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| 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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| 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.
Source Code
References
[[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]]