REFERENCES
associated with the circulation patterns shown in figure 11. During winter the very strong ridge and northerly direction of the height arionialy (fig. 11A) favored repeated, strong outbreaks of Arctic air masses. In spring (fig. 11B) heights were below nornial in western Canada and there was a troug...
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.2677 http://docs.lib.noaa.gov/rescue/mwr/091/mwr-091-08-0410.pdf |