Simulated range of mid-Holocene precipitation changes from extended lakes and wetlands over North Africa

Abstract ∘ farther north in simulations with a maximum lake or wetland extent than in simulations with a small lake extent. This northward extent is caused by a stronger and prolonged monsoon rainfall season over North Africa which is associated with an increased monsoon precipitation over the southern Sahara and an increased precipitation from tropical plumes over the northwestern Sahara. Replacing lakes with vegetated wetlands causes an enhanced precipitation increase, which is likely due to the high surface roughness of the wetlands. A moisture budget analysis reveals that both lakes and wetlands cause a local precipitation increase not only by enhanced evaporation but also by a stronger inland moisture transport and local moisture recycling to the south of Lake Chad and the west Saharan lakes. Analysis of the dynamic response shows that lakes and wetlands cause a circulation response inverse to the one associated with the Saharan heat low. Depending on the latitudinal position of the lakes and wetlands, they predominantly cause a northward shift or a decay of the African Easterly Jet. These results indicate that the latitudinal position of the lakes and wetlands strongly affects the northward extension of the African summer monsoon.

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
Simulated range of mid-Holocene precipitation changes from extended lakes and wetlands over North Africa ; volume:18 ; number:5 ; year:2022 ; pages:1035-1046 ; extent:12
Climate of the past ; 18, Heft 5 (2022), 1035-1046 (gesamt 12)

Urheber
Specht, Nora Farina
Claussen, Martin
Kleinen, Thomas

DOI
10.5194/cp-18-1035-2022
URN
urn:nbn:de:101:1-2022051905393207439945
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
15.08.2025, 07:23 MESZ

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