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Vancouver microclimate case study

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in detailed case study for CIE a-level core geography. has everything you need to know about each case study in detail

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  • May 29, 2019
  • 4
  • 2018/2019
  • Class notes
  • Unknown
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Case study: candidates must study an urban area which shows the effects of human activity
on climate: temperature (heat island), humidity, precipitation and winds.

Vancouver heat island and micro climates

- Vancouver is Canadas third largest city.


- it is open to the sea but backed by mountain broken by the valley of the Fraser river,
which enters to the eat of the city

heat island

 on sunny summer days a surface temperature traverse across the city shows a
marked heat island

 the sea has the lowest temperature, followed by the river.

 Stanley park also has relatively cool temperatures, similar to those in the rural
farmland of the Fraser valley.

 The international airport records higher temperature than the well-vegetated
Stanley park because of the terminal buildings and runways.

 Temperatures are higher in the suburbs of west Vancouver and surrey

 But the ‘dome’ of the heat island is centred on the downtown (CBD) area

 This is due to the high density of skyscrapers

 Temperatures near the coast can be 5-10C cooler due to the sea breeze in the
summer

 Whereas the inland areas are about 2C cooler in winter

 Steep rise in temperature at the edge of the built-up area

 Temperatures increase gradually till it peaks at the CBD

 All larger urban areas have earlier springs, later autumns and fewer frosts than the
nearby rural areas

 Brick, concreate and dark tarmac surfaces have a large specific heat capacity and low
albedos

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