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Sign on the Trans-Canada Highway near Winnipeg, marking the longitude centre of Canada. The rural village of Taché, Mantioba, east of Winnipeg on the Trans-Canada Highway, has a sign at 96°48'35"W that proclaims it the longitudinal centre of Canada. [1] The sign was upgraded with the opening of Centre of Canada Park in 2017. [2]
The term originally derives from the early fourteenth century sense of trade (in late Middle English) still often meaning "path" or "track". [2] The Portuguese recognized the importance of the trade winds (then the volta do mar, meaning in Portuguese "turn of the sea" but also "return from the sea") in navigation in both the north and south Atlantic Ocean as early as the 15th century. [3]
Two generic types of wave turbulence should be distinguished: statistical wave turbulence (SWT) and discrete wave turbulence (DWT). In SWT theory exact and quasi-resonances are omitted, which allows using some statistical assumptions and describing the wave system by kinetic equations and their stationary solutions – the approach developed by Vladimir E. Zakharov.
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.
Established in 1987, the Center for Turbulence Research is devoted to fundamental studies of turbulent flows. The main elements of the Center are a research fellows program, a biennial summer program, seminars and conferences. [2] CTR is known for fundamental studies in turbulent flows along with large scale numerical investigations. [3] [4] [5]
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 ...
Like trade winds and unlike the westerlies, these prevailing winds blow from the east to the west, and are often weak and irregular. [15] Due to the low sun angle, cold air builds up and subsides at the pole creating surface high-pressure areas, forcing an outflow of air toward the equator; [16] that outflow is deflected westward by the ...