Last Glacial Maximum lacustrine and fluviatile Formations in the Tibesti and other Saharan mountains, and large-scale climatic teleconnections linked to the activity of the Subtropical Jet Stream

2000/11/01 by Jean Maley, J Maley · 3 citations
Earth and Planetary Sciences · #Ecology #Geography #Geological and Geophysical Studies Worldwide #Geological formations and processes #Geology #Geology and Paleoclimatology Research #Glacial period #Holocene #Holocene climatic optimum #Last Glacial Maximum #Oceanography #Paleontology #Physical geography #Pleistocene #Subtropics #Westerlies

paper · doi:10.1016/s0921-8181(00)00039-4

crossref issued 2000/11/01 · crossref published 2000/11/01 · crossref published-print 2000/11/01 · openalex publication_date 2000/11/01 · crossref created 2002/07/25 · crossref deposited 2019/04/28 · openalex created_date 2025/10/10 · crossref indexed 2026/04/29 · openalex updated_date 2026/07/29

Citations

• Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years
• Origin of the northern Atlantic's Heinrich events
• GENERAL CIRCULATION EXPERIMENTS WITH THE PRIMITIVE EQUATIONS

Cited by

• Charophytes as bio-indicators for lake level high stand at “Trou au Natron”, Tibesti, Chad, during the Late Pleistocene
• Holocene Lake Mega-Chad palaeoshorelines from space
• Tibesti Mountains [wikipedia]