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Geography of    Precipitation
Western Canada
Precipitation

• The amount of precipitation a location receives
  depends on its distance from the sea and the
  prevailing winds
• Precipitation = drizzle, showers, heavy rain, hail, or
  snow — all have an impact on the location they fall
• Western Canada experience three types:
  orographic, convectional, and frontal
Orographic
Precipitation
Orographic Precipitation

• The prevailing winds blow moist air onshore
• As the air hits higher land, the air is forced to rise
• When air rises it begins to cool
• When it can no longer hold all its water; it starts to
  condense and form clouds
• Orographic = affected by mountains
Convectional
Precipitation
Convectional Precipitation

• Water in the ocean and lakes is warmed by the sun
• The air above becomes heated
• This makes the air less dense, so it rises; as it rises it
  cools
• Cool air can not hold as much water vapour =
  condensation occurs, gradually becoming clouds
Frontal
Precipitation
Frontal Precipitation

• Two air masses of warm and cold air meet, causing
  a front
• When they meet, the less dense, warm air is forced
  above the denser, heavier cold air
• When air can no longer hold its water, clouds form

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Precipitation

  • 1. Geography of Precipitation Western Canada
  • 2. Precipitation • The amount of precipitation a location receives depends on its distance from the sea and the prevailing winds • Precipitation = drizzle, showers, heavy rain, hail, or snow — all have an impact on the location they fall • Western Canada experience three types: orographic, convectional, and frontal
  • 4. Orographic Precipitation • The prevailing winds blow moist air onshore • As the air hits higher land, the air is forced to rise • When air rises it begins to cool • When it can no longer hold all its water; it starts to condense and form clouds • Orographic = affected by mountains
  • 6. Convectional Precipitation • Water in the ocean and lakes is warmed by the sun • The air above becomes heated • This makes the air less dense, so it rises; as it rises it cools • Cool air can not hold as much water vapour = condensation occurs, gradually becoming clouds
  • 8. Frontal Precipitation • Two air masses of warm and cold air meet, causing a front • When they meet, the less dense, warm air is forced above the denser, heavier cold air • When air can no longer hold its water, clouds form