Climate feedbacks at the tundra-taiga interface

Feedbacks, or internal interactions, play a crucial role in the climate system. Negative feedback will reduce the impact of an external perturbation, a positive feedback will amplify the effect and could lead to an unstable system. Many of the feedbacks found in the climate system are positive; thus...

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Main Authors: Harding, Richard, Kuhry, Peter, Christensen, Torben R., Sykes, Martin T., Dankers, Rutger, Van der Linden, Sandra
Format: Article in Journal/Newspaper
Language:English
Published: 2002
Subjects:
Online Access:https://research.wur.nl/en/publications/climate-feedbacks-at-the-tundra-taiga-interface
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spelling ftunivwagenin:oai:library.wur.nl:wurpubs/566635 2024-02-04T09:58:00+01:00 Climate feedbacks at the tundra-taiga interface Harding, Richard Kuhry, Peter Christensen, Torben R. Sykes, Martin T. Dankers, Rutger Van der Linden, Sandra 2002 https://research.wur.nl/en/publications/climate-feedbacks-at-the-tundra-taiga-interface en eng https://research.wur.nl/en/publications/climate-feedbacks-at-the-tundra-taiga-interface info:eu-repo/semantics/closedAccess Wageningen University & Research Ambio 31 (2002) SPEC. ISS. 12 ISSN: 0044-7447 Life Science info:eu-repo/semantics/article Article/Letter to editor info:eu-repo/semantics/publishedVersion 2002 ftunivwagenin 2024-01-10T23:27:21Z Feedbacks, or internal interactions, play a crucial role in the climate system. Negative feedback will reduce the impact of an external perturbation, a positive feedback will amplify the effect and could lead to an unstable system. Many of the feedbacks found in the climate system are positive; thus, for example, increasing CO2 levels will increase temperature, reduce the snow cover, increase the absorption of radiation and hence increase temperature further. The most obvious feedbacks, such as the snow example quoted above, are already included within our models of the climate and earth system. Others, such as the impact of increasing forest cover due to global warming, are only just being included. Others, such as, the impact of global warming on the northern peatlands and the impact of freshwater flows on the Arctic Ocean are not yet considered. The contrast in surface characteristics between low tundra vegetation to high taiga forest is considerable. The contrast is greatest in the winter, when the tundra is snow covered but the trees of the taiga protrude through the snow pack, and is probably the greatest contrast found on the land surface anywhere. This variation causes massive changes in the energy fluxes at the surface and hence the temperature conditions on the ground and within the atmosphere. There will be large resultant changes in the vegetation development, the carbon fluxes, the permafrost and the hydrology. The Arctic is already experiencing change and it is essential for us to understand the basic processes, and how these interact, to be confident of our predictions of environmental change in the future. Article in Journal/Newspaper Arctic Arctic Ocean Global warming permafrost taiga Tundra Wageningen UR (University & Research Centre): Digital Library Arctic Arctic Ocean
institution Open Polar
collection Wageningen UR (University & Research Centre): Digital Library
op_collection_id ftunivwagenin
language English
topic Life Science
spellingShingle Life Science
Harding, Richard
Kuhry, Peter
Christensen, Torben R.
Sykes, Martin T.
Dankers, Rutger
Van der Linden, Sandra
Climate feedbacks at the tundra-taiga interface
topic_facet Life Science
description Feedbacks, or internal interactions, play a crucial role in the climate system. Negative feedback will reduce the impact of an external perturbation, a positive feedback will amplify the effect and could lead to an unstable system. Many of the feedbacks found in the climate system are positive; thus, for example, increasing CO2 levels will increase temperature, reduce the snow cover, increase the absorption of radiation and hence increase temperature further. The most obvious feedbacks, such as the snow example quoted above, are already included within our models of the climate and earth system. Others, such as the impact of increasing forest cover due to global warming, are only just being included. Others, such as, the impact of global warming on the northern peatlands and the impact of freshwater flows on the Arctic Ocean are not yet considered. The contrast in surface characteristics between low tundra vegetation to high taiga forest is considerable. The contrast is greatest in the winter, when the tundra is snow covered but the trees of the taiga protrude through the snow pack, and is probably the greatest contrast found on the land surface anywhere. This variation causes massive changes in the energy fluxes at the surface and hence the temperature conditions on the ground and within the atmosphere. There will be large resultant changes in the vegetation development, the carbon fluxes, the permafrost and the hydrology. The Arctic is already experiencing change and it is essential for us to understand the basic processes, and how these interact, to be confident of our predictions of environmental change in the future.
format Article in Journal/Newspaper
author Harding, Richard
Kuhry, Peter
Christensen, Torben R.
Sykes, Martin T.
Dankers, Rutger
Van der Linden, Sandra
author_facet Harding, Richard
Kuhry, Peter
Christensen, Torben R.
Sykes, Martin T.
Dankers, Rutger
Van der Linden, Sandra
author_sort Harding, Richard
title Climate feedbacks at the tundra-taiga interface
title_short Climate feedbacks at the tundra-taiga interface
title_full Climate feedbacks at the tundra-taiga interface
title_fullStr Climate feedbacks at the tundra-taiga interface
title_full_unstemmed Climate feedbacks at the tundra-taiga interface
title_sort climate feedbacks at the tundra-taiga interface
publishDate 2002
url https://research.wur.nl/en/publications/climate-feedbacks-at-the-tundra-taiga-interface
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Global warming
permafrost
taiga
Tundra
genre_facet Arctic
Arctic Ocean
Global warming
permafrost
taiga
Tundra
op_source Ambio 31 (2002) SPEC. ISS. 12
ISSN: 0044-7447
op_relation https://research.wur.nl/en/publications/climate-feedbacks-at-the-tundra-taiga-interface
op_rights info:eu-repo/semantics/closedAccess
Wageningen University & Research
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