Answer :
Final answer:
Conduction, convection, and radiation all play roles in transferring heat within a city. Conduction involves direct heat transfer between contacting objects, convection moves heat through the air, and radiation allows sunlight to warm objects. All three contribute to the city’s temperature and weather patterns.
Explanation:
Heat is transferred by conduction, convection, and radiation. Conduction is the transfer of heat between objects in direct contact, such as from the pavement to your shoe on a hot day. Convection is the heat transfer by the movement of mass, this often happens when hot air rises from a city's surfaces. An example in a city context would be warm air rising from heated buildings and surfaces, creating a mini weather system. Radiation is the transfer of heat by electromagnetic waves, such as when sunlight warms up objects in the city. This means that radiation can influence both indoor and outdoor temperatures.
In reality, all three mechanisms of heat transfer conduction, convection, and radiation work concurrently and play a significant role in determining terrestrial weather patterns and microclimate of the city. Particularly in a city, the balance of these processes would determine whether it becomes a 'heat island' - an urban area that is significantly warmer than its surrounding rural areas due to human activities.
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