Global, regional and local scale factors determining glaciation extent in Eastern Siberia over the last 140,000 years

Quaternary Science Reviews

Volumn 30, Issue 7-8, 2011, Pages 821-831

  Krinner, Gerhard ^a,b   Diekmann, Bernhard ^b   Colleoni, Florence ^a,c   Stauch, Georg ^d  

^a LABORATOIRE DE GLACIOLOGIE ET GÉOPHYSIQUE DE L ENVIRONNEMENT   (France)

^b ALFRED WEGENER INSTITUTE FOR POLAR AND MARINE RESEARCH   (Germany)

^c CENTRO EURO MEDITERRANEO SUI CAMBIAMENTI CLIMATICI   (Italy)

^d RWTH AACHEN UNIVERSITY   (Germany)

Author keywords

Modelling; Mountain glaciations; Paleoclimate; Quaternary; Siberia

Indexed keywords

MODELLING; MOUNTAIN GLACIATIONS; PALEOCLIMATES; QUATERNARY; SIBERIA;

DUST; GLACIERS; GLOBAL WARMING; GREENHOUSE EFFECT; GREENHOUSE GASES; ICE; INCIDENT SOLAR RADIATION; LANDFORMS; MOISTURE; ORBITAL LABORATORIES; VEGETATION;

GLACIAL GEOLOGY;

ATMOSPHERIC GENERAL CIRCULATION MODEL; BOUNDARY CONDITION; ENVIRONMENTAL FACTOR; GLACIATION; GREENHOUSE GAS; ICE SHEET; MASS BALANCE; PALEOCLIMATE; SEA SURFACE; TIMESCALE; WEICHSELIAN;

SIBERIA;

EID: 79952444014     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2011.01.001     Document Type: Article

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