Satellite-derived changes in the permafrost landscape of central Yakutia, 2000-2011: Wetting, drying, and fires

International audience The focus of this research has been on detecting changes in lake areas, vegetation, land surface temperatures, and the area covered by snow, using data from remote sensing. The study area covers the main (central) part of the Lena River catchment in the Yakutia region of Siber...

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Published in:Global and Planetary Change
Main Authors: Boike, Julia, Grau, Thomas, Heim, Birgit, Günther, Frank, Langer, Moritz, Muster, Sina, Gouttevin, Isabelle, Lange, Stephan
Other Authors: Alfred Wegener Institute Potsdam, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Department Computational Hydrosystems UFZ Leipzig, Helmholtz Zentrum für Umweltforschung = Helmholtz Centre for Environmental Research (UFZ), Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2016
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-01387168
https://doi.org/10.1016/j.gloplacha.2016.01.001
id ftccsdartic:oai:HAL:insu-01387168v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic Land surface warming
Remote sensing
Permafrost
Central Yakutia
Lakes
Land cover
[SDE]Environmental Sciences
spellingShingle Land surface warming
Remote sensing
Permafrost
Central Yakutia
Lakes
Land cover
[SDE]Environmental Sciences
Boike, Julia
Grau, Thomas
Heim, Birgit
Günther, Frank
Langer, Moritz
Muster, Sina
Gouttevin, Isabelle,
Lange, Stephan
Satellite-derived changes in the permafrost landscape of central Yakutia, 2000-2011: Wetting, drying, and fires
topic_facet Land surface warming
Remote sensing
Permafrost
Central Yakutia
Lakes
Land cover
[SDE]Environmental Sciences
description International audience The focus of this research has been on detecting changes in lake areas, vegetation, land surface temperatures, and the area covered by snow, using data from remote sensing. The study area covers the main (central) part of the Lena River catchment in the Yakutia region of Siberia (Russia), extending from east of Yakutsk to the central Siberian Plateau, and from the southern Lena River to north of the Vilyui River. Approximately 90% of the area is underlain by continuous permafrost. Remote sensing products were used to analyze changes in water bodies, land surface temperature (LST), and leaf area index (LAI), as well as the occurrence and extent of forest fires, and the area and duration of snow cover. The remote sensing analyses (for LST, snow cover, LAI, and fire) were based on MODIS–derived NASA products (250–1000 m) for 2000 to 2011. Changes in water bodies were calculated from two mosaics of (USGS) Landsat (30 m) satellite images from 2002 and 2009. Within the study area's 315,000 km2 the total area covered by lakes increased by 17.9% between 2002 and 2009, but this increase varied in different parts of the study area, ranging between 11% and 42%.The land surface temperatures showed a consistent warming trend, with an average increase of about 0.12 °C/year. The average rate of warming during the April–May transition period was 0.17 °C/year and 0.19 °C/year in the September–October period, but ranged up to 0.49 °C/year during September–October. Regional differences in the rates of land surface temperature change, and possible reasons for the temperature changes, are discussed with respect to changes in the land cover.Our analysis of a broad spectrum of variables over the study area suggests that the spring warming trend is very likely to be due to changes in the area covered by snow. The warming trend observed in fall does not, however, appear to be directly related to any changes in the area of snow cover, or to the atmospheric conditions, or to the proportion of the land surface that ...
author2 Alfred Wegener Institute Potsdam
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI)
Department Computational Hydrosystems UFZ Leipzig
Helmholtz Zentrum für Umweltforschung = Helmholtz Centre for Environmental Research (UFZ)
Laboratoire de glaciologie et géophysique de l'environnement (LGGE)
Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG )
Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )
Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)
format Article in Journal/Newspaper
author Boike, Julia
Grau, Thomas
Heim, Birgit
Günther, Frank
Langer, Moritz
Muster, Sina
Gouttevin, Isabelle,
Lange, Stephan
author_facet Boike, Julia
Grau, Thomas
Heim, Birgit
Günther, Frank
Langer, Moritz
Muster, Sina
Gouttevin, Isabelle,
Lange, Stephan
author_sort Boike, Julia
title Satellite-derived changes in the permafrost landscape of central Yakutia, 2000-2011: Wetting, drying, and fires
title_short Satellite-derived changes in the permafrost landscape of central Yakutia, 2000-2011: Wetting, drying, and fires
title_full Satellite-derived changes in the permafrost landscape of central Yakutia, 2000-2011: Wetting, drying, and fires
title_fullStr Satellite-derived changes in the permafrost landscape of central Yakutia, 2000-2011: Wetting, drying, and fires
title_full_unstemmed Satellite-derived changes in the permafrost landscape of central Yakutia, 2000-2011: Wetting, drying, and fires
title_sort satellite-derived changes in the permafrost landscape of central yakutia, 2000-2011: wetting, drying, and fires
publisher HAL CCSD
publishDate 2016
url https://hal-insu.archives-ouvertes.fr/insu-01387168
https://doi.org/10.1016/j.gloplacha.2016.01.001
geographic Yakutsk
geographic_facet Yakutsk
genre lena river
permafrost
Yakutia
Yakutsk
Siberia
genre_facet lena river
permafrost
Yakutia
Yakutsk
Siberia
op_source ISSN: 0921-8181
Global and Planetary Change
https://hal-insu.archives-ouvertes.fr/insu-01387168
Global and Planetary Change, Elsevier, 2016, 139 (april 2016), pp.116-127. ⟨10.1016/j.gloplacha.2016.01.001⟩
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insu-01387168
https://hal-insu.archives-ouvertes.fr/insu-01387168
doi:10.1016/j.gloplacha.2016.01.001
IRSTEA: PUB00052191
op_doi https://doi.org/10.1016/j.gloplacha.2016.01.001
container_title Global and Planetary Change
container_volume 139
container_start_page 116
op_container_end_page 127
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spelling ftccsdartic:oai:HAL:insu-01387168v1 2023-05-15T17:07:39+02:00 Satellite-derived changes in the permafrost landscape of central Yakutia, 2000-2011: Wetting, drying, and fires Boike, Julia Grau, Thomas Heim, Birgit Günther, Frank Langer, Moritz Muster, Sina Gouttevin, Isabelle, Lange, Stephan Alfred Wegener Institute Potsdam Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI) Department Computational Hydrosystems UFZ Leipzig Helmholtz Zentrum für Umweltforschung = Helmholtz Centre for Environmental Research (UFZ) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ) Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) 2016 https://hal-insu.archives-ouvertes.fr/insu-01387168 https://doi.org/10.1016/j.gloplacha.2016.01.001 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gloplacha.2016.01.001 insu-01387168 https://hal-insu.archives-ouvertes.fr/insu-01387168 doi:10.1016/j.gloplacha.2016.01.001 IRSTEA: PUB00052191 ISSN: 0921-8181 Global and Planetary Change https://hal-insu.archives-ouvertes.fr/insu-01387168 Global and Planetary Change, Elsevier, 2016, 139 (april 2016), pp.116-127. ⟨10.1016/j.gloplacha.2016.01.001⟩ Land surface warming Remote sensing Permafrost Central Yakutia Lakes Land cover [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2016 ftccsdartic https://doi.org/10.1016/j.gloplacha.2016.01.001 2021-12-05T02:57:10Z International audience The focus of this research has been on detecting changes in lake areas, vegetation, land surface temperatures, and the area covered by snow, using data from remote sensing. The study area covers the main (central) part of the Lena River catchment in the Yakutia region of Siberia (Russia), extending from east of Yakutsk to the central Siberian Plateau, and from the southern Lena River to north of the Vilyui River. Approximately 90% of the area is underlain by continuous permafrost. Remote sensing products were used to analyze changes in water bodies, land surface temperature (LST), and leaf area index (LAI), as well as the occurrence and extent of forest fires, and the area and duration of snow cover. The remote sensing analyses (for LST, snow cover, LAI, and fire) were based on MODIS–derived NASA products (250–1000 m) for 2000 to 2011. Changes in water bodies were calculated from two mosaics of (USGS) Landsat (30 m) satellite images from 2002 and 2009. Within the study area's 315,000 km2 the total area covered by lakes increased by 17.9% between 2002 and 2009, but this increase varied in different parts of the study area, ranging between 11% and 42%.The land surface temperatures showed a consistent warming trend, with an average increase of about 0.12 °C/year. The average rate of warming during the April–May transition period was 0.17 °C/year and 0.19 °C/year in the September–October period, but ranged up to 0.49 °C/year during September–October. Regional differences in the rates of land surface temperature change, and possible reasons for the temperature changes, are discussed with respect to changes in the land cover.Our analysis of a broad spectrum of variables over the study area suggests that the spring warming trend is very likely to be due to changes in the area covered by snow. The warming trend observed in fall does not, however, appear to be directly related to any changes in the area of snow cover, or to the atmospheric conditions, or to the proportion of the land surface that ... Article in Journal/Newspaper lena river permafrost Yakutia Yakutsk Siberia Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Yakutsk Global and Planetary Change 139 116 127