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

Global and Planetary Change

Volumn 26, Issue 1-3, 2000, Pages 121-136

  Maley, J ^a  

^a CNRS   (France)

Author keywords

Heinrich layers; Lake levels; Last Glacial Maximum; Paleoclimatology; Quaternary; Sahara; Subtropical jetstream; The subtropics; Tropical Africa

Indexed keywords

AUSTRALIA; CLIMATE CHANGE; DESERT; MOUNTAIN; SEDIMENT; SOUTH AFRICA; UNITED STATES;

ALLUVIAL DEPOSIT; JET STREAM; LACUSTRINE DEPOSIT; LAST GLACIAL MAXIMUM; PALEOENVIRONMENT; PLEISTOCENE; TELECONNECTION;

AFRICA;

EID: 0033711704     PISSN: 09218181     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0921-8181(00)00039-4     Document Type: Article

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