Thermobaric effect on slantwise convection in cold seawater
References
-
Aagard
, Swift, J. H.and Carmack. Thermohaline circulation in the Arctic Mediterranean Seas. J. Geophys. Res. 90, 4833– 4846. -
Akitomo
. Open-ocean deep convection due to thermobaricity. 1. Scaling argument. J. Geophys. Res. 104, 5225– 5234. -
Akitomo
. Open-ocean deep convection due to thermobaricity. 2. Numerical experiments. J. Geophys. Res. 104, 5225– 5234. -
Allen
, J. S.and Newberger, P. A.. Downwelling circulation on the Oregon Continental Shelf. Part I: response to idealizes forcing. J. Phys. Oceanogr, 2011– 2035. -
Allen
, J. S.and Newberger, P. A.. On symmetric instabilities in oceanic bottom boundary layers. J. Phys. Oceanogr, 1131– 1151. -
Eliassen
and Kleinschmidt. Dynamic Meteorology. In: Hand- buch der Physik (ed S. Flagge). Springer-Verlag, Berlin, 1– 154. -
Emanuel
, K. A.. Inertial instability and mesoscale convective sys-tems. part I: linear theory of inertial instability in rotating viscous fluids. J. Atmos. Sci. 36, 2425– 2449. -
Emanuel
, K. A.. Atmospheric Convection . Oxford University Press, Oxford. -
Finlayson
, B. A.. The Method of Weighted Residuals and Varia-tional Principles with Application in Fluid Mechanics, Heat and Mass Transfer . Academic Press, New York. -
Garwood
Jr. , R., Isakari, and Gallacher. Thermobaric convec-tion. In: The Polar Oceans and Their Role in Shaping the Global Environment, Geophys. Monogr. Ser. 85(eds O. M., R. D.and J. E.), AGU, Washington, D.C., 199– 209. -
Gill
, A. E.. Circulation and bottom water production in the Weddel Sea. Deep-Sea Res. 20, 111– 140. -
Gill
, A. E.. Atmosphere-Ocean Dynamics . Academic Press, New York. -
Hoskins
, B. J.. The role of potential vorticity in symmetric stability and instability. Quart. J. Roy. Meteor. Soc. 100, 480– 482. -
Killworth
, P. D.. Mixing on the Weddel Sea continental slope. Deep-Sea Res. 24, 427– 448. -
Killworth
, P. D.. On “chimney” formations in the ocean., 531– 553. -
Løyning
, T. B.and Weber, J. E.. Thermobaric effects on buoyancy-driven convection in cold seawater.. 102, 27.874– 27.885. -
McDougal
, T. J.. The relative roles of diapycnal and isopycnal mixing on subsurface water mass conversion, J. Phys. Oceanogr, 1577– 1589. -
McDougal
, T. J.. Neutral surfaces. J. Phys. Oceanogr, 1950– 1964. -
McDougal
, T. J.. Thermobaricity, cabbeling and water-mass con-version. J. Geophys. Res. 92, 5448– 5464. -
Ooyama
. On the stability of the baroclinic circular vortex: a sufficient criterion for instability. J. Atmos. Sci. 23, 43– 53. -
Stone
, P. H.. On non-geostrophic baroclinic instability. J. Atmos. Sci. 23, 390– 400. -
Torkildsen
, F.and Haugan, P.M.. Modelling of deep water renewal through cold convective plumes., 1357– 1383. -
Walton
, I. C.. The viscous nonlinear symmetric baroclinic instability of a zonal shear flow. J. Fluid Mech. 68, 757– 768. -
Weber
, J. E.. Symmetric instability of stratified geostrophic flow. Tellus, 176– 185.
DOI: https://doi.org/10.1111/j.1600-0870.2006.00179.x | Journal eISSN: 3035-9554
Language: English
Page range: 385 - 391
Submitted on: May 23, 2005
Accepted on: Nov 24, 2005
Published on: Jan 1, 2006
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 2006 Jan Erik H. Weber, Terje Brinck Løyning, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.