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Tellus A: Dynamic Meteorology and Oceanography Volume 48, 1996 - Issue 3

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Original Articles

An inconsistency between two classical models of the ocean buoyancy driven circulation

David N. StraubDepartment of Atmospheric and Oceanic Sciences and Centre for Climate and Global Change Research, McGill University, 805 Rue Sherbrooke O., Montreal, QuebecH3A 2K6, Canada;Also affiliated with Centre de Recherche en Calcul Appliqué, 5160 boul. Decarie, bureau 400, Montreal, Quebec H3X 2H9, Canada.

Pages 477-481 | Received 10 Jul 1995, Accepted 13 Nov 1995, Published online: 15 Dec 2016

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https://doi.org/10.3402/tellusa.v48i3.12073

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Articles from other publishers (5)

Ashwita Chouksey, Alexa Griesel, Manita Chouksey & Carsten Eden. (2022) Changes in Global Ocean Circulation due to Isopycnal Diffusion. Journal of Physical Oceanography 52:9, pages 2219-2235.
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B. B. Cael & Malte F. Jansen. (2020) On freshwater fluxes and the Atlantic meridional overturning circulation. Limnology and Oceanography Letters 5:2, pages 185-192.
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Nils Brüggemann, Carsten Eden & Dirk Olbers. (2011) A Dynamically Consistent Closure for Zonally Averaged Ocean Models. Journal of Physical Oceanography 41:11, pages 2242-2258.
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D. Swingedouw, P. Braconnot, P. Delecluse, E. Guilyardi & O. Marti. (2007) Quantifying the AMOC feedbacks during a 2×CO2 stabilization experiment with land-ice melting. Climate Dynamics 29:5, pages 521-534.
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Richard J. Greatbatch & Jian Lu. (2003) Reconciling the Stommel Box Model with the Stommel–Arons Model: A Possible Role for Southern Hemisphere Wind Forcing?. Journal of Physical Oceanography 33:8, pages 1618-1632.
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