/[MITgcm]/manual/s_examples/plume_on_slope/plume_on_slope.tex
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revision 1.7 by edhill, Sat Apr 8 01:50:50 2006 UTC revision 1.8 by molod, Tue Jun 27 19:08:23 2006 UTC
# Line 28  to radiate transients at the deep water Line 28  to radiate transients at the deep water
28  can also be forced by a dense inflow prescribed on the continental  can also be forced by a dense inflow prescribed on the continental
29  shelf; this configuration is being implemented by the DOME (Dynamics  shelf; this configuration is being implemented by the DOME (Dynamics
30  of Overflow Mixing and Entrainment) collaboration to compare solutions  of Overflow Mixing and Entrainment) collaboration to compare solutions
31  in different models).  in different models). The files for this experiment can be found in
32    the verification directory under tutorial\_plume\_on\_slope.
33    
34  The fluid is initially unstratified.  The surface buoyancy loss $B_0$  The fluid is initially unstratified.  The surface buoyancy loss $B_0$
35  (dimensions of L$^2$T$^{-3}$) over a cross-shelf distance $R$ causes  (dimensions of L$^2$T$^{-3}$) over a cross-shelf distance $R$ causes
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