Document Type
Article
Publication Title
Journal of Glaciology
Rights and Access Note
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Publication Date
2010
First Page
715
Last Page
722
Issue Number
198
Volume Number
56
Abstract/ Summary
Samples were collected from a snow pit and shallow urn core near Kahiltna Pass (2970 m a.s.l.), Denali National Park, Alaska, USA, in May 2008. The record spans autumn 2003 to spring 2008 and reveals clusters of ice layers interpreted as summertime intervals of above-freezing temperatures. High correlation coefficients (0.75-1.00) between annual ice-layer thickness and regional summertime station temperatures for 4 years (n=4) indicate ice-layer thickness is a good proxy for mean and extreme summertime temperatures across Alaska, at least over the short period of record. A Rex-block (aka high-over-low) pattern, a downstream trough over Hudson Bay, Canada, and an upstream trough over eastern Siberia occurred during the three melting events that lasted at least 2 weeks. About half of all shorter melting events were associated with a cut-off low traversing the Gulf of Alaska. We hypothesize that a surface-to-bedrock core extracted from this location would provide a high-quality record of summer temperature and atmospheric blocking variability for the last several hundred years.
Repository Citation
Kelsey, Eric P.; Wake, Cameron P.; Kreutz, Karl J.; and Osterberg, Erich, "Ice Layers as an Indicator of Summer Warmth and Atmospheric Blocking in Alaska" (2010). Earth Science Faculty Scholarship. 48.
https://digitalcommons.library.umaine.edu/ers_facpub/48
Citation/Publisher Attribution
Kelsey, EP, Wake, CP, Kreutz, K, and Osterberg, E, 2010, Ice Layers as an Indicator of Summer Warmth and Atmospheric Blocking in Alaska: Journal of Glaciology, v. 56, p. 715-722. Available on publisher's site at: http://www.ingentaconnect.com/content/igsoc/jog/2010/00000056/00000198/art00015
Publisher Statement
© Copyright 2010 by the International Glaciological Society
Version
publisher's version of the published document