Contents

  1. BARBI
  2. Source Code
  3. References

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.

barbi.jpg

Streamfunction in Sv in steady state in a simulation of the BARBI model with N=0 1/s (a), a simulation with a flat bottom (b), and the standard model simulation with topographic variations and stratification (c). Also shown are isobaths (lines).

Source Code

BARBI source code

References

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

IfmWiki: TO/barbi (last edited 2011-10-11 12:46:15 by anonymous)