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The Geography and Climate of North America

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Title: The Geography and Climate of North America


1
The Geography and Climate of North America
2
Orography
  • The Cordillera, extensive system of mountain
    ranges stretching from Alaska , through British
    Columbia, Sierra Nevada, the Coast and Cascade
    ranges, and the Rocky Mountains and the Sierra
    Madre in Mexico.

3
The Climates of North America ( Based on Bryson
and Hare, 1974)
  • The dominant geographic features of N. America
    are the high Cordillera and the eastern Lowlands
  • The Cordillera is a most significant obstacle to
    the zonal westerly and to the easterly trade
    winds
  • The plains allow unobstructed path to great
    meridional excursions of both Arctic and Tropical
    air masses
  • The Cordillera consists largely of a 1.5-2 km
    plateau with superimposed mountain ranges

4
Transport Pathways
  • wegwegweg
  • Low level westerly winds impinging on the
    Cordillera barrier are mostly deflected, some
    pass through to the Plains
  • At about 500 N the low-level westerly zonal flow
    divides into northerly and southerly branches
    along the western slopes.
  • There are three main routes for the low-level
    westerlies to cross the Cordillera the most
    notable is the Columbia-Snake-Wyoming Channel.
  • In Mexico, the southward deflected westerlies
    usually do not cross the Sierras.
  • Over the Gulf of Mexico, the low level easterly
    the trade winds are usually deflected northward.
  • South of the Yucatan, the trade winds cross the
    continent and turn southward.

5
Features of Air Flow over North America
  • North America is under the influence of Pacific,
    Arctic and Tropical air masses.
  • Between 300-500 the the strong westerlies and a
    more broken mountain barrier allows maximum
    eastward transit of Pacific air.
  • This jet of westerly flow penetrating NAM at
    mid-latitudes entrains and mixes with air from
    the Arctic and the tropics.
  • This unique distribution of land, sea and
    mountains produces a highly variable weather
    From one day to another, mild, sunny air from the
    Rocky Mountains may replace moist, warm, cloudy
    tropical air and then give way to cold Arctic
    air.

6
Seasonal Air Flowover North America
January
April
  • NAVAIR, 1966

October
July
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