Observational evidence of recent change in the northern high-latitude environment

Serreze et al present an overview of accounts from different disciplines that document recent change in the northern high-latitude environment. These accounts paint a reasonably coherent picture of climatic change, though their interpretation as signals of enhanced greenhouse warming is debatable.

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Veröffentlicht in:	Climatic change 2000-07, Vol.46 (1-2), p.159-207
Hauptverfasser:	SERREZE, M. C, WALSH, J. E, CHAPIN, F. S, OSTERKAMP, T, DYURGEROV, M, ROMANOVSKY, V, OECHEL, W. C, MORISON, J, ZHANG, T, BARRY, R. G
Format:	Artikel
Sprache:	eng
Schlagworte:	20th century Alaska anthropogenic activities Anthropogenic factors Arctic glaciers Arctic Ocean Arctic Oscillation Arctic region Atmospheric circulation Autumn Boreal ecosystems Brackish Canada Carbon dioxide Climate change Climatology. Bioclimatology. Climate change Continents Earth, ocean, space El Nino Environmental monitoring Exact sciences and technology External geophysics Freshwater General circulation models Glaciers Greenhouse effect greenhouses Human influences Ice Land area Latitude Marine Meteorology Northern Hemisphere Oceans Oscillations Paleoclimate paleoclimatology Permafrost Plant growth Precipitation Russia Sea ice shrubs Snow Snow cover snowpack Southern Oscillation spring Temperature Time series treeline Trends Tundra Winter Winter temperatures
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Beschreibung
Zusammenfassung:	Serreze et al present an overview of accounts from different disciplines that document recent change in the northern high-latitude environment. These accounts paint a reasonably coherent picture of climatic change, though their interpretation as signals of enhanced greenhouse warming is debatable.
ISSN:	0165-0009 1573-1480
DOI:	10.1023/a:1005504031923