DOI 10.1007/s10584-008-9413-1 The millennial atmospheric lifetime of anthropogenic CO 2
public at large that the climate impacts of fossil fuel CO 2 release will only persist for a few centuries. This conclusion has no basis in theory or models of the atmosphere/ocean carbon cycle, which we review here. The largest fraction of the CO 2 recovery will take place on time scales of centuri...
Main Authors: | , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
2006
|
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.150.7135 http://www.atmos-dynamics.damtp.cam.ac.uk/people/mem/archer-carbon-tail08.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.150.7135 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.150.7135 2023-05-15T16:37:44+02:00 DOI 10.1007/s10584-008-9413-1 The millennial atmospheric lifetime of anthropogenic CO 2 David Archer Victor Brovkin The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.150.7135 http://www.atmos-dynamics.damtp.cam.ac.uk/people/mem/archer-carbon-tail08.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.150.7135 http://www.atmos-dynamics.damtp.cam.ac.uk/people/mem/archer-carbon-tail08.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.atmos-dynamics.damtp.cam.ac.uk/people/mem/archer-carbon-tail08.pdf text 2006 ftciteseerx 2016-01-07T15:20:14Z public at large that the climate impacts of fossil fuel CO 2 release will only persist for a few centuries. This conclusion has no basis in theory or models of the atmosphere/ocean carbon cycle, which we review here. The largest fraction of the CO 2 recovery will take place on time scales of centuries, as CO 2 invades the ocean, but a significant fraction of the fossil fuel CO 2, ranging in published models in the literature from 20–60%, remains airborne for a thousand years or longer. Ultimate recovery takes place on time scales of hundreds of thousands of years, a geologic longevity typically associated in public perceptions with nuclear waste. The glacial/interglacial climate cycles demonstrate that ice sheets and sea level respond dramatically to millennial-timescale changes in climate forcing. There are also potential positive feedbacks in the carbon cycle, including methane hydrates in the ocean, and peat frozen in permafrost, that are most sensitive to the long tail of the fossil fuel CO 2 in the atmosphere. 1 Text Ice permafrost Unknown |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
public at large that the climate impacts of fossil fuel CO 2 release will only persist for a few centuries. This conclusion has no basis in theory or models of the atmosphere/ocean carbon cycle, which we review here. The largest fraction of the CO 2 recovery will take place on time scales of centuries, as CO 2 invades the ocean, but a significant fraction of the fossil fuel CO 2, ranging in published models in the literature from 20–60%, remains airborne for a thousand years or longer. Ultimate recovery takes place on time scales of hundreds of thousands of years, a geologic longevity typically associated in public perceptions with nuclear waste. The glacial/interglacial climate cycles demonstrate that ice sheets and sea level respond dramatically to millennial-timescale changes in climate forcing. There are also potential positive feedbacks in the carbon cycle, including methane hydrates in the ocean, and peat frozen in permafrost, that are most sensitive to the long tail of the fossil fuel CO 2 in the atmosphere. 1 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
David Archer Victor Brovkin |
spellingShingle |
David Archer Victor Brovkin DOI 10.1007/s10584-008-9413-1 The millennial atmospheric lifetime of anthropogenic CO 2 |
author_facet |
David Archer Victor Brovkin |
author_sort |
David Archer |
title |
DOI 10.1007/s10584-008-9413-1 The millennial atmospheric lifetime of anthropogenic CO 2 |
title_short |
DOI 10.1007/s10584-008-9413-1 The millennial atmospheric lifetime of anthropogenic CO 2 |
title_full |
DOI 10.1007/s10584-008-9413-1 The millennial atmospheric lifetime of anthropogenic CO 2 |
title_fullStr |
DOI 10.1007/s10584-008-9413-1 The millennial atmospheric lifetime of anthropogenic CO 2 |
title_full_unstemmed |
DOI 10.1007/s10584-008-9413-1 The millennial atmospheric lifetime of anthropogenic CO 2 |
title_sort |
doi 10.1007/s10584-008-9413-1 the millennial atmospheric lifetime of anthropogenic co 2 |
publishDate |
2006 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.150.7135 http://www.atmos-dynamics.damtp.cam.ac.uk/people/mem/archer-carbon-tail08.pdf |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
http://www.atmos-dynamics.damtp.cam.ac.uk/people/mem/archer-carbon-tail08.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.150.7135 http://www.atmos-dynamics.damtp.cam.ac.uk/people/mem/archer-carbon-tail08.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766028037069996032 |