SIMULATION SETUP Modeled after conditions found in the central coast of California (CalCOFI line 70) during a typical July Domain is unstructured in alongshore.

Slides:



Advertisements
Similar presentations
WHERE IS F3 IN MODELING LARVAL DISPERSAL? Satoshi Mitarai, David Siegel University of California, Santa Barbara, CA Kraig Winters Scripps Institution of.
Advertisements

Seasonal and Interannual Variability of Peruvian anchovy Population Dynamics --progress report-- Yi Xu and Fei Chai June 2007.
Simulating Larval Dispersal in the Santa Barbara Channel James R. Watson 1, David A. Siegel 1, Satoshi Mitarai 1, Lie-Yauw Oey 2, Changming Dong 3 1 Institute.
ROMS Modeling for Marine Protected Area (MPA) Connectivity Satoshi Mitarai, Dave Siegel, James Watson (UCSB) Charles Dong & Jim McWilliams (UCLA) A biocomplexity.
Potential Approaches Empirical downscaling: Ecosystem indicators for stock projection models are projected from IPCC global climate model simulations.
Turbulent Coexistence Heather Berkley, Satoshi Mitarai, Bruce Kendall, David Siegel.
Connectivity by numbers James Watson, UCSB. ...the probability of transport of a parcel of water between one place and another Lagrangian particle simulations.
IDEALZED KERNEL SIMULATIONS REPORT #3 SATOSHI MITARAI UCSB F3 MEETING, 12/3/04.
Marine reserves and fishery profit: practical designs offer optimal solutions. Crow White, Bruce Kendall, Dave Siegel, and Chris Costello University of.
Modeling Larval Connectivity for the SoCal Bight Satoshi Mitarai, James Watson & David Siegel Institute for Computational Earth System Science University.
FISHING FOR PROFIT, NOT FISH: AN ECONOMIC ASSESSMENT OF MARINE RESERVE EFFECTS ON FISHERIES Crow White, Bruce Kendall, Dave Siegel, and Chris Costello.
Lagrangian Descriptions of Marine Larval Dispersion David A. Siegel Brian P. Kinlan Brian Gaylord Steven D. Gaines Institute for Computational Earth System.
Coexistence with Stochastic Dispersal in a Nearshore Multi-Species Fishery Heather Berkley & Satoshi Mitarai.
A SCALING TOOL TO ACCOUNT FOR INHERENT STOCHASTICITY IN LARVAL DISPERSAL Mitarai S., Siegel D. A., Warner R.R., Kendall B.E., Gaines S.D., Costello C.J.
ROLE OF HEADLANDS IN LARVAL DISPERSAL Tim Chaffey, Satoshi Mitarai Preliminary results and research plan.
Quantitative Description of Particle Dispersal over Irregular Coastlines Tim Chaffey, Satoshi Mitarai, Dave Siegel.
Connectivity in SoCal Bight UCLA-UCSB Telecon 1/14/08.
Citations 1.Poulain, P. M. and P. P. Niiler Statistical-Analysis of the Surface Circulation in the California Current System Using Satellite-Tracked.
Flow, Fish and Fishing 2007 All-Hands Meeting. F3’s Bottom Line… Larval transport is a stochastic process driven by coastal stirring Fish stocks, yields.
MODELING OF LARVAL DISPERSAL IN CALIFORNIA CURRENT Satoshi Mitarai 06/26/05.
SPACE / TIME SCALS OF LARVAL SETTLEMENT AND ITS MODELING Satoshi Mitarai Oct. 18, 2005.
GOAL OF THIS WORK ■ To investigate larval transport in “idealized” simulations ● To describe long term & short term dispersal kernels ● Four scenarios.
Flow, Fish and Fishing 2006 All-Hands Meeting July UCSB.
Stochastic Transport Generates Coexistence in a Nearshore Multi-Species Fishery Heather Berkley, Satoshi Mitarai, Bruce Kendall, David Siegel, Robert Warner.
Population Dynamics in a Stirred, not Mixed, Ocean Bruce Kendall, David Siegel, Christopher Costello, Stephen Gaines, Ray Hilborn, Robert Warner, Kraig.
Temperature Profiles of Settling Larvae+ Satoshi Mitarai 06/26/06.
Larval Connectivity Talk Goals 1.) INTRODUCE A NEW FLOW DATASET 2.) COMPARE WITH OLD 3.) STATISTICS... SOME WAYS OF VISUALIZING THE DATA.
Flow, Fish & Fishing A Biocomplexity Project
Optimal Spatial Fishery Management for the Southern California Bight Dave Siegel, Chris Costello, Satoshi Mitarai (UCSB), Jim McWilliams & Charles Dong.
Simulating Larval Dispersal in the Santa Barbara Channel.
Marine reserve spacing and fishery yield: practical designs offer optimal solutions. Crow White, Bruce Kendall, Dave Siegel, and Chris Costello University.
DOES LARVAL BEHAVIOR MATTER? No because cross-shore transport does not change within above 50 m or so Yes because larvae will be on different flow layers.
Scaling of Larval Transport in the Coastal Ocean Satoshi Mitarai, Dave Siegel, Kraig Winters Postdoctoral Researcher University of California, Santa Barbara.
Flow, Fish and Fishing: Building Spatial Fishing Scenarios Dave Siegel, James Watson, Chris Costello, Crow White, Satoshi Mitarai, Dan Kaffine, Will White,
Coastal Connectivity in the Southern California Bight Dave Siegel, James Watson, Satoshi Mitarai, (UCSB) Charles Dong & Jim McWilliams (UCLA) Coastal Environmental.
Inherent Uncertainties in Nearshore Fisheries: The Biocomplexity of Flow, Fish and Fishing Dave Siegel 1, Satoshi Mitarai 1, Crow White 1, Heather Berkley.
Scaling of larval dispersal in the coastal ocean Satoshi Mitarai Postdoctoral Researcher University of California, Santa Barbara.
Inherent Uncertainties in Nearshore Fisheries: The Biocomplexity of Flow, Fish and Fishing Dave Siegel 1, Satoshi Mitarai 1, Crow White 1, Heather Berkley.
Quantifying Connectivity in the Coastal Ocean With Application to the Southern California Bight Satoshi Mitarai, Dave Siegel, James Watson (UCSB) Charles.
Fishing in a stirred ocean: sustainable harvest can increase spatial variation in fish populations Heather Berkley Bruce Kendall, David Siegel, Christopher.
ROLE OF HEADLAND IN LARVAL DISPERSAL Satoshi Mitarai Preliminary results and research plan (Maybe for the next F3 meeting)
Spatial and Temporal Patterns in Modeling Marine Fisheries Heather Berkley.
Fishing in a stirred ocean: sustainable harvest can increase spatial variation in fish populations Heather Berkley Bruce Kendall David Siegel.
ROLE OF IRREGULAR COASTLINES IN LARVAL DISPERSAL Tim Chaffey, Satoshi Mitarai, Dave Siegel Results and research plan.
Examining the interaction of density dependence and stochastic dispersal over several life history scenarios Heather Berkley Bruce Kendall David Siegel.
Settlement Scheme & Connectivity Satoshi Mitarai 1/17/2007.
Can Packet Larval Transport Create Favorable Conditions for the Storage Effect? Heather & Satoshi “Flow, Fish & Fishing,” UCSB Group Meeting Feb. 21, 2007.
Scaling and Modeling of Larval Settlement Satoshi Mitarai Oct. 19, 2005.
“IDEALIZED” WEST COAST SIMULATIONS Numerical domain Boundary conditions Forcings Wind stress: modeled as a Gaussian random process - Statistics (i.e.,
The Influence of Diel Vertical Migration on Krill Recruitment to Monterey Bay Sarah Carr Summer Internship Project Monterey Bay Aquarium Research Institute.
1.Introduction 2.Description of model 3.Experimental design 4.Ocean ciruculation on an aquaplanet represented in the model depth latitude depth latitude.
Introduction Greenland halibut (Reinhardtius hippoglossoides; GH) have declined significantly since the 1970’s in the eastern Bering Sea (EBS). The reasons.
Partnership for Interdisciplinary Studies of Coastal Oceans PISCO.
SCCOOS Goals and Efforts Within COCMP, SCCOOS aims to develop products and procedures—based on observational data—that effectively evaluate and improve.
Southern California Coast Observed Temperature Anomalies Observed Salinity Anomalies Geostrophic Along-shore Currents Warming Trend Low Frequency Salinity.
Ocean currents move ocean animals around. Small animals in the ocean can be pushed around by currents, and may not be able to choose where to go. Adult.
Modeling the biological response to the eddy-resolved circulation in the California Current Arthur J. Miller SIO, La Jolla, CA John R. Moisan NASA.
Flow, Fish and Fishing Dave Siegel, Chris Costello, Steve Gaines, Bruce Kendall, Satoshi Mitarai & Bob Warner [UCSB] Ray Hilborn [UW] Steve Polasky [UMn]
Santa Barbara Coastal LTER & California’s Marine Protected Areas Dave Siegel University of California, Santa Barbara Santa Barbara Coastal LTER.
Over the northern West Florida Shelf several reef fish species (with gag grouper being a key species) spawn near the outer shelf edge in winter and early.
The management of small pelagics. Comprise the 1/3 of the total world landings Comprise more than 50% of the total Mediterranean landings, while Two species,
Issues of Scale Both time & space – Time: waves, tides, day, year, ENSO – Space: local, regional, global Set how processes interact Scale invariance.
Hydrodynamic Connectivity in Marine Population Dynamics Satoshi Mitarai 1, David A. Siegel 1, Bruce E. Kendall 1, Robert R. Warner 1, Steven D. Gaines.
Ocean Surface Current Observations in PWS Carter Ohlmann Institute for Computational Earth System Science, University of California, Santa Barbara, CA.
Operational fish larval drift modelling Bjørn Ådlandsvik og Frode Vikebø Institute of Marine Research Opnet meeting, Geilo, May 2008.
Current Oversights in Marine Reserve Design. MARINE RESERVE DATA BASE 81 studies, 102 measurements Halpern, in press.
Southern California Coast Observed Temperature Anomalies Observed Salinity Anomalies Geostrophic Along-shore Currents Warming Trend Low Frequency Salinity.
The California Current System from a Lagrangian Perspective Carter Ohlmann Institute for Computational Earth System Science, University of California,
Coastal Upwelling. What comes up… Equatorward winds drive nearshore upwelling Reversals of these winds have important effects -> downwelling Has implications.
Ecosystem Connectivity
Presentation transcript:

SIMULATION SETUP Modeled after conditions found in the central coast of California (CalCOFI line 70) during a typical July Domain is unstructured in alongshore direction Forced by stochastic wind and alongshore pressure gradient, derived from observation Larvae are assumed to follow surface water parcels and are released daily for 90 days within the inner 20 km. Settlement occurs after the larvae have developed competency for their next life stage and if they find suitable habitat We consider settlement successful if a larva is found within the inner 20 km within 20 to 40 days after release Biological sources of larval mortality are not included CONNECTIVITY AMONG NEARSHORE ECOSYSTEMS: NATURE OF LARVAL TRANSPORT S. Mitarai 1, D.A. Siegel 1, C.J. Costello 1, S.D. Gaines 1, B.E. Kendall 1, R.R. Warner 1 and K.B. Winters 2 1 Institute for Computational Earth System Science, University of California, Santa Barbara, Santa Barbara, CA Integrative Oceanography Division, Scripps Institution of Oceanography, La Jolla, CA ABSTRACT Key to the predictive understanding of many nearshore marine ecosystems is the transport of larvae by ocean circulation processes. Many species release thousands to billions of larvae to develop in pelagic waters, but only a few lucky ones successfully settle to suitable habitat and recruit to adult life stages. Methodologies for predicting the larval transport are still primitive, and simple diffusive analyses are still used for many important applications. In this study, we investigate mechanisms of larval transport using idealized simulations of time-evolving coastal circulations in the California Current system with Lagrangian particles as models for planktonic larvae. Connectivity matrices, which describe the source- destination relationships for larval transport for a given larval development time course, are used to diagnose the time-space dynamics of larval settlement. Many important fishery management applications require knowledge of fish stocks on a year-to-year or generation-to-generation basis. For these short time scales (typically less than 1 year), larval dispersal is generally far from a simple diffusive process and the consideration of the stochastic and episodic nature of larval dispersal is required. This work provides new insights into spatial temporal dynamics of nearshore fish stocks. GOALS OF THIS STUDY Understand the role of larval transport in predicting nearshore fish stocks & its proper management Investigate source-to-destination relationships for Lagrangian particles as models for planktonic larvae which originate & settle in nearshore environment by using idealized realizations of coastal circulation tied to real data Develop simple models for the connectivity of nearshore habitat based on the obtained simulation results, and use them in fish stock/harvest models Figure 1: Depictions of the sea level distribution (color contours in cm) and sample larval trajectories. The circles show the location of the larvae while the white trails behind each show their previous 2 day trajectories. The vertical dashed red line indicates the boundary for the nearshore habitat where from which larvae are released from and settlement can occur. SUMMARY & FUTURE PLAN Summary The coastal circulation simulation suggest that the connectivity of coastal habitats is heterogeneous when viewed on short time scales (e.g., less than 10 years). Such stochastic will create unavoidable uncertainty in fish recruitment, potentially complicating the management of nearshore ecosystem. We proposed a new simple model that reasonably accounts for stochastic nature of larval transport found in the simulations. Future plan Test more elaborate larval behaviors and address its role in the connectivity of coastal habitats. Assess the role of headlands Use the proposed model in fish stock/harvest model in place of a simple diffusion model. STOCHASTIC NATURE OF LARVAL SETTLEMENT Only a limited number of independent settlement events occur during one spawning season Sometimes, arrival events occur coincident with reversals in the alongshore wind, which would advect surface water parcels onshore. More often than not, successful settlement occurs because eddy advect larvae to suitable habitat Figure 2: Time series showing a) the departure density of successful settlers at a given alongshore location (vertical axis) and at a give time (horizontal axis), b) the arrival density of successful settlers at a given alongshore location and at a given time and c) the alongshore wind speed forcing the model. The first larvae are able to settle on day 20 (left vertical dashed line). Larval releases stop at day 90 (middle vertical dashed line) and settlement is possible until day 130 (right vertical dashed line). Consider connectivity among nearshore sites as a superposition of “larval packets” Describe the number of “larval packets” based on simple scaling N = (T/t)(L/l)f, where T is larval release duration, t is Lagrangian de-correlation time scale, L is the domain size, l is Rossby radius of deformation (or the packet size) and f is larval survivability. Source and destination of each larval packet are randomly assigned based on the distribution given by diffusion model Nearshore eddies sweep larvae together into “packets” which stay together through much of pelagic stage CONNECTIVITY AMONG NEARSHORE HABITATS Connectivity is heterogeneous & intermittent even in unstructured domain Connectivity can differ for differing life histories Connectivity can differ for differing larval behavior PACKET MODELING Figure 6: Connectivity matrices for larval dispersal examining the role of the duration of the observation time. (a) Connectivity matrices obtained from the simulations for 1, 6 and 12 years of observation time. (b) Prediction by a simple advection-diffusion approach. (c) Prediction by the settlement-pulse model for 1, 6, 12 and 120 years of observation time. We measure spatial heterogeneity in connectivity by using the coefficient of variation of the connectivity along the mean source location line (black dash-dotted lines). The obtained results are 0.5, 0.25, 0.15 and 0 (upper panels from left to right) and 0.4, 0.22, 0.16 and 0.08 (lower panels from left to right) Figure 3: Connectivity matrices for larval dispersal for (a) a first realization of simulation, (b) diffusion model and c) a second realization of simulation. Source locations (vertical axis) and destination locations (horizontal axis) are identified with their alongshore location. The dashed slanted line indicates self settlement, i.e., where source locations are identical to destination locations. The connectivity matrices normalized so that the summed value becomes unity. Proposed model can capture the stochastic nature of connectivity fairly well Figure 4: Connectivity matrices examining the role of life histories. Larval settlement competency time window is set to a) 20 to 40 days and b) 5 to 10 days. The same flow field is used here. Figure 5: Connectivity matrices examining the role of larval behavior. a) Larvae are surface followers. b) Mimicking ontogenetic vertical migration by letting larvae change their depth from the surface to 30 m (after 10 days at surface). Here, the same flow field is used.