens northern permafrost environments. This compromises the existence of permafrost landforms, such as palsas and peat plateaus, which have been assessed to be critically endangered habitats. In this study, we integrated geospatial datasets and statistical methods to model the suitable environments for palsas and peat plateaus across the Northern Hemisphere permafrost region. The models were calibrated using data from years 1950–2000. The effects of climate change on the suitable environments for the landforms were assessed by using low-, moderate-, and high-emissions scenarios (Representative Concentration Pathway climate scenarios: RCP2.6, RCP4.5, and RCP8.5, respectively) for two periods (2041–2060 and 2061–2080). Hotspots for palsa and peat plateau environments occurred in northern Europe, western Siberia, and subarctic Canada. Climate change was predicted to cause an almost complete loss (decrease of 98.2 %) of suitable environmental spaces under the high-emissions scenario by 2061–2080, while under low- and moderate-emissions scenarios the predicted loss was 76.3 % and 89.3 % respectively. Our modeling results are in line with previously published thermokarst data pointing out areas of recent degradation of palsa and peat plateau environments. Our results provide new insights into the distribution of the permafrost landforms in less studied areas such as central and eastern Siberia. In addition, the predictions provide new understanding of the changing geoecological conditions of the circumpolar region with important implications for greenhouse gas emissions. Text palsa palsas Peat Peat plateau permafrost Subarctic Thermokarst Siberia Copernicus Publications: E-Journals Canada The Cryosphere 17 8 3157 3176
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Anthropogenic climate change threatens northern permafrost environments. This compromises the existence of permafrost landforms, such as palsas and peat plateaus, which have been assessed to be critically endangered habitats. In this study, we integrated geospatial datasets and statistical methods to model the suitable environments for palsas and peat plateaus across the Northern Hemisphere permafrost region. The models were calibrated using data from years 1950–2000. The effects of climate change on the suitable environments for the landforms were assessed by using low-, moderate-, and high-emissions scenarios (Representative Concentration Pathway climate scenarios: RCP2.6, RCP4.5, and RCP8.5, respectively) for two periods (2041–2060 and 2061–2080). Hotspots for palsa and peat plateau environments occurred in northern Europe, western Siberia, and subarctic Canada. Climate change was predicted to cause an almost complete loss (decrease of 98.2 %) of suitable environmental spaces under the high-emissions scenario by 2061–2080, while under low- and moderate-emissions scenarios the predicted loss was 76.3 % and 89.3 % respectively. Our modeling results are in line with previously published thermokarst data pointing out areas of recent degradation of palsa and peat plateau environments. Our results provide new insights into the distribution of the permafrost landforms in less studied areas such as central and eastern Siberia. In addition, the predictions provide new understanding of the changing geoecological conditions of the circumpolar region with important implications for greenhouse gas emissions.
format Text
author Leppiniemi, Oona
Karjalainen, Olli
Aalto, Juha
Luoto, Miska
Hjort, Jan
spellingShingle Leppiniemi, Oona
Karjalainen, Olli
Aalto, Juha
Luoto, Miska
Hjort, Jan
Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale
author_facet Leppiniemi, Oona
Karjalainen, Olli
Aalto, Juha
Luoto, Miska
Hjort, Jan
author_sort Leppiniemi, Oona
title Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale
title_short Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale
title_full Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale
title_fullStr Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale
title_full_unstemmed Environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale
title_sort environmental spaces for palsas and peat plateaus are disappearing at a circumpolar scale
publishDate 2023
url https://doi.org/10.5194/tc-17-3157-2023
https://tc.copernicus.org/articles/17/3157/2023/
geographic Canada
geographic_facet Canada
genre palsa
palsas
Peat
Peat plateau
permafrost
Subarctic
Thermokarst
Siberia
genre_facet palsa
palsas
Peat
Peat plateau
permafrost
Subarctic
Thermokarst
Siberia
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-3157-2023
https://tc.copernicus.org/articles/17/3157/2023/
op_doi https://doi.org/10.5194/tc-17-3157-2023
container_title The Cryosphere
container_volume 17
container_issue 8
container_start_page 3157
op_container_end_page 3176
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