Saharan dust and phosphatic fidelity: A three-dimensional biogeochemical model of Trichodesmium as a nutrient source for red tides on the West Florida Shelf

2008 ◽  
Vol 28 (9) ◽  
pp. 1091-1115 ◽  
Author(s):  
J.M. Lenes ◽  
B.A. Darrow ◽  
J.J. Walsh ◽  
J.M. Prospero ◽  
R. He ◽  
...  
Keyword(s):  
Three Dimensional ◽  
Saharan Dust ◽  
Biogeochemical Model ◽  
Red Tides ◽  
West Florida Shelf ◽  
Nutrient Source ◽  
The West ◽  
Florida Shelf

A three-dimensional biophysical model of Karenia brevis dynamics on the west Florida shelf: A look at physical transport and potential zooplankton grazing controls

2008 ◽  
Vol 28 (1) ◽  
pp. 112-136 ◽  
Author(s):  
Scott P. Milroy ◽  
Dwight A. Dieterle ◽  
Ruoying He ◽  
Gary J. Kirkpatrick ◽  
Kristen M. Lester ◽  
...  
Keyword(s):  
Three Dimensional ◽  
Karenia Brevis ◽  
Biophysical Model ◽  
Zooplankton Grazing ◽  
West Florida Shelf ◽  
The West ◽  
Florida Shelf

The potential contribution of primary production by red tides to the west Florida shelf ecosystem1

1987 ◽  
Vol 32 (3) ◽  
pp. 762-767 ◽  
Author(s):  
G. A. Vargo ◽  
K. L. Carder ◽  
W. Gregg ◽  
E. Shanley ◽  
C. Heil ◽  
...  
Keyword(s):  
Primary Production ◽  
Potential Contribution ◽  
Red Tides ◽  
West Florida Shelf ◽  
The West ◽  
Florida Shelf

scholarly journals Isolation on the West Florida Shelf with implications for red tides and pollutant dispersal in the Gulf of Mexico

2010 ◽  
Vol 17 (6) ◽  
pp. 685-696 ◽  
Author(s):  
M. J. Olascoaga
Keyword(s):  
Gulf Of Mexico ◽  
Red Tide ◽  
Large Degree ◽  
Ocean Model ◽  
Red Tides ◽  
West Florida Shelf ◽  
The West ◽  
Transport Barrier ◽  
Florida Shelf ◽  
Simulated Surface

Abstract. Analysis of year-long drifter trajectories and records of simulated surface Lagrangian Coherent Structures (LCSs) have suggested the presence of a resilient Cross-Shelf Transport Barrier (CSTB) on the West Florida Shelf (WFS). The CSTB was conjectured to provide a large degree of isolation, which is consequential for the fueling of red tides on the southern WFS by nutrients possibly released by rivers and canals directly on the region. Here this conjecture is thoroughly tested by identifying LCSs as well as performing tracer advection calculations based on seven-year-long records of surface and subsurface currents produced by a HYbrid-Coordinate Ocean Model (HYCOM) simulation of the Gulf of Mexico (GoM). The identified LCSs suggest that the CSTB extends downward in the water column. The tracer calculations suggest that, while the majority of the nutrients possibly released by rivers and canals directly on the southern WFS are retained within the region for long times, only a small fraction of the nutrients possibly released by rivers outside the WFS reach the southern WFS, mainly accompanying shoreward excursions of the CSTB. These results add importance to the role played by the CSTB in controlling red tide development on the WFS. Implications of the results for the dispersal of pollutants, such as oil, in the GoM are discussed.

KNOWLEDGE-GUIDED CLASSIFICATION OF COASTAL ZONE COLOR IMAGES OFF THE WEST FLORIDA SHELF

2000 ◽  
Vol 14 (08) ◽  
pp. 987-1007 ◽  
Author(s):  
MINGRUI ZHANG ◽  
LAWRENCE O. HALL ◽  
DMITRY B. GOLDGOF ◽  
FRANK E. MÜLLER-KARGER
Keyword(s):  
Knowledge Base ◽  
Coastal Zone ◽  
Spatial Information ◽  
River Plume ◽  
Color Images ◽  
Red Tides ◽  
West Florida Shelf ◽  
The West ◽  
Florida Shelf

A knowledge-guided approach to automatic classification of Coastal Zone Color images off the West Florida Shelf is described. The approach is used to identify red tides on the West Florida Shelf, as well as areas with high concentration of dissolved organic matter such as a river plume found seasonally along the West Florida coast over the middle of the shelf. The Coastal Zone Color images are initially segmented by the unsupervised Multistage Random Sampling Fuzzy c-Means algorithm. Then, a knowledge-guided system is applied to the centroid values of resultant clusters to label case I, case II waters, a dilute river plume ("green river"), and red tide. The domain knowledge base contains information on cluster distribution in feature space, as well as spatial information such as bathymetry data. Our knowledge base consists of a rule-guided system and an embedded neural network. From 60 images, after training the system, this procedure recognizes all 15 images which contained a river plume and 45 images without. The system can correctly classify 74% of the pixels that belong to the river plume, which provides a substantial advantage to users looking for offshore extensions of riverine influence. Red tides are also successfully identified in a time series of images for which ground truth confirmed the presence of a harmful bloom.

USGS field activity 09FSH02 on the west Florida shelf, Gulf of Mexico, in August 2009

Data Series ◽  
2009 ◽  
Author(s):  
Lisa L. Robbins ◽  
Paul O. Knorr ◽  
Xuewu Liu ◽  
Robert H. Byrne ◽  
Ellen A. Raabe
Keyword(s):  
Gulf Of Mexico ◽  
West Florida Shelf ◽  
The West ◽  
Florida Shelf ◽  
Field Activity

USGS Field Activities 11CEV01 and 11CEV02 on the West Florida Shelf, Gulf of Mexico, in January and February 2011

Data Series ◽  
10.3133/ds711 ◽  
2014 ◽  
Author(s):  
Lisa L. Robbins ◽  
Paul O. Knorr ◽  
Kendra L. Daly ◽  
Carl A. Taylor
Keyword(s):  
Gulf Of Mexico ◽  
West Florida Shelf ◽  
The West ◽  
Florida Shelf

High-Frequency Radar Mapping of Surface Currents Using WERA

2007 ◽  
Vol 24 (3) ◽  
pp. 484-503 ◽  
Author(s):  
Lynn K. Shay ◽  
Jorge Martinez-Pedraja ◽  
Thomas M. Cook ◽  
Brian K. Haus ◽  
Robert H. Weisberg
Keyword(s):  
Time Series ◽  
High Frequency ◽  
Tidal Currents ◽  
Tropical Storm ◽  
Surface Velocity ◽  
Surface Currents ◽  
West Florida Shelf ◽  
The West ◽  
Florida Shelf ◽  
East West

Abstract A dual-station high-frequency Wellen Radar (WERA), transmitting at 16.045 MHz, was deployed along the west Florida shelf in phased array mode during the summer of 2003. A 33-day, continuous time series of radial and vector surface current fields was acquired starting on 23 August ending 25 September 2003. Over a 30-min sample interval, WERA mapped coastal ocean currents over an ≈40 km × 80 km footprint with a 1.2-km horizontal resolution. A total of 1628 snapshots of the vector surface currents was acquired, with only 70 samples (4.3%) missing from the vector time series. Comparisons to subsurface measurements from two moored acoustic Doppler current profilers revealed RMS differences of 1 to 5 cm s−1 for both radial and Cartesian current components. Regression analyses indicated slopes close to unity with small biases between surface and subsurface measurements at 4-m depth in the east–west (u) and north–south (υ) components, respectively. Vector correlation coefficients were 0.9 with complex phases of −3° and 5° at EC4 (20-m isobath) and NA2 (25-m isobath) moorings, respectively. Complex surface circulation patterns were observed that included tidal and wind-driven currents over the west Florida shelf. Tidal current amplitudes were 4 to 5 cm s−1 for the diurnal and semidiurnal constituents. Vertical structure of these tidal currents indicated that the semidiurnal components were predominantly barotropic whereas diurnal tidal currents had more of a baroclinic component. Tidal currents were removed from the observed current time series and were compared to the 10-m adjusted winds at a surface mooring. Based on these time series comparisons, regression slopes were 0.02 to 0.03 in the east–west and north–south directions, respectively. During Tropical Storm Henri’s passage on 5 September 2003, cyclonically rotating surface winds forced surface velocities of more than 35 cm s−1 as Henri made landfall north of Tampa Bay, Florida. These results suggest that the WERA measured the surface velocity well under weak to tropical storm wind conditions.

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