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Contemporary Urban Environments

The Urban Heat Island and Urban Precipitation

  • 3 things to know
  • Component 2

Overview

Recall questions on the urban heat island and its causes in dark surfaces, reduced vegetation, anthropogenic heat and urban canyons, when it is strongest, and on urban precipitation, condensation nuclei, thunderstorms, reduced radiation fog and historic smog.

What you need to know

Answer each one before you reveal it.

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Key term

What is the urban heat island effect?

Key term

How does urban canyon geometry affect nocturnal temperatures?

Key term

Explain how the urban heat island effect promotes increased precipitation over and downwind of cities.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is the urban heat island effect?

    Model answer

    The phenomenon where urban areas experience higher temperatures than surrounding rural areas.

  2. 2

    How do dark surfaces such as asphalt and concrete contribute to the urban heat island effect?

    Model answer

    They absorb solar radiation during the day and re-radiate it as heat, raising urban temperatures.

  3. 3

    Why does reduced vegetation in cities contribute to higher temperatures?

    Model answer

    Less vegetation means decreased evapotranspiration, which limits the natural cooling effect that plants provide.

  4. 4

    What is anthropogenic heat and what are its main urban sources?

    Model answer

    Heat released directly by human activities, including buildings, vehicles, industry and air conditioning systems.

  5. 5

    How does urban canyon geometry affect nocturnal temperatures?

    Model answer

    Tall buildings trap longwave radiation between them, reducing heat loss and maintaining higher temperatures at night.

  6. 6

    At what time of day is the urban heat island effect most pronounced, and why?

    Model answer

    At night, because rural areas cool more rapidly than urban areas which retain absorbed heat.

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