PPT-SO254
Author : giovanna-bartolotta | Published Date : 2017-07-12
Extratropical cyclones View of an extratropical cyclone from above top panel and from the side bottom panel In top panel gray lines are isobars with pressures in
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SO254: Transcript
Extratropical cyclones View of an extratropical cyclone from above top panel and from the side bottom panel In top panel gray lines are isobars with pressures in mb red L indicates the center of the . What is advection?. Advection is the transfer of a property of the air by the wind. There are many things that can be . advected. : temperature, vorticity (relative and planetary), momentum, moisture. Upper-air circulation tied to the 3-cell model. We saw in Lesson 2 that differences in insolation (more in the tropics, less in the polar regions), combined with the Earth’s rotation, drives complex circulation patterns. What is . vorticity. ?. Many meteorological web sites include some form of . vorticity. contours on the 500-mb charts. Why. ? How does having contours of vorticity help a meteorologist understand the atmosphere. Advection is the transfer of a property of the air by the wind. There are many things that can be . advected. : temperature, vorticity (relative and planetary), momentum, moisture. Advection of . “.
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