Multiple Zonal Jets in a Differentially Heated Rotating Annulus
A laboratory experiment of multiple baroclinic zonal jets is described, thought to be dynamically similar to flow observed in the Antarctic Circumpolar Current. Differential heating sets the overall temperature difference and drives unstable baroclinic flow, but the circulation is free to determine...
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ftanucanberra:oai:digitalcollections.anu.edu.au:1885/58315 2023-05-15T13:36:32+02:00 Multiple Zonal Jets in a Differentially Heated Rotating Annulus Smith, Carlowen Speer, Kevin G Griffiths, Ross 2015-12-10T22:43:46Z http://hdl.handle.net/1885/58315 unknown American Meteorological Society 0022-3670 http://hdl.handle.net/1885/58315 Journal of Physical Oceanography Journal article 2015 ftanucanberra 2015-12-28T23:30:15Z A laboratory experiment of multiple baroclinic zonal jets is described, thought to be dynamically similar to flow observed in the Antarctic Circumpolar Current. Differential heating sets the overall temperature difference and drives unstable baroclinic flow, but the circulation is free to determine its own structure and local stratification; experiments were run to a stationary state and extend the dynamical regime of previous experiments. Atopographic analog to the planetary β effect is imposed by the gradient of fluid depth with radius supplied by a sloping bottom and a parabolic free surface. New regimes of a low thermal Rossby number (RoT ~ 10-3) and high Taylor number (Ta ~ 1011) are explored such that the deformation radius Lp is much smaller than the annulus gap width L and similar to the Rhines length. Multiple jets emerge in rough proportion to the smallness of the Rhines scale, relatively insensitive to the Taylor number; a regime diagram taking the β effect into account better reflects the emergence of the jets. Eddy momentum fluxes are consistent with an active role in maintaining the jets, and jet development appears to follow the Vallis and Maltrud phenomenology of anisotropic wave-turbulence interaction on a ß plane. Intermittency and episodes of coherent meridional jet migration occur, especially during spinup. Article in Journal/Newspaper Antarc* Antarctic Australian National University: ANU Digital Collections Antarctic The Antarctic |
institution |
Open Polar |
collection |
Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
unknown |
description |
A laboratory experiment of multiple baroclinic zonal jets is described, thought to be dynamically similar to flow observed in the Antarctic Circumpolar Current. Differential heating sets the overall temperature difference and drives unstable baroclinic flow, but the circulation is free to determine its own structure and local stratification; experiments were run to a stationary state and extend the dynamical regime of previous experiments. Atopographic analog to the planetary β effect is imposed by the gradient of fluid depth with radius supplied by a sloping bottom and a parabolic free surface. New regimes of a low thermal Rossby number (RoT ~ 10-3) and high Taylor number (Ta ~ 1011) are explored such that the deformation radius Lp is much smaller than the annulus gap width L and similar to the Rhines length. Multiple jets emerge in rough proportion to the smallness of the Rhines scale, relatively insensitive to the Taylor number; a regime diagram taking the β effect into account better reflects the emergence of the jets. Eddy momentum fluxes are consistent with an active role in maintaining the jets, and jet development appears to follow the Vallis and Maltrud phenomenology of anisotropic wave-turbulence interaction on a ß plane. Intermittency and episodes of coherent meridional jet migration occur, especially during spinup. |
format |
Article in Journal/Newspaper |
author |
Smith, Carlowen Speer, Kevin G Griffiths, Ross |
spellingShingle |
Smith, Carlowen Speer, Kevin G Griffiths, Ross Multiple Zonal Jets in a Differentially Heated Rotating Annulus |
author_facet |
Smith, Carlowen Speer, Kevin G Griffiths, Ross |
author_sort |
Smith, Carlowen |
title |
Multiple Zonal Jets in a Differentially Heated Rotating Annulus |
title_short |
Multiple Zonal Jets in a Differentially Heated Rotating Annulus |
title_full |
Multiple Zonal Jets in a Differentially Heated Rotating Annulus |
title_fullStr |
Multiple Zonal Jets in a Differentially Heated Rotating Annulus |
title_full_unstemmed |
Multiple Zonal Jets in a Differentially Heated Rotating Annulus |
title_sort |
multiple zonal jets in a differentially heated rotating annulus |
publisher |
American Meteorological Society |
publishDate |
2015 |
url |
http://hdl.handle.net/1885/58315 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Journal of Physical Oceanography |
op_relation |
0022-3670 http://hdl.handle.net/1885/58315 |
_version_ |
1766080201211510784 |