coastal connectivity in the southern california bight
DESCRIPTION
Coastal Environmental Quality Initiative 2007-2008. Coastal Connectivity in the Southern California Bight. Dave Siegel, James Watson, Satoshi Mitarai, (UCSB) Charles Dong & Jim McWilliams (UCLA). Goal of This Study. Assess coastal connectivity via advection of water parcels in SoCal Bight - PowerPoint PPT PresentationTRANSCRIPT
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
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
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
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
Where do they go?(From North Shore of SBC Islands)
Day 0 = 7/1/02 Day 0 =1/1/02
• Natal areas (self settlement)• Nowhere (few settlements)
Red dots = settling particles (competency = 20 - 40 d)
Single day release in Summer Single day release in Winter
Where do they go?(From Palos Verdes Peninsula)
• “Everywhere” • North of PV / SBC
Red dots = settling particles (competency = 20 - 40 d)
Summer Winter
Day 0 = 7/1/02 Day 0 =1/1/02
Where do they go?(From San Niclolas Islands)
• Few settlements • Mainland / SBC Islands
Red dots = settling particles (competency = 20 - 40 d)
Summer Winter
Day 0 = 7/1/02 Day 0 =1/1/02
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)
Summer Winter
Day 0 = 7/1/02 Day 0 =1/1/02
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)
Summer Winter
Day 0 = 7/1/02 Day 0 =1/1/02
Where do they come from?(To San Nicholas Islands)
• PV / natal areas (few) • PV / SBC (few)
Red dots = settling particles (competency = 20 - 40 d)
Summer Winter
Day 0 = 7/1/02 Day 0 =1/1/02
Role of Chaotic Eddying Motions(From San Nicholas Island)
Day 0 = Jan. 1, 2002 Day 0 = Jan. 15, 2002
• From “everywhere” • Palos Verdes / Natal
Red dots = settling particles (competency = 20 - 40 d)
Summer Winter
Rolf of Vertical Positioning(From Palos Verdes)
Day 0 = July 1, 2002 Day 0 = Jan. 1, 2002
• More spread • More clustering
Red dots = settling particles (competency = 20 - 40 d)
Passive vertical transport DVM (20 m)
And more...
•Inter-annual variability
•Climate variability (e.g., ENSO)
•Eileen brought 1997 & 1998 flow simulations