Optical variability associated with a Gymnodinium breve red tide event off northwestern Florida 

Lohrenz, Steven E.1, Donald G. Redalje1, and Gary J. Kirkpatrick2

 Red tides of the toxic dinoflagellate, Gymnodinium breve, are commonly observed along the Florida coast.  Our ability to detect and quantify these phenomena has the potential to be greatly enhanced by observations of in situ and remotely sensed optical properties.  During October 2000, optical measurements were conducted in the area of a red tide bloom off the northwest Florida coast as part of the Florida ECOHAB program.  Time-series sampling of the bloom was carried out over a 48 h period while tracking a surface drifter (Fig. 1).  Cells of G. breve accounted for the vast majority of particles visible by light microscopy.  Repetitive profiles with a spectral absorption and attenuation meter (WETLabs, Inc. ac-9) revealed substantial vertical structure in attenuation and absorption that was largely attributable to G. breve distributions.  Observed temporal variations in vertical structure were consistent with vertical migration and apparent wind-induced mixing.  Our results illustrate the utility of optical measurements for characterizing red tide phenomena. 

 1The University of Southern Mississippi Department of Marine Science, Stennis Space Center, MS 39529

2Mote Marine Laboratory, 1600 Ken Thompson Parkway, Sarasota, FL  34236

Figure 1.  Time-series of beam attenuation at 532 nm measured with a WETLabs, Inc. spectral absorption and attenuation meter (ac-9).  Regions of high attenuation near the surface and bottom appeart to correspond to dense accumulations of G. breve cells.    

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Mie approximation of light scattering by Gymnodinium breve and its relationship to in situ scattering during a red tide event  

Mahoney, Kevin L.1, Steven E. Lohrenz1, Gary J. Kirkpatrick2, Gary L. Fahnenstiel3

 Scattering of light by particles in aquatic environments varies in relationship to particle properties including size distribution, shape and composition (refractive index).  The backscattering of light strongly influences water-leaving radiance and, subsequently, remote sensing reflectance.  Ideally, information about particle properties and concentrations can be derived from remotely sensed signatures.  However, the contribution to backscatter by specific types of particles is difficult to measure in the field.  Backscattering by particles of known characteristics can be modeled through Mie calculations for homogeneous spheres.  During October 2000, a cruise was conducted during a red tide event off the northwest Florida coast as part of the Florida ECOHAB program.  Measurements included spectral absorption and particle size distributions and concentrations in samples dominated by the red tide organism, Gymnodinium breve.  In addition, in situ total scattering and absorption were determined using a spectral absorption and attenuation meter (WETLabs, Inc. ac-9).  The objective of this project was to compare Mie approximations of scattering to measurements of total in situ scattering, and to assess variability in the backscattering ratio attributable to G. breve.  This information will be used to evaluate the potential for using remote sensing to detect red tide events.   

1The University of Southern Mississippi Department of Marine Science, Stennis Space Center, MS 39529

2Mote Marine Laboratory, 1600 Ken Thompson Parkway, Sarasota, Florida  34236

3NOAA Great Lakes Environmental Research Laboratory, 1431 Beach St., Muskegon, MI 49441

 

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