Phytomass and soil carbon storage of different land cover classes in the Usa river basin ...

This study describes detailed partitioning of phytomass carbon (C) and soil organic carbon (SOC) for four study areas in discontinuous permafrost terrain, Northeast European Russia. The mean aboveground phytomass C storage is 0.7 kg C/m**2. Estimated landscape SOC storage in the four areas varies be...

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Main Authors: Hugelius, Gustaf, Virtanen, Tarmo A, Kaverin, Dmitry, Pastukhov, Alexander, Rivkin, Felix, Marchenko, Sergey, Romanovsky, Vladimir E, Kuhry, Peter
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2011
Subjects:
IPY
Online Access:https://dx.doi.org/10.1594/pangaea.811368
https://doi.pangaea.de/10.1594/PANGAEA.811368
id ftdatacite:10.1594/pangaea.811368
record_format openpolar
spelling ftdatacite:10.1594/pangaea.811368 2024-02-27T08:32:29+00:00 Phytomass and soil carbon storage of different land cover classes in the Usa river basin ... Hugelius, Gustaf Virtanen, Tarmo A Kaverin, Dmitry Pastukhov, Alexander Rivkin, Felix Marchenko, Sergey Romanovsky, Vladimir E Kuhry, Peter 2011 application/zip https://dx.doi.org/10.1594/pangaea.811368 https://doi.pangaea.de/10.1594/PANGAEA.811368 en eng PANGAEA https://dx.doi.org/10.1029/2010jg001606 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 International Polar Year 2007-2008 IPY Supplementary Publication Series of Datasets Collection article 2011 ftdatacite https://doi.org/10.1594/pangaea.81136810.1029/2010jg001606 2024-02-01T16:54:49Z This study describes detailed partitioning of phytomass carbon (C) and soil organic carbon (SOC) for four study areas in discontinuous permafrost terrain, Northeast European Russia. The mean aboveground phytomass C storage is 0.7 kg C/m**2. Estimated landscape SOC storage in the four areas varies between 34.5 and 47.0 kg C/m**2 with LCC (land cover classification) upscaling and 32.5-49.0 kg C/m**2 with soil map upscaling. A nested upscaling approach using a Landsat thematic mapper land cover classification for the surrounding region provides estimates within 5 ± 5% of the local high-resolution estimates. Permafrost peat plateaus hold the majority of total and frozen SOC, especially in the more southern study areas. Burying of SOC through cryoturbation of O- or A-horizons contributes between 1% and 16% (mean 5%) of total landscape SOC. The effect of active layer deepening and thermokarst expansion on SOC remobilization is modeled for one of the four areas. The active layer thickness dynamics from 1980 to 2099 ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Article in Journal/Newspaper Active layer thickness International Polar Year IPY Peat permafrost Thermokarst DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic International Polar Year 2007-2008 IPY
spellingShingle International Polar Year 2007-2008 IPY
Hugelius, Gustaf
Virtanen, Tarmo A
Kaverin, Dmitry
Pastukhov, Alexander
Rivkin, Felix
Marchenko, Sergey
Romanovsky, Vladimir E
Kuhry, Peter
Phytomass and soil carbon storage of different land cover classes in the Usa river basin ...
topic_facet International Polar Year 2007-2008 IPY
description This study describes detailed partitioning of phytomass carbon (C) and soil organic carbon (SOC) for four study areas in discontinuous permafrost terrain, Northeast European Russia. The mean aboveground phytomass C storage is 0.7 kg C/m**2. Estimated landscape SOC storage in the four areas varies between 34.5 and 47.0 kg C/m**2 with LCC (land cover classification) upscaling and 32.5-49.0 kg C/m**2 with soil map upscaling. A nested upscaling approach using a Landsat thematic mapper land cover classification for the surrounding region provides estimates within 5 ± 5% of the local high-resolution estimates. Permafrost peat plateaus hold the majority of total and frozen SOC, especially in the more southern study areas. Burying of SOC through cryoturbation of O- or A-horizons contributes between 1% and 16% (mean 5%) of total landscape SOC. The effect of active layer deepening and thermokarst expansion on SOC remobilization is modeled for one of the four areas. The active layer thickness dynamics from 1980 to 2099 ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ...
format Article in Journal/Newspaper
author Hugelius, Gustaf
Virtanen, Tarmo A
Kaverin, Dmitry
Pastukhov, Alexander
Rivkin, Felix
Marchenko, Sergey
Romanovsky, Vladimir E
Kuhry, Peter
author_facet Hugelius, Gustaf
Virtanen, Tarmo A
Kaverin, Dmitry
Pastukhov, Alexander
Rivkin, Felix
Marchenko, Sergey
Romanovsky, Vladimir E
Kuhry, Peter
author_sort Hugelius, Gustaf
title Phytomass and soil carbon storage of different land cover classes in the Usa river basin ...
title_short Phytomass and soil carbon storage of different land cover classes in the Usa river basin ...
title_full Phytomass and soil carbon storage of different land cover classes in the Usa river basin ...
title_fullStr Phytomass and soil carbon storage of different land cover classes in the Usa river basin ...
title_full_unstemmed Phytomass and soil carbon storage of different land cover classes in the Usa river basin ...
title_sort phytomass and soil carbon storage of different land cover classes in the usa river basin ...
publisher PANGAEA
publishDate 2011
url https://dx.doi.org/10.1594/pangaea.811368
https://doi.pangaea.de/10.1594/PANGAEA.811368
genre Active layer thickness
International Polar Year
IPY
Peat
permafrost
Thermokarst
genre_facet Active layer thickness
International Polar Year
IPY
Peat
permafrost
Thermokarst
op_relation https://dx.doi.org/10.1029/2010jg001606
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.81136810.1029/2010jg001606
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