Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum
The importance of the biogeophysical atmosphere-vegetation feedback in comparison with the radiative effect of lower atmospheric CO2 concentrations and the presence of ice sheets at the last glacial maximum (LGM) is investigated with the climate system model CLIMBER-2. Equilibrium experiments reveal...
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fttriple:oai:gotriple.eu:10670/1.y2q7sc 2023-05-15T18:30:50+02:00 Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum Jahn, A. Claussen, M. Ganopolski, A. Brovkin, V. 2018-09-27 https://doi.org/10.5194/cp-1-1-2005 https://cp.copernicus.org/articles/1/1/2005/ en eng doi:10.5194/cp-1-1-2005 10670/1.y2q7sc https://cp.copernicus.org/articles/1/1/2005/ undefined Geographica Helvetica - geography eISSN: 1814-9332 geo envir Text https://vocabularies.coar-repositories.org/resource_types/c_18cf/ 2018 fttriple https://doi.org/10.5194/cp-1-1-2005 2023-01-22T18:25:53Z The importance of the biogeophysical atmosphere-vegetation feedback in comparison with the radiative effect of lower atmospheric CO2 concentrations and the presence of ice sheets at the last glacial maximum (LGM) is investigated with the climate system model CLIMBER-2. Equilibrium experiments reveal that most of the global cooling at the LGM (-5.1°C) relative to (natural) present-day conditions is caused by the introduction of ice sheets into the model (-3.0°C), followed by the effect of lower atmospheric CO2 levels at the LGM (-1.5°C), while a synergy between these two factors appears to be very small on global average. The biogeophysical effects of changes in vegetation cover are found to cool the global LGM climate by 0.6°C. The latter are most pronounced in the northern high latitudes, where the taiga-tundra feedback causes annually averaged temperature changes of up to -2.0°C, while the radiative effect of lower atmospheric CO2 in this region only produces a cooling of 1.5°C. Hence, in this region, the temperature changes caused by vegetation dynamics at the LGM exceed the cooling due to lower atmospheric CO2 concentrations. Text taiga Tundra Unknown Climate of the Past 1 1 1 7 |
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geo envir Jahn, A. Claussen, M. Ganopolski, A. Brovkin, V. Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum |
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The importance of the biogeophysical atmosphere-vegetation feedback in comparison with the radiative effect of lower atmospheric CO2 concentrations and the presence of ice sheets at the last glacial maximum (LGM) is investigated with the climate system model CLIMBER-2. Equilibrium experiments reveal that most of the global cooling at the LGM (-5.1°C) relative to (natural) present-day conditions is caused by the introduction of ice sheets into the model (-3.0°C), followed by the effect of lower atmospheric CO2 levels at the LGM (-1.5°C), while a synergy between these two factors appears to be very small on global average. The biogeophysical effects of changes in vegetation cover are found to cool the global LGM climate by 0.6°C. The latter are most pronounced in the northern high latitudes, where the taiga-tundra feedback causes annually averaged temperature changes of up to -2.0°C, while the radiative effect of lower atmospheric CO2 in this region only produces a cooling of 1.5°C. Hence, in this region, the temperature changes caused by vegetation dynamics at the LGM exceed the cooling due to lower atmospheric CO2 concentrations. |
format |
Text |
author |
Jahn, A. Claussen, M. Ganopolski, A. Brovkin, V. |
author_facet |
Jahn, A. Claussen, M. Ganopolski, A. Brovkin, V. |
author_sort |
Jahn, A. |
title |
Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum |
title_short |
Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum |
title_full |
Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum |
title_fullStr |
Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum |
title_full_unstemmed |
Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum |
title_sort |
quantifying the effect of vegetation dynamics on the climate of the last glacial maximum |
publishDate |
2018 |
url |
https://doi.org/10.5194/cp-1-1-2005 https://cp.copernicus.org/articles/1/1/2005/ |
genre |
taiga Tundra |
genre_facet |
taiga Tundra |
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Geographica Helvetica - geography eISSN: 1814-9332 |
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doi:10.5194/cp-1-1-2005 10670/1.y2q7sc https://cp.copernicus.org/articles/1/1/2005/ |
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undefined |
op_doi |
https://doi.org/10.5194/cp-1-1-2005 |
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Climate of the Past |
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