Bioclimatic change as a function of global warming from CMIP6 climate projections
Abstract f Δ T) is estimated by combining the results from the individual models. Despite the discrete nature of the bioclimatic classification scheme, we find only a weakly saturating dependence of this fraction on global warming f 1 - e - 0.14 Δ T, which implies about 13 % of land experiencing a major change in climate per 1 K increase in global mean temperature between the global warming levels of 1 and 3 K. Therefore, we estimate that stabilizing the climate at 1.5 K rather than 2 K of global warming would save over 7.5 million square kilometres of land from a major bioclimatic change.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Bioclimatic change as a function of global warming from CMIP6 climate projections ; volume:20 ; number:2 ; year:2023 ; pages:451-488 ; extent:38
Biogeosciences ; 20, Heft 2 (2023), 451-488 (gesamt 38)
- Creator
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Sparey, Morgan
Cox, Peter
Williamson, Mark S.
- DOI
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10.5194/bg-20-451-2023
- URN
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urn:nbn:de:101:1-2023033007490762424756
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:53 AM CEST
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Associated
- Sparey, Morgan
- Cox, Peter
- Williamson, Mark S.
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