Vegetation-climate feedbacks in a greenhouse world
The potential for feedbacks between terrestrial vegetation, climate, and the atmospheric CO2 partial pressure have been addressed by modelling. Previous research has established that under global warming and CO2 enrichment, the stomatal conductance of vegetation tends to decrease, causing a warming...
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ftpubmed:oai:pubmedcentral.nih.gov:1692170 2023-05-15T18:18:32+02:00 Vegetation-climate feedbacks in a greenhouse world Woodward, F. I. 1998-01-29 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC1692170 https://doi.org/10.1098/rstb.1998.0188 en eng http://www.ncbi.nlm.nih.gov/pmc/articles/PMC1692170 http://dx.doi.org/10.1098/rstb.1998.0188 Article Text 1998 ftpubmed https://doi.org/10.1098/rstb.1998.0188 2013-08-31T12:37:44Z The potential for feedbacks between terrestrial vegetation, climate, and the atmospheric CO2 partial pressure have been addressed by modelling. Previous research has established that under global warming and CO2 enrichment, the stomatal conductance of vegetation tends to decrease, causing a warming effect on top of the driving change in greenhouse warming. At the global scale, this positive feedback is ultimately changed to a negative feedback through changes in vegetation structure. In spatial terms this structural feedback has a variable geographical pattern in terms of magnitude and sign. At high latitudes, increases in vegetation leaf area index (LAI) and vegetation height cause a positive feedback, and warming through reductions in the winter snow-cover albedo. At lower latitudes when vegetation becomes more sparse with warming, the higher albedo of the underlying soil leads to cooling. However, the largest area effects are of negative feedbacks caused by increased evaporative cooling with increasing LAI. These effects do not include feedbacks on the atmospheric CO2 concentration, through changes in the carbon cycle of the vegetation. Modelling experiments, with biogeochemical, physiological and structural feedbacks on atmospheric CO2, but with no changes in precipitation, ocean activity or sea ice formation, have shown that a consequence of the CO2 fertilization effect on vegetation will be a reduction of atmospheric CO2 concentration, in the order of 12% by the year 2100 and a reduced global warming by 0.7°C, in a total greenhouse warming of 3.9°C. Text Sea ice PubMed Central (PMC) Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 353 1365 29 39 |
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Article Woodward, F. I. Vegetation-climate feedbacks in a greenhouse world |
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The potential for feedbacks between terrestrial vegetation, climate, and the atmospheric CO2 partial pressure have been addressed by modelling. Previous research has established that under global warming and CO2 enrichment, the stomatal conductance of vegetation tends to decrease, causing a warming effect on top of the driving change in greenhouse warming. At the global scale, this positive feedback is ultimately changed to a negative feedback through changes in vegetation structure. In spatial terms this structural feedback has a variable geographical pattern in terms of magnitude and sign. At high latitudes, increases in vegetation leaf area index (LAI) and vegetation height cause a positive feedback, and warming through reductions in the winter snow-cover albedo. At lower latitudes when vegetation becomes more sparse with warming, the higher albedo of the underlying soil leads to cooling. However, the largest area effects are of negative feedbacks caused by increased evaporative cooling with increasing LAI. These effects do not include feedbacks on the atmospheric CO2 concentration, through changes in the carbon cycle of the vegetation. Modelling experiments, with biogeochemical, physiological and structural feedbacks on atmospheric CO2, but with no changes in precipitation, ocean activity or sea ice formation, have shown that a consequence of the CO2 fertilization effect on vegetation will be a reduction of atmospheric CO2 concentration, in the order of 12% by the year 2100 and a reduced global warming by 0.7°C, in a total greenhouse warming of 3.9°C. |
format |
Text |
author |
Woodward, F. I. |
author_facet |
Woodward, F. I. |
author_sort |
Woodward, F. I. |
title |
Vegetation-climate feedbacks in a greenhouse world |
title_short |
Vegetation-climate feedbacks in a greenhouse world |
title_full |
Vegetation-climate feedbacks in a greenhouse world |
title_fullStr |
Vegetation-climate feedbacks in a greenhouse world |
title_full_unstemmed |
Vegetation-climate feedbacks in a greenhouse world |
title_sort |
vegetation-climate feedbacks in a greenhouse world |
publishDate |
1998 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC1692170 https://doi.org/10.1098/rstb.1998.0188 |
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Sea ice |
genre_facet |
Sea ice |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC1692170 http://dx.doi.org/10.1098/rstb.1998.0188 |
op_doi |
https://doi.org/10.1098/rstb.1998.0188 |
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Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences |
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353 |
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1365 |
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29 |
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39 |
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