Temperatures @specific sites

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Type of surfaces and distance from the sea

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9 Terms

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Man-made Materials

  • Densely built-up area of buildings and road networks

  • asphalt, concrete etc.

  • Absorbs and releases heat from sunlight quickly to the air above

  • Higher temperatures in the day where the roads are

  • Heat absorbed is also emitted at night

  • Increasing temperature

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Man-made Heat Sources

  • Vehicles

    • Release exhaust fumes (CO2) → greenhouse gas

    • Trap heat

  • Air-conditioning unit

    • Transfers warmth from inside buildings to the air outside with electricity

    • Generates and vents out waste heat 

Thus, higher temps in sites such as urban locations (cities).

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Water Bodies

  • ponds, reservoir, sea, river etc.

  • Poor conductivity so

  • Release heat slower than land in the day

  • Air above pond is cooler (hence decreases nearby temp)

  • Water heats and evaporates into water vapour

  • Evaporative cooling

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Difference in Colour of Earth’s Surfaces

  • Dark colour (asphalt)

    • Absorb more heat

    • Radiate more heat

    • More heating of air above

    • Higher temps

  • Light colour (ice and snow)

    • Reflects more heat

    • Radiate less heat

    • Less heating of air above

    • Lower temps

Urban areas have more dark surfaces experience higher temps that sites w/ veg and water bodies  

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The Maritime Effect

The sea has a moderating influence on temp of coastal locations because it absorbs and loses heat at a slower rate than land. 

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Maritime effect during summer

  • sea absorbs heat slower

  • Land absorbs heat quickly

  • Sea is cooler than land

  • Onshore wind blows to land lowers temp 

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Maritime effect during winter

  • sea loses heat slowly

  • Land loses heat rapidly

  • Sea is warmer than land

  • Warm wind blows towards land increases temp

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Continental effect during summer

  • inland/interior of the continent

  • Air over land is warmer that air over sea 

  • As land heats more quickly

  • No moderating impact of cool winds format he sea

  • HOT SUMMERSS instead of warm

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Continental Effect in winter

  • air over land is cooler

  • Land cools more quickly

  • No moderating impact

  • Temp remains low

  • Cold winters instead of cool