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H. Glahn, D. Lowry (1972)
The Use of Model Output Statistics (MOS) in Objective Weather ForecastingJournal of Applied Meteorology, 11
M. Serreze, F. Carse, R. Barry, J. Rogers (1997)
Icelandic low cyclone activity : Climatological features, linkages with the NAO, and relationships with recent changes in the Northern Hemisphere circulationJournal of Climate, 10
H. Wexler (1936)
COOLING IN THE LOWER ATMOSPHERE AND THE STRUCTURE OF POLAR CONTINENTAL AIRMonthly Weather Review, 64
A. Proshutinsky, Robert Bourke, Fiona McLaughlin (2002)
The role of the Beaufort Gyre in Arctic climate variability: Seasonal to decadal climate scalesGeophysical Research Letters, 29
F. Bodurtha (1952)
AN INVESTIGATION OF ANTICYCLOGENESIS IN ALASKAJournal of Meteorology, 9
Mads Knudsen, Peter Riisager, Bo Jacobsen, Raimund Muscheler, Ian Snowball, Marit-Solveig Seidenkrantz, M Knudsen, P Riisager, B Jacobsen, R Muscheler, I Snowball, M.-S Seidenkrantz (1989)
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J. Kahl (1990)
Characteristics of the low‐level temperature inversion along the Alaskan Arctic coastInternational Journal of Climatology, 10
J. Overland, J. Adams, N. Bond (1999)
Decadal Variability of the Aleutian Low and Its Relation to High-Latitude Circulation*Journal of Climate, 12
K. Aagaard, E. Carmack (1989)
The role of sea ice and other fresh water in the Arctic circulationJournal of Geophysical Research, 94
G. Wendler, K. Jayaweera (1972)
Some measurements of the development of the surface inversion in Central Alaska during winterpure and applied geophysics, 99
Kalnay (1996)
The NCEP/NCAR 40-Year Reanalysis Project.Bull. Amer. Meteor. Soc., 77
S. Bowling (1986)
Climatology of High-Latitude Air Pollution as Illustrated by Fairbanks and Anchorage, Alaska, 25
M. Alexander, U. Bhatt, J. Walsh, M. Timlin, Jack Miller, James Scott (2004)
The Atmospheric Response to Realistic Arctic Sea Ice Anomalies in an AGCM during Winter.Journal of Climate, 17
(1989)
The role of sea ice and fresh
G. Wendler, P. Nicpon (1975)
Low-Level Temperature Inversions in Fairbanks, Central AlaskaMonthly Weather Review, 103
Yihui Ding, T. Krishnamurti (1987)
Heat Budget of the Siberian High and the Winter MonsoonMonthly Weather Review, 115
B. Hartmann, G. Wendler (2005)
The Significance of the 1976 Pacific Climate Shift in the Climatology of AlaskaJournal of Climate, 18
A. Henry (1897)
CLIMATE OF ALASKAMonthly Weather Review, 25
M. Serreze, R. Barry (2005)
The Arctic climate system
J. Papineau (2001)
Wintertime temperature anomalies in Alaska correlated with ENSO and PDOInternational Journal of Climatology, 21
V. Semenov (2007)
Structure of temperature variability in the high latitudes of the Northern HemisphereIzvestiya, Atmospheric and Oceanic Physics, 43
J. Overland, P. Guest (1991)
The Arctic snow and air temperature budget over sea ice during winterJournal of Geophysical Research, 96
Stroeve (2007)
Arctic sea ice decline: Faster than forecast.Geophys. Res. Lett., 34
During the early winter of 2002 and late winter of 2007, the Alaskan sector of the North Pacific Ocean region experienced record-breaking temperature anomalies. The duration of these episodes was unusually long, with each lasting more than 1 month: 55 days for the warm anomaly of October–December 2002 and 37 days for the cold anomaly of February–March 2007. Temperature departures over each respective period were the largest for the continental climate of interior Alaska (>10°C) and the smallest for the maritime regions of Alaska (<4°C). Mean temperatures over the event periods in 2002 and 2007 easily ranked as the record warmest and coldest, respectively, for many surface observing stations. In addition, heating degree-day anomalies were on the order of 700 units for these periods. Atmospheric circulation patterns at the surface and upper levels for the circum-Arctic proved to be the driver for these persistent events. The 2002 warm anomaly was driven by enhanced southerly advection associated with an unusually strong Aleutian low and a positive Pacific decadal oscillation index, which resulted in a large area of anomalous temperatures in Alaska and northern Canada. The 2007 cold anomaly was driven by a weakening of the circulation pattern in the subpolar Pacific sector and a strengthening of the Siberian high, with the strongest temperature anomalies in Alaska and northwestern Canada.
Monthly Weather Review – American Meteorological Society
Published: Apr 21, 2009
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