New ROMS configuration for Southern California Bight

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New ROMS configuration for Southern Californi 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 - use of UCLA ROMS (were IRD-ROMS-AGRIF) better hydrodynamic kernel, robust KPP, better MPI - more frequent boundary update (was 30 days → 2 hours) - inclusion of surface gravity waves - utility of WRF (was MM5) and SWAN

description

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,...) - PowerPoint PPT Presentation

Transcript of New ROMS configuration for Southern California Bight

Page 1: New ROMS configuration for Southern California Bight

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

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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)

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L3 (250 m) runs(Aug. - Nov., 2006)

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USWL3 250 m, z = 0 m

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USWL3 250 m, z = -100 m

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USWL3 250 m, z = -500 m

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Effects of surface waves(subtidal EKE)

w/o wave

w/ wave

difference

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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 %

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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=

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L4 (75 m) runs(Aug. - Nov., 2006)

HTP 1-/5-mile outfalls

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mean depth-integrated passive tracer concentration

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mean tracer concentration along HTP transect

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mean velocity along HTP transect

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Mean mixed layer depth(from KPP)

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Hovmoller plotsof depth-averagedtracer concentration

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Alongshore profiles of depth-averaged tracer concentration at the shoreline

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Time series of depth-averaged tracer concentration at the shoreline at selected locations.

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Single-point PDF of depth-averaged passive tracer concentrations at the shore

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PSD of depth-averaged passive tracer concentrations at the shoreline

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SSS

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Hovmoller plotsof shoreline SSS

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Mean surface normalized relative vorticity and TKE (all frequencies)

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bandpass-filtered surface kinetic energy

high frq. (< 8h) semi-diurnal diurnal sub-tidal (> 36h)

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L5 (20 m) test run(7 days in Nov., 2006)

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