Thursday, 16 June 2005
Riverside (Hyatt Regency Cambridge, MA)
Handout (207.4 kB)
Recent studies of the Canadian climate have indicated significant changes in the observed surface temperature during the past five decades. A strong warming is identified in the western part of Canada while cooling occurs in the north-eastern part of the country, particularly during winter and spring. It is pertinent to determine if related trends also occur in upper levels of the atmosphere. This work presents a preliminary analysis of the trends and variability in temperature at the surface and various standard upper air pressure levels at several locations in Canada.
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