Dynamic interaction between lakes, climate, and vegetation across northern Africa during the mid-Holocene
Abstract m, without changing the horizontal lake area. By reducing the depth of Lake Chad, the heat storage capacity of the lake decreases, and the lake warms faster during the summer months. Thus, in the ICON-JSBACH4 model, the lake depth significantly influences the simulated surface temperature and the simulated meridional surface-temperature gradient between the simulated lakes and vegetation, thereby affecting mid-Holocene precipitation over northern Africa.
- Standort
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Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
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Online-Ressource
- Sprache
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Englisch
- Erschienen in
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Dynamic interaction between lakes, climate, and vegetation across northern Africa during the mid-Holocene ; volume:20 ; number:7 ; year:2024 ; pages:1595-1613 ; extent:19
Climate of the past ; 20, Heft 7 (2024), 1595-1613 (gesamt 19)
- Urheber
- DOI
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10.5194/cp-20-1595-2024
- URN
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urn:nbn:de:101:1-2408061447064.979826178211
- Rechteinformation
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
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14.08.2025, 11:02 MESZ
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Beteiligte
- Specht, Nora Farina
- Claussen, Martin
- Kleinen, Thomas
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