On the mix-down times of dynamically active potential vorticity filaments

A simple model is used to study the evolution of potential vorticity filaments, viewed in cross-section, subject to steady shear and deformation flows representative of the large-scale atmospheric circulation. It is found that the balanced, ageostrophic circulation induced by the anomalous potential...

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Bibliographic Details
Main Authors: Polvani, Lorenzo M. (Author), Esler Jr, Kenneth P (Contributor), Plumb, Raymond Alan (Contributor)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor), Massachusetts Institute of Technology. Program in Atmospheres, Oceans, and Climate (Contributor)
Format: Article
Language:English
Published: American Geophysical Union (AGU), 2017-05-02T18:24:14Z.
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Online Access:Get fulltext
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100 1 0 |a Polvani, Lorenzo M.  |e author 
100 1 0 |a Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences  |e contributor 
100 1 0 |a Massachusetts Institute of Technology. Program in Atmospheres, Oceans, and Climate  |e contributor 
100 1 0 |a Esler Jr, Kenneth P  |e contributor 
100 1 0 |a Plumb, Raymond Alan  |e contributor 
700 1 0 |a Esler Jr, Kenneth P  |e author 
700 1 0 |a Plumb, Raymond Alan  |e author 
245 0 0 |a On the mix-down times of dynamically active potential vorticity filaments 
260 |b American Geophysical Union (AGU),   |c 2017-05-02T18:24:14Z. 
856 |z Get fulltext  |u http://hdl.handle.net/1721.1/108606 
520 |a A simple model is used to study the evolution of potential vorticity filaments, viewed in cross-section, subject to steady shear and deformation flows representative of the large-scale atmospheric circulation. It is found that the balanced, ageostrophic circulation induced by the anomalous potential vorticity can cause the evolution of a dynamically active filament to differ substantially from that of a dynamically passive filament in a similar background flow. It is suggested that estimates of the mix-down time of material contained in atmospheric filaments need to be corrected to allow for this effect. 
546 |a en_US 
655 7 |a Article 
773 |t Geophysical Research Letters