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  Poster Programme - OS15 Small and Meso-Scale Processes and their Impact on the Large Scale

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Convener: Dewar, W.
Co-Convener: Killworth, P.
Co-Sponsorship:


Author in Attendance:

Tuesday, 4 April 2006 13:30 - 15:00
Display Time: Tuesday, 4 April 2006 08:00 -
Tuesday, 4 April 2006 19:30
Poster Area: Halls X/Y

Chairperson: KILLWORTH

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XY0706
EGU06-A-03566;  OS15-1TU3P-0706
Wilson, C. ; Williams, R. G.
When are eddy tracer fluxes directed down gradient?

XY0707
EGU06-A-04068;  OS15-1TU3P-0707
Badin, G.; Williams, R.G.; Roussenov, V.M.
The effect of interior mixing on eddy exchange across a front

XY0708
EGU06-A-05655;  OS15-1TU3P-0708
Mignot, J.; de Boyer Montégut, C.; Lazar, A.; Cravatte, S.
Control of salinity on the mixed layer depth in the world ocean (cancelled)

XY0709
EGU06-A-09489;  OS15-1TU3P-0709
Lumpkin, R.
Eddy-driven dispersion in the Tropical and North Atlantic

XY0710
EGU06-A-10088;  OS15-1TU3P-0710
Killworth, P. D.; Nurser, A. J.
Implementing a nonlocal eddy parameterization into a global ocean model

XY0711
EGU06-A-10047;  OS15-1TU3P-0711
Nurser, A. J.
Eddy flux convergence and its impact on mixed layer depth in the Southern Ocean

XY0712
EGU06-A-10997;  OS15-1TU3P-0712
Dewar, W. K.; Haine, T.; Ring, D.
Slow Nonhydrostatic Flow and Balanced Energetics (cancelled)

XY0713
EGU06-A-09522;  OS15-1TU3P-0713
Rodriguez-Santana, A.; Marrero-Diaz, A. ; Martinez, A. ; Sangra, P. ; Machin, F.
Vertical eddy diffusivity in the southeast of the North Atlantic

XY0714
EGU06-A-09601;  OS15-1TU3P-0714
Blokhina, M.; Afanasyev, Ya.
Mesoscale surface circulation in the Black Sea: satellite observations

XY0715
EGU06-A-09623;  OS15-1TU3P-0715
Delgado, J.; Lafuente, J. G.; Sánchez, A.; Vargas, J. M.
Short period sea level oscillations at Gibraltar Strait: observations versus model results

XY0716
EGU06-A-05635;  OS15-1TU3P-0716
Van Leeuwen, P.J.
Why cyclones move westward

XY0717
EGU06-A-07220;  OS15-1TU3P-0717
Losch, M.; Herlufsen, S.; Timmermann, R.
Effects of heterogeneous surface boundary conditions on parameterized oceanic deep convection




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