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Type of surfaces and distance from the sea
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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
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).
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
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
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.
Maritime effect during summer
sea absorbs heat slower
Land absorbs heat quickly
Sea is cooler than land
Onshore wind blows to land lowers temp
Maritime effect during winter
sea loses heat slowly
Land loses heat rapidly
Sea is warmer than land
Warm wind blows towards land increases temp
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
Continental Effect in winter
air over land is cooler
Land cools more quickly
No moderating impact
Temp remains low
Cold winters instead of cool