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Instability of horizontally and vertically sheared parallel flow

dc.contributor.authorRingerud, Mark A., author
dc.contributor.authorStevens, Duane E., author
dc.contributor.authorCiesielski, Paul E., author
dc.date.accessioned2022-03-23T17:53:40Z
dc.date.available2022-03-23T17:53:40Z
dc.date.issued1989-06
dc.descriptionJune 1989.
dc.descriptionAlso issued as Mark A. Ringerud's thesis (M.S.) -- Colorado State University, 1988.
dc.description.abstractThis study examines the effects of various windshears on the perturbation growths within inertially unstable regions. A primary focus is determining what type of instability is preferred, symmetric or asymmetric, through the development of a two-dimensional model using the primitive equations and a jet with horizontally and vertically sheared flow. A necessary condition for inertial instability is when the basic state potential vorticity, f P < 0. The potential vorticity can be viewed as having two influences, that due to the horizontal wind shear and vertical shear. With this in mind, I examine the relationship between the shears in inertial instability. This study extends previous results where the basic state contained only horizontal shear, u(y). These results, obtained with a shallow water model, showed that asymmetric modes had larger growth rates than symmetric modes. By examining various jet profiles which contained both horizontal and vertical shear, the results in this more general case (i.e., u(y, z) again revealed that asymmetric instabilities are preferred.
dc.description.sponsorshipSponsored by the National Science Foundation under grants ATM-8305759 and ATM-8352205.
dc.format.mediumreports
dc.identifier.urihttps://hdl.handle.net/10217/234569
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991023629869703361
dc.relationQC852 .C6 no. 445
dc.relation.ispartofAtmospheric Science Papers (Blue Books)
dc.relation.ispartofAtmospheric science paper, no. 445
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subject.lcshWind shear
dc.subject.lcshVertical wind shear
dc.subject.lcshDynamic meteorology -- Mathematical models
dc.titleInstability of horizontally and vertically sheared parallel flow
dc.typeText
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