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5148512
Precipitation in Urban Microclimates
Descripción
Urban microclimates
Sin etiquetas
geography
as
a2
Mapa Mental por
orlaamy10
, actualizado hace más de 1 año
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Creado por
orlaamy10
hace más de 8 años
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Resumen del Recurso
Precipitation in Urban Microclimates
Distribution of rainfall over a town or city is very much influenced by topography
Largest values occurring over the more hilly regions
Lowest values in more low— lying areas.
Higher levels of rainfall in urban areas than surrounding counrtyside
Rain is more intense
Why?
The Urban Heat Island effect means that the air in urban areas is warm, which can hold more water. The warm moist air rises - convectional uplift
As it rises it cools, and water vapour condenses and it rains - convectional rainfall
Urban areas generate large amounts of dust and pollution. These particles floating in the air act as condensation nuclei.
Condensation nuclei cause water to condense around them
This encourage clouds to form, rather than allowing the warm, moist air to disperse.
A mixture of building heights causes air turbulence, which promotes increased vertical motion
Higher number of thunderstorms
Likely in late afternoon and evenings in the summer months
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