New ROMS configuration for Southern California Bight
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New ROMS configuration for Southern California Bight
Descendant of the previous UCLA configurations(cf., Marchesiello et al. 2003; Dong at al., 2009)
Improved from the previous SCB 1-km modeling
- higher resolutions(L1: 20 km → 5 km, L2: 6 km → 1 km, L3: 1 km → 250 m,...)
- use of UCLA ROMS (were IRD-ROMS-AGRIF)better hydrodynamic kernel, robust KPP, better MPI scaling,...
- more frequent boundary update (was 30 days → 2 hours)
- inclusion of surface gravity waves
- utility of WRF (was MM5) and SWAN
Newest quadrupleNested ROMS configuration
L1 (5 km)
L2 (1 km)L2 (1 km)
L3 (250 m)
L3 (250 m) L4 (75 m) L4 (75 m)
L3 (250 m) runs(Aug. - Nov., 2006)
USWL3 250 m, z = 0 m
USWL3 250 m, z = -100 m
USWL3 250 m, z = -500 m
Effects of surface waves(subtidal EKE)
w/o wave
w/ wave
difference
Conservative Wave Effects: Overall Thermocline Deepening and Altering Upper Mean Circulation
with WEC (with WEC) – (no WEC)
mean mixed-layer depth(KPP hbl)
mean stream function(upper layer > -25 m)
x 103 (m2/s)
(m)
with WEC (with WEC) – (no WEC)
~15 %
~15 %
Vortex force vs. Stokes-Coriolis effect
- mean advection of eddies (JSC : Stokes-Coriolis force)- eddy-wave interaction (JVF : vortex force) --> exceeds JSC
~ <JVF>/<JSC>Ro=
L4 (75 m) runs(Aug. - Nov., 2006)
HTP 1-/5-mile outfalls
mean depth-integrated passive tracer concentration
mean tracer concentration along HTP transect
mean velocity along HTP transect
Mean mixed layer depth(from KPP)
Hovmoller plotsof depth-averagedtracer concentration
Alongshore profiles of depth-averaged tracer concentration at the shoreline
Time series of depth-averaged tracer concentration at the shoreline at selected locations.
Single-point PDF of depth-averaged passive tracer concentrations at the shore
PSD of depth-averaged passive tracer concentrations at the shoreline
SSS
Hovmoller plotsof shoreline SSS
Mean surface normalized relative vorticity and TKE (all frequencies)
bandpass-filtered surface kinetic energy
high frq. (< 8h) semi-diurnal diurnal sub-tidal (> 36h)
L5 (20 m) test run(7 days in Nov., 2006)