Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra

The potential contribution of high altitude permafrost as a climate feedback is unknown. Here the authors show seven years of sustained carbon emissions from snow-scoured alpine tundra including respiration of older carbon substrate from solifluction lobes associated with permafrost during the winte...

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Published in:Nature Communications
Main Authors: John F. Knowles, Peter D. Blanken, Corey R. Lawrence, Mark W. Williams
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2019
Subjects:
Science
Q
permafrost
Tundra
Online Access:https://doi.org/10.1038/s41467-019-09149-2
https://doaj.org/article/a19005955fed4590bd4c5c030e06d999
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spelling ftdoajarticles:oai:doaj.org/article:a19005955fed4590bd4c5c030e06d999 2023-05-15T17:55:55+02:00 Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra John F. Knowles Peter D. Blanken Corey R. Lawrence Mark W. Williams 2019-03-01T00:00:00Z https://doi.org/10.1038/s41467-019-09149-2 https://doaj.org/article/a19005955fed4590bd4c5c030e06d999 EN eng Nature Portfolio https://doi.org/10.1038/s41467-019-09149-2 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-019-09149-2 2041-1723 https://doaj.org/article/a19005955fed4590bd4c5c030e06d999 Nature Communications, Vol 10, Iss 1, Pp 1-9 (2019) Science Q article 2019 ftdoajarticles https://doi.org/10.1038/s41467-019-09149-2 2022-12-31T13:53:20Z The potential contribution of high altitude permafrost as a climate feedback is unknown. Here the authors show seven years of sustained carbon emissions from snow-scoured alpine tundra including respiration of older carbon substrate from solifluction lobes associated with permafrost during the winter. Article in Journal/Newspaper permafrost Tundra Directory of Open Access Journals: DOAJ Articles Nature Communications 10 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle Science
Q
John F. Knowles
Peter D. Blanken
Corey R. Lawrence
Mark W. Williams
Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra
topic_facet Science
Q
description The potential contribution of high altitude permafrost as a climate feedback is unknown. Here the authors show seven years of sustained carbon emissions from snow-scoured alpine tundra including respiration of older carbon substrate from solifluction lobes associated with permafrost during the winter.
format Article in Journal/Newspaper
author John F. Knowles
Peter D. Blanken
Corey R. Lawrence
Mark W. Williams
author_facet John F. Knowles
Peter D. Blanken
Corey R. Lawrence
Mark W. Williams
author_sort John F. Knowles
title Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra
title_short Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra
title_full Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra
title_fullStr Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra
title_full_unstemmed Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra
title_sort evidence for non-steady-state carbon emissions from snow-scoured alpine tundra
publisher Nature Portfolio
publishDate 2019
url https://doi.org/10.1038/s41467-019-09149-2
https://doaj.org/article/a19005955fed4590bd4c5c030e06d999
genre permafrost
Tundra
genre_facet permafrost
Tundra
op_source Nature Communications, Vol 10, Iss 1, Pp 1-9 (2019)
op_relation https://doi.org/10.1038/s41467-019-09149-2
https://doaj.org/toc/2041-1723
doi:10.1038/s41467-019-09149-2
2041-1723
https://doaj.org/article/a19005955fed4590bd4c5c030e06d999
op_doi https://doi.org/10.1038/s41467-019-09149-2
container_title Nature Communications
container_volume 10
container_issue 1
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