A Winter Season Synoptic Climatology of Alaska: 1956-1986

An objective, descriptive study of Alaska's winter climate is undertaken to identify regional monthly mean surface temperature and precipitation variability during the thirty-year period from 1956-57 to 1985-86. Ten basic anomaly 700-mb height patterns are described in terms of frequency of occ...

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Bibliographic Details
Main Author: Milkovich, Mary F.
Other Authors: ALASKA UNIV FAIRBANKS INST OF MARINE SCIENCE
Format: Text
Language:English
Published: 1992
Subjects:
Meteorology
*CLIMATE
*SYNOPTIC METEOROLOGY
ALASKA
ANOMALIES
PATTERNS
PRECIPITATION
RECORDS
SURFACE TEMPERATURE
SURFACES
TEMPERATURE
VARIABLES
WINTER
GREENHOUSE EFFECT
ENVIRONMENTAL IMPACT
*Global climate change
Component Reports
*Climate variability
Arctic
Fairbanks
Gulf of Alaska
Climate change
Alaska
Online Access:http://www.dtic.mil/docs/citations/ADP007289
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADP007289
Description
Summary:An objective, descriptive study of Alaska's winter climate is undertaken to identify regional monthly mean surface temperature and precipitation variability during the thirty-year period from 1956-57 to 1985-86. Ten basic anomaly 700-mb height patterns are described in terms of frequency of occurrence and possible associations with the surface climate variability observed in the nine NOAA land-based climate divisions of Alaska and the Gulf of Alaska (tenth division). Results indicate a cool, dry period from 1964-1976. Anomaly height patterns occurring during this period were predominantly characterized by northerly/northwesterly flow from the High Arctic or northeasterly flow from the Canadian Interior. The period from 1956-1962 was generally warm, and the most frequently occurring anomaly height patterns were characterized by southerly flow. The period following 1977 is the most variable of the thirty-year record. This period also includes some of the warmest temperatures seen in the records. Cold anomaly height patterns are interspersed among the slightly more frequent warm anomaly height patterns from 1977-1986. Overall seasonal-scale linear (best-fit approximations) trends appear to indicate a warmer, drier shift in the Interior climate and a warmer, wetter shift in the southern coastal climate. This article is from 'Proceedings of the International Conference on the Role of the Polar Regions in Global Change Held in Fairbanks, Alaska on 11-15 June 1990. Volume 1', AD-A253 027, p210-219. See also Volume 2, AD-A253 028.

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