Geomorphological Evidence of Holocene Climatic Change from Northwest Ellesmere Island, Canadian High Arctic

Datos Bibliográficos

ID12265373
AutoresDavid J A Evans (0000-0002-1840-2513, Department of Geography and Topographic Science, University of Glasgow, Glasgow G12 8QQ, UK; Department of Geography, University of Alberta, Edmonton, Alberta T6G 2H4, Canada, autor de correspondencia), John England (Department of Geography and Topographic Science, University of Glasgow, Glasgow G12 8QQ, UK; Department of Geography, University of Alberta, Edmonton, Alberta T6G 2H4, Canada)
Año1992
Volumen2
Número2
Páginas148-158
Fecha de publicación1992-07-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaThe Holocene (JOURNAL)
Identificadores de la revistaISSN: 0959-6836 • E-ISSN: 1477-0911
EditorialSAGE Publishing (PUBLISHER • US)
DOI10.1177/095968369200200206
OpenAlexW1558273432
IdiomaEN
Citas recibidas3
Referencias citadas48

Proxy data from the northern coast of Ellesmere Island are used to reconstruct Holocene palaeoclimate and appear to corroborate the ice core record from the Canadian and Greenland high arctic despite some regional variation. Geomorphological evidence indicates that deglaciation was associated with a marked climatic amelioration in the late Pleistocene/early Holocene (≥10 ka BP). This contrasts with glaciers on the south side of Grant Land Mountains which started to retreat at 7.5 ka BP perhaps due to significant differences in glacioclimatic regime and the influence of the Arctic Ocean. Indicators of sea ice conditions on northern Ellesmere Island suggest that the early Holocene was a period of considerable open water. Radiocarbon dates on driftwood collected from behind the north coast ice shelves suggest that the ice shelves formed during a mid-Holocene climatic deterioration. Geomorphic evidence shows that the ice shelves are presently breaking up and melting in response to recent warming. Glaciers have responded to Holocene climate change at varying rates which are related to drainage basin size. Many large glaciers are still advancing in response to the mid-Holocene climatic deterioration. Some glaciers display evidence of dual advances which may reflect mid-Holocene and ‘Little Ice Age’ accumulation. Other evidence of ‘Little Ice Age’ cold and recent warmth is perennial snowbank retreat and fluvially eroded ice wedge polygons near sea level. Different cryogenic systems on northern Ellesmere Island have responded to Holocene climate change at various rates: 10 3 a for glaciers with drainage basin areas >5 km 2 ; 10 2 a for ice shelves and glaciers <5 km 2 ; and 10 1 a for sea ice

Arctic · Climate change · Cryosphere · Deglaciation · Geography · Glacier · Holocene · Holocene climatic optimum · Ice core · Ice sheet · Physical geography · Sea ice · Climate change and permafrost · Cryospheric studies and observations · Geology and Paleoclimatology Research · Geology · Oceanography · Paleontology