Behavior of the northwestern part of the Fennoscandian Ice Sheet during the Last Glacial Maximum - a response to external forcing

Quaternary Science Reviews

Volumn 29, Issue 17-18, 2010, Pages 2224-2237

  Rorvik K L ^a   Laberg, J S ^a   Hald, M ^a   Ravna, E K ^a   Vorren, T O ^a  

^a UNIVERSITY OF TROMSØ   (Norway)

Author keywords

[No Author keywords available]

Indexed keywords

ADJACENT SURFACES; CONTINENTAL SLOPE; DATA POINTS; DEGLACIATIONS; ECLOGITES; EXTERNAL FORCING; HIGH RESOLUTION; HOLOCENES; ICE SHEET; ICE STREAMS; INCREASED TEMPERATURE; LAST GLACIAL MAXIMUM; MONOCRYSTALLINE; RESPONSE TO EXTERNAL FORCING; SEA SURFACE TEMPERATURES; SEDIMENT CORE; SOLAR VARIATIONS; TIME CYCLES; TIME INTERVAL; TIME STEP; WATER MASS;

ATMOSPHERIC TEMPERATURE; CRYSTALLINE MATERIALS; CRYSTALLINE ROCKS; DEBRIS; GLACIAL GEOLOGY; HYDRAULICS; METAMORPHIC ROCKS; OCEANOGRAPHY; SEA ICE; SEDIMENTARY ROCKS; SEDIMENTOLOGY; SURFACE WATERS;

GLACIERS;

CONTINENTAL SLOPE; DEGLACIATION; GLACIAL DEPOSIT; ICE SHEET; ICEBERG; LAST GLACIAL MAXIMUM; PALEOENVIRONMENT; SEDIMENT CORE; SURFACE WATER;

FENNOSCANDIA;

EID: 77955267217     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2010.05.022     Document Type: Article

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