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{{attachment:barbi.jpg}} Streamfunction in Sv in steady state in a simulation of the BARBI model (left), a simulation with a flat bottom (middle), and the standard model simulation with topographic variations and stratification. Also shown are isobaths (lines). |
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| [[http://journals.ametsoc.org/doi/abs/10.1175/1520-0485(2003)033<2719:ASGCMF>2.0.CO;2|Olbers D., C. Eden, 2003: A simplified General Circulation Model for a Baroclinic Ocean with Topography. Part I: Theory, Waves and Wind-Driven Circulations. ''J. Phys. Oceanogr.'', '''33''', 2719-2737]] | |
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| [http://journals.ametsoc.org/doi/abs/10.1175/1520-0485(2003)033%3C2719%3AASGCMF%3E2.0.CO%3B2|Olbers D., C. Eden, 2003: A simplified General Circulation Model for a Baroclinic Ocean with Topography. Part I: Theory, Waves and Wind-Driven Circulations. ''J. Phys. Oceanogr.'', '''33''', 2719-2737] Eden, C. and D. Olbers (2009): Why western boundary currents are diffusive: A link between bottom pressure torque and bolus velocity. ''Ocean Modeling'', doi:10.1016/j.ocemod.2009.07.003 |
[[http://www.sciencedirect.com/science/article/pii/S1463500309001437|Eden, C. and D. Olbers (2009): Why western boundary currents are diffusive: A link between bottom pressure torque and bolus velocity. ''Ocean Modeling'', doi:10.1016/j.ocemod.2009.07.003]] |
Contents
BARBI
BARBI is an acronym for BARotropic Baroclinic Interaction. It is a model with simplified circulation dynamics based on the vertically averaged equations of motion for a baroclinic ocean with topography (Olbers and Eden, 2002). The source code of a numerical implementation is provided. A better (finite element) numerical implementation was developed by Sergey Danilov, AWI, Bremerhaven.
Streamfunction in Sv in steady state in a simulation of the BARBI model (left), a simulation with a flat bottom (middle), and the standard model simulation with topographic variations and stratification. Also shown are isobaths (lines).
Source Code