Download Climate and Weather - Campbell`s Web Soup

Survey
yes no Was this document useful for you?
   Thank you for your participation!

* Your assessment is very important for improving the work of artificial intelligence, which forms the content of this project

Document related concepts
no text concepts found
Transcript
Climate and Weather
Climate Controls and Precipitation
Climates of Canada

Continental Climate


the climate of a continent’s interior
it is a climate of temperature extremes and
low precipitation
Maritime Climate


a coastal climate, usually referring to the
West Coast
it is a climate of mild temperatures and high
precipitation
Latitude & Altitude
 Latitude

the higher the latitude the lower the average
annual temperature and the greater annual
temperature range
Altitude

the higher the altitude, the lower the
temperature
Distance from Sea
 Because
land and water heat and cool at
different rates, a large land mass such as
western Canada can swing between
temperature extremes.

maritime vs. continental climates
Ocean Currents
 Ocean
currents affect the temperature of
the land by warming or heating the air
blowing over them.
 Warm
air can absorb more water than cold
air. Hence, the west coast enjoys a mild,
wet climate.
Ocean Currents
Mountain Barriers
 If
mountain ranges lie across the path of
prevailing winds, they have an affect on
temperature, cloudiness and precipitation
 The
heaviest rains of Canada fall on the
western slopes of the coastal and interior
mountains of British Columbia
Types of Precipitation
Orographic Precipitation
A more moist climate usually prevails on
the windward side of a mountain than on
the leeward (downwind) side.
Moisture is removed by orographic lift,
leaving drier air on the descending
(generally warming), leeward side where a
rain shadow is observed.[
Orographic Precipitation
Convectional Precipitation
 Associated
with hot climates
 Is
brought about by rising and abrupt
cooling of air that has been warmed by
extreme heat on the ground surface
 In
Canada, convectional rainfall is most
common on the Prairies during the
summer
Convectional Precipitation
Frontal Precipitation
 Takes
place at the boundary, or front,
between a mass of warm air from the
tropics and a mass of cold air from the
poles.
 Water
vapour in the warm air is chilled and
condenses to form clouds and rain.
Frontal Precipitation
http://www.youtube.com/watch?v=Z5E3P_XuV6E
Climate Graphs
Related documents