Page 250 - Geosystems An Introduction to Physical Geography 4th Canadian Edition
P. 250
214 part II The Water, Weather, and Climate Systems
Egg Island, British Columbia 100 Mile House, British Columbia
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Mt. Calgary Fidelity International
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Glacier National Park, Mount Fidelity, British Columbia
▲Figure 8.7 Orographic patterns in British Columbia and Alberta. Four stations in British Columbia and Alberta provide examples of oro- graphic effects of windward precipitation and leeward rain shadows. Isohyets (lines connecting points of equal precipitation) that form the boundaries between the colours on the map indicate precipitation (in mm). [Data courtesy of Meteorological Service of Canada, and map by Jessica Mueller and Pam Schaus.]
air pressure rises in response to the cooler, denser air; cloud cover breaks and clears.
On weather maps, such as the example in Critical Thinking 8.1, page 222, a cold front is depicted as a line with triangular spikes that point in the direction of fron- tal movement along an advancing air mass. The particu- lar shape and size of the North American landmass and its latitudinal position present conditions where cP and
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mT air masses are best developed and have the most di- rect access to each other. The resulting contrast can lead to dramatic weather, particularly in late spring, with siz- able temperature differences from one side of a cold front to the other.
A fast-advancing cold front can cause violent lift- ing, creating a zone known as a squall line right along or slightly ahead of the front. (A squall is a sudden episode of
Coast Mountains Mt. Waddington
Interior Plain Rocky Mountains Prairies
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