Urban boundary layer: Difference between revisions
From Glossary of Meteorology
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|Meaning=The [[internal boundary layer]] formed when air flows over a city. | |||
|Explanation=It is a [[mesoscale]] phenomenon, the characteristics of which are affected by the nature of the urban surface. When a new rural [[boundary layer]] downwind of the city forms at the surface, the urban boundary layer is isolated aloft and is then called the urban plume. <br/>''Compare'' [[urban heat island|urban heat island]], [[urban canopy layer]]. | |||
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Latest revision as of 03:41, 27 March 2024
The internal boundary layer formed when air flows over a city.
It is a mesoscale phenomenon, the characteristics of which are affected by the nature of the urban surface. When a new rural boundary layer downwind of the city forms at the surface, the urban boundary layer is isolated aloft and is then called the urban plume.
Compare urban heat island, urban canopy layer.