Abstract
The transient and stationary flow fields produced when initial zonal solid body rotation currents flow over topography is studied in spherical barotropic models for eastward and westward flow directions and with variable and constant Coriolis parameters (f). Fully nonlinear analytical solutions are obtained using the methods of equilibrium statistical mechanics and are compared with linearized solutions and with the qualitative results of previous laboratory and numerical experiments.-from Author
| Original language | English |
|---|---|
| Pages (from-to) | 2477-2489 |
| Number of pages | 13 |
| Journal | Journal of the Atmosperhic Sciences |
| Volume | 39 |
| Issue number | 11 |
| Publication status | Published - 1982 |
| Externally published | Yes |
Cite this
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Eastward and westward flows over topography in nonlinear and linear barotropic models. / Frederiksen, J. S.
In: Journal of the Atmosperhic Sciences, Vol. 39, No. 11, 1982, p. 2477-2489.Research output: Contribution to journal › Article › Other
TY - JOUR
T1 - Eastward and westward flows over topography in nonlinear and linear barotropic models.
AU - Frederiksen, J. S.
PY - 1982
Y1 - 1982
N2 - The transient and stationary flow fields produced when initial zonal solid body rotation currents flow over topography is studied in spherical barotropic models for eastward and westward flow directions and with variable and constant Coriolis parameters (f). Fully nonlinear analytical solutions are obtained using the methods of equilibrium statistical mechanics and are compared with linearized solutions and with the qualitative results of previous laboratory and numerical experiments.-from Author
AB - The transient and stationary flow fields produced when initial zonal solid body rotation currents flow over topography is studied in spherical barotropic models for eastward and westward flow directions and with variable and constant Coriolis parameters (f). Fully nonlinear analytical solutions are obtained using the methods of equilibrium statistical mechanics and are compared with linearized solutions and with the qualitative results of previous laboratory and numerical experiments.-from Author
UR - http://www.scopus.com/inward/record.url?scp=0020330865&partnerID=8YFLogxK
M3 - Article
VL - 39
SP - 2477
EP - 2489
JO - Journal of the Atmosperhic Sciences
JF - Journal of the Atmosperhic Sciences
SN - 0022-4928
IS - 11
ER -