A coordinated coastal ocean observing and modeling system for the West Florida Continental Shelf

The evolution of harmful algal blooms, while dependent upon complex biological interactions, is equally dependent upon the ocean circulation since the circulation provides the basis for the biological interactions by uniting nutrients with light and distributing water properties. For the coastal ocean, the circulation and the resultant water properties, in turn, depend on interactions between both the continental shelf and the deep-ocean and the continental shelf and the estuaries since the deep-ocean and the estuaries are primary nutrient sources. Here we consider a coordinated program of observations and models for the West Florida Continental Shelf (WFS) intended to provide a supportive framework for K. brevis red-tide prediction as well as for other coastal ocean matters of societal concern. Predicated on lessons learned, the goal is to achieve a system complete enough to support data assimilative modeling and prediction. Examples of the observations and models are presented and application is made to aspects of the 2005 red-tide. From an observational perspective, no single set of measurements is adequate. Required are a broad mix of sensors and sensor delivery systems capable of describing the three-dimensional structure of the velocity and density fields. Similarly, models must be complete enough to include the relevant physical processes, and data assimilation provides the integrative framework for maximizing the joint utility of the observations and models. While we are still in the exploratory stages of development, the lessons learned and application examples may be useful to similar programs under development elsewhere. One scientific finding is that the key to understanding K. brevis red-tide on the WFS lies not at the surface, but at depth.

[1]  R. Weisberg,et al.  A Simulation of the Hurricane Charley Storm Surge and its Breach of North Captiva Island , 2006 .

[2]  C. Garrett,et al.  Boundary Mixing and Arrested Ekman Layers: Rotating Stratified Flow Near a Sloping Boundary , 1993 .

[3]  R. Weisberg,et al.  An upwelling case study on Florida's west coast , 2000 .

[4]  Karen A. Steidinger,et al.  Gymnodinium breve red tide blooms: Initiation, transport, and consequences of surface circulation , 1997 .

[5]  R. Weisberg,et al.  West Florida shelf response to upwelling favorable wind forcing: Kinematics , 1999 .

[6]  Changsheng Chen,et al.  An Unstructured Grid, Finite-Volume, Three-Dimensional, Primitive Equations Ocean Model: Application to Coastal Ocean and Estuaries , 2003 .

[7]  Ruoying He,et al.  West Florida Shelf Circulation on Synoptic, Seasonal, and Interannual Time Scales , 2013 .

[8]  F. Muller‐Karger,et al.  Phytoplankton Response to Intrusions of Slope Water on the West Florida Shelf: Models and Observations , 2003 .

[9]  R. Weisberg,et al.  Rookery Bay and Naples Bay circulation simulations: applications to tides and fresh water inflow regulation. , 2010 .

[10]  Frank E. Muller-Karger,et al.  West Florida Shelf Response to Local Wind Forcing: April 1998 , 2001 .

[11]  R. Weisberg,et al.  Local and deep‐ocean forcing contributions to anomalous water properties on the West Florida Shelf , 2003 .

[12]  Alexander F. Shchepetkin,et al.  The regional oceanic modeling system (ROMS): a split-explicit, free-surface, topography-following-coordinate oceanic model , 2005 .

[13]  Donald M. Anderson,et al.  Physiological ecology of harmful algal blooms , 1998 .

[14]  J. Beckers,et al.  Multivariate reconstruction of missing data in sea surface temperature, chlorophyll, and wind satellite fields , 2007 .

[15]  S. Lentz,et al.  Asymmetric Behavior of an Oceanic Boundary Layer above a Sloping Bottom , 1991 .

[16]  Daniel R. Lynch,et al.  Mechanisms regulating large-scale seasonal fluctuations in Alexandrium fundyense populations in the Gulf of Maine: Results from a physical–biological model , 2005 .

[17]  F. Muller‐Karger,et al.  Coastal Ocean Circulation Influences on Remotely Sensed Optical Properties: a West Florida Shelf Case Study , 2004 .

[18]  Remy Baraille,et al.  The HYCOM (HYbrid Coordinate Ocean Model) data assimilative system , 2007 .

[19]  R. Weisberg,et al.  West Florida shelf circulation and temperature budget for the 1999 spring transition , 2001 .

[20]  Scott P. Milroy,et al.  Red tides in the Gulf of Mexico: Where, when, and why? , 2006, Journal of geophysical research.

[21]  G. Janowitz,et al.  A Model and Observations of Time-Dependent Upwelling over the Mid-Shelf and Slope , 1980 .

[22]  Ruoying He,et al.  A cloud‐free, satellite‐derived, sea surface temperature analysis for the West Florida Shelf , 2003 .

[23]  James C. McWilliams,et al.  The Regional Ocean Modeling System : A Split-Explicit , Free-Surface , Topography-Following-Coordinate Ocean Model , 2022 .

[24]  Robert H. Weisberg,et al.  Hurricane storm surge simulations for Tampa Bay , 2006 .

[25]  K. Steidinger Implications of dinoflagellate life cycles on initiation of Gymnodinium breve red tides. , 1975, Environmental letters.

[26]  R. Weisberg,et al.  West Florida Continental Shelf Response to Upwelling Favorable Wind Forcing 2. Dynamics , 1999 .

[27]  Robert H. Weisberg,et al.  Patterns of ocean current variability on the West Florida Shelf using the self-organizing map , 2005 .

[28]  Eric P. Chassignet,et al.  North Atlantic Simulations with the Hybrid Coordinate Ocean Model (HYCOM): Impact of the Vertical Coordinate Choice, Reference Pressure, and Thermobaricity , 2003 .

[29]  G. Vargo,et al.  Nutrient availability in support of Karenia brevis blooms on the central West Florida Shelf: What keeps Karenia blooming? , 2008 .

[30]  Ruoying He,et al.  Coastal ocean wind fields gauged against the performance of an ocean circulation model , 2004 .

[31]  K. Brink,et al.  The Response of Stratified, Frictional Flow of Shelf and Slope Waters to Fluctuating Large-Scale, Low-Frequency Wind Forcing , 1985 .

[32]  Robert H. Weisberg,et al.  Circulation of Tampa Bay driven by buoyancy, tides, and winds, as simulated using a finite volume coastal ocean model , 2006 .

[33]  A. Barth,et al.  Benefit of Nesting a Regional Model into a Large-Scale Ocean Model Instead of Climatology. Application to the West Florida Shelf , 2008 .