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CMC building viewed from the West CMC building viewed from the South. The Canadian Meteorological Centre (CMC; French: Centre météorologique canadien), located in Dorval, Quebec, is the branch of Environment Canada's Meteorological Service of Canada that is tasked with providing forecast guidance to national and regional prediction centres, and is responsible for running the Global ...
The Meteorological Service of Canada (MSC; French: Service météorologique du Canada – SMC) is a branch of Environment and Climate Change Canada, which primarily provides public meteorological information and weather forecasts and warnings of severe weather and other environmental hazards.
The advent of numerical weather prediction in the early 1960s changed the forecasting system in Canada to one of large regional forecast centres, called "Weather Centrals", with local support offices called "Weather Offices". For the Canadian prairie provinces and the arctic territories, the Prairie Weather Central was established in Winnipeg ...
The Global Environmental Multiscale Model (GEM), often known as the CMC model in North America, is an integrated forecasting and data assimilation system developed in the Recherche en Prévision Numérique (RPN), Meteorological Research Branch (MRB), and the Canadian Meteorological Centre (CMC).
Canada Canadian Meteorological Centre; Environment and Climate Change Canada. Meteorological Service of Canada. Canadian Ice Service; United States: National Center for Atmospheric Research NCAR; National Oceanic and Atmospheric Administration. National Severe Storms Laboratory; National Climatic Data Center; National Weather Service
"The storm track in the West can retreat quickly and center more over the Pacific Northwest and western Canada by March," Pastelok said. "The transition to spring will be near average or faster ...
September 21, 1938: The 1938 New England hurricane tracked into Canada, bringing strong winds to eastern Ontario and southern Quebec. Damage was primarily limited to trees and power lines; structural damage was minimal. This storm, along with Hurricane Hazel in 1954, was one of the few hurricanes to cause hurricane-force winds in Canada's interior.
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