Abstract
A novel approach to the modeling of tornado-like vortexgenesis has been developed and is used to articulate the sequence of events that leads to tornadogenesis. The "pseudostorm' is an idealized thunderstorm representation and emulates the storm-relative flow, into an updraft, of the horizontal streamwise vorticity that is baroclinically generated in cool arid outflow. By not explicitly simulating the morphology of a tornadic thunderstorm, but instead concentrating on the development of low-level rotation and tornado-scale vortices, the authors are able to transcend many of the experimental limitations encountered by cloud modelers. -from Authors
Original language | English (US) |
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Pages (from-to) | 3757-3778 |
Number of pages | 22 |
Journal | Journal of the Atmospheric Sciences |
Volume | 52 |
Issue number | 21 |
DOIs | |
State | Published - 1995 |
Externally published | Yes |
ASJC Scopus subject areas
- Atmospheric Science