West Florida Shelf and Tampa Bay Responses to Hurricane Irma: What Happened and Why

Join SECOORA for a webinar that analyzes the West Florida Continental Shelf's response to Hurricane Irma using a combination of in situ observations and numerical circulation models. Reserve your spot now! Download the Flyer

NEWS
February 1, 2018

Join SECOORA for a webinar that analyzes the West Florida Continental Shelf’s response to Hurricane Irma using a combination of in situ observations and numerical circulation models.  More info below!

Reserve your spot now!

Download the Flyer

West Florida Shelf and Tampa Bay Responses to Hurricane Irma: What Happened and Why

Presenter: Dr. Bob Weisberg, University of South Florida College of Marine Science
Date: February 13, 12 PM ET

Hurricane Irma impacted the west Florida continental shelf (WFS) as it transited the State of Florida from September 10-12, 2017, first making landfall at Cudjoe Key and then again at Naples, as a Category 2 hurricane.  The WFS response to Irma is analyzed using a combination of in situ observations and numerical circulation models. The observations include water column velocity, sea surface temperature, winds and sea level. The models are: 1) the West Florida Coastal Ocean Model (WFCOM) that downscales from the deep Gulf of Mexico, across the shelf and into the estuaries by nesting the unstructured grid FVCOM in the Gulf of Mexico HYCOM and 2) the Tampa Bay Coastal Ocean Model (TBCOM) that provides much higher resolution for the Tampa Bay vicinity (Tampa Bay, Sarasota Bay, the Intracoastal Waterway and all of the inlets connecting these with the Gulf of Mexico) by nesting FVCOM in WFCOM.

Both the observations and the model simulations revealed strong upwelling and vertical mixing followed by a downwelling as the storm passed by.  This was accompanied by a rapid drop in sea surface temperature by about 4 degrees C and large decreases in sea level with negative surges causing drying in the Florida Bay, Charlotte Harbor, Tampa Bay estuaries and the Big Bend region.  The transport and exchange of water between the shelf and the estuaries and between the shelf and the Florida Keys reef track during the hurricane have important ecosystem and sediment transport implications, including an inlet breach that occurred at the Pinellas Co. Shell Key preserve

About the Presenter

Dr. Robert Weisberg is a Distinguished University Professor of Physical Oceanography at the University of South Florida (USF). His current research emphasizes the West Florida Continental Shelf (WFS) and the interactions occurring between the shelf and the deep ocean and between the shelf and the estuaries. He maintains a coordinated program of in situ observations, analyses, and numerical circulation models aimed at describing and understanding the processes that determine WFS water properties, with applications to matters of societal concern. Dr. Weisberg is on the Board of Directors for the SECOORA and is a Fellow of the Southeastern Universities Research Association (SURA). Dr. Weisberg is a member of the Oceanography Society, the American Geophysical Union, the American Meteorological Society and Sigma Xi. He obtained his MS and PhD in physical oceanography in 1972 and 1975 from the University of Rhode Island.