Unbalanced frontogenesis with constant potential vorticity
The numerical model of Williams et al. (1992) is used to study frontogenesis from unbalanced initial conditions. The dependent variables are assumed to be independent of y. The hydrostatic Boussinesq primitive equations are used with no diffusion of heat or momentum. The model is bounded at the top...
Main Author: | Neves, Alberto P. C. |
---|---|
Other Authors: | Roger T. Williams |
Language: | en_US |
Published: |
Monterey, California. Naval Postgraduate School
2013
|
Online Access: | http://hdl.handle.net/10945/32024 |
Similar Items
-
Mid-tropospheric frontogenesis and potential vorticity behavior,
by: Bosart, Lance F
Published: (2010) -
Frontogenesis
by: Heckley, W. A.
Published: (1980) -
Maritime frontogenesis.
by: McDougall, Catherine M.
Published: (2012) -
Atmospheric frontogenesis
by: Hoskins, B. J.
Published: (1970) -
Frontogenesis at Estuarine Junctions
by: Corlett, William Bryce, et al.
Published: (2020)