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Coastal Connectivity in the Southern California Bight Dave Siegel, James Watson, Satoshi Mitarai, (UCSB) Charles Dong & Jim McWilliams (UCLA) Coastal Environmental Quality Initiative 2007-2008
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Goal of This Study Assess coastal connectivity via advection of water parcels in SoCal Bight Help MPA design (e.g., Chris’s work) Approach: implement offline particle tracking in Charles’ flow simulations
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Charles’ ROMS Simulations Simulated flow fields (surface vorticity normailized by f) Forced by “realistic” wind Dong and McWilliams (2007) Conil & Hall (2006) Simulated wind field Wind forcing
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Flow Circulation in SoCal Bight A Big Upllwelling shadow 6 synoptic views of circulation in SBC
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Offline Particle Tracking Nearshore habitat = 100 m or shallower Lagrangian particles are released & settle within habitats Settlement = particles within nearshore habitat during competency time window Nearshore habitat range 100-m isobath
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Where do they go? (From North Shore of SBC Islands) Day 0 = 7/1/02Day 0 =1/1/02 Natal areas (self settlement) Nowhere (few settlements) Red dots = settling particles (competency = 20 - 40 d) Single day release in SummerSingle day release in Winter
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Where do they go? (From Palos Verdes Peninsula) “Everywhere” North of PV / SBC Red dots = settling particles (competency = 20 - 40 d) SummerWinter Day 0 = 7/1/02Day 0 =1/1/02
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Where do they go? (From San Niclolas Islands) Few settlements Mainland / SBC Islands Red dots = settling particles (competency = 20 - 40 d) SummerWinter Day 0 = 7/1/02Day 0 =1/1/02
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Where do they come from? (To North Shore of SBC Islands) Mostly from Ventura / LA From “everywhere” Red dots = settling particles (competency = 20 - 40 d) SummerWinter Day 0 = 7/1/02Day 0 =1/1/02
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Where do they come from? (To Palos Verdes Peninsula) From natal areas South of PV / San Nicholas Red dots = settling particles (competency = 20 - 40 d) SummerWinter Day 0 = 7/1/02Day 0 =1/1/02
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Where do they come from? (To San Nicholas Islands) PV / natal areas (few) PV / SBC (few) Red dots = settling particles (competency = 20 - 40 d) SummerWinter Day 0 = 7/1/02Day 0 =1/1/02
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Schematic Diagram
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Role of Chaotic Eddying Motions (From San Nicholas Island) Day 0 = Jan. 1, 2002Day 0 = Jan. 15, 2002 From “everywhere” Palos Verdes / Natal Red dots = settling particles (competency = 20 - 40 d) SummerWinter
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Rolf of Vertical Positioning (From Palos Verdes) Day 0 = July 1, 2002Day 0 = Jan. 1, 2002 More spread More clustering Red dots = settling particles (competency = 20 - 40 d) Passive vertical transportDVM (20 m)
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And more... Inter-annual variability Climate variability (e.g., ENSO) Eileen brought 1997 & 1998 flow simulations
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Short-term Goal Write up a physical oceanographic two papers describing dispersal patterns in SCB By January James talk more about connectivity
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