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50-year seasonal variability in East African droughts and floods recorded in central Afar lake sediments and their connections with the El Niño-Southern Oscillation

Understanding past and present hydrosystem feedbacks to global ocean-atmospheric interactions represents one of the main challenges to preventing droughts, extreme events, and related human catastrophes in the face of global warming, especially in arid and semiarid environments. In eastern Africa, t...

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Bibliographic Details
Published in:Climate of the past 2024-08, Vol.20 (8), p.1837-1860
Main Authors: Mologni, Carlo, Revel, Marie, Chaumillon, Eric, Malet, Emmanuel, Coulombier, Thibault, Sabatier, Pierre, Brigode, Pierre, Hervé, Gwenael, Develle, Anne-Lise, Schenini, Laure, Messous, Medhi, Davtian, Gourguen, Carré, Alain, Bosch, Delphine, Volto, Natacha, Ménard, Clément, Khalidi, Lamya, Arnaud, Fabien
Format: Article
Language:English
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Summary:Understanding past and present hydrosystem feedbacks to global ocean-atmospheric interactions represents one of the main challenges to preventing droughts, extreme events, and related human catastrophes in the face of global warming, especially in arid and semiarid environments. In eastern Africa, the El Niño-Southern Oscillation (ENSO) was identified as one of the primary drivers of precipitation variability affecting water availability. However, the northern East African Rift System (EARS) still suffers from the underrepresentation of predictive and ENSO teleconnection models because of the scarcity of local to regional historical or palaeo-data.
ISSN:1814-9332
1814-9324
1814-9332
DOI:10.5194/cp-20-1837-2024