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Nomenclature & Glossary

$\rho$ water density = 1000 kg/m3
$\eta$ water height above mean level
$\overline{H}$ mean level
Hu depth below mean level
H distance from sea bottom to water surface
$
\overline{u}, \overline{v} $ depth averaged velocities
g gravity acceleration
$\Omega$ coefficient giving place to Coriolis force
$\omega$ earth's angular velocity, [rad/s]
$\phi$ latitude, $35^\circ$
Ch bottom stress Chezy coefficient
Z0 bottom roughness, 0.001 m
$\tau _{sx},\tau _{sy}$ wind stress components at sea surface
$\varepsilon$ coefficient for turbulent viscosity
Wx, Wy wind velocity components measured 10 meters above
  sea level
$\rho_a$ air density = 1 kg/m3
CD sea surface stress coefficient
$\Delta t$ time step
$\Delta x$ grid size
$\overrightarrow{c} =(c^x,c^y)$ wave celerity
th5 mesh of 5.000 cells
th20 mesh of 20.000 cells
th80 mesh of 80.000 cells
$\alpha$ latency time
$\beta$ bandwidth throughput
Rc communication time rate between the use of mesh
  th20 to mesh th5
Sg numerical solution using grid g
Eg pointwise error estimate
L exact solution
p accuracy order
np Number of processes into which the parallel program is
  distributed.
Tcompute computation time for 1 time step
Tcommunic communication time for 1 time step
PVM Parallel Virtual Machine
DD Domain Decomposition.
ADI Alternate Directions Implicit.
SMP Symmetric Multi-Processing.
MFLOPS Millions of floating point operations by second.
CFL Courant-Friedrichs-Lewy .
CFD Computational Fluid Dynamics


next up previous contents
Next: General Performance Considerations Up: Final Remarks. Previous: Further Work.
Elias Kaplan M.Sc.
1998-07-22