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Tampa

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About Tampa

Coming Soon...

Storm Surge History

Coming Soon...

Infographics 



Storm Surge Data

Raw Data
Peak water level 
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The Tampa data selection circle is centered on the following coordinates: Lat: 27.9313, Lon: -82.4689​.
storm-by-storm
about storm surge data

Data Selection

Ideally, storm surge data would be taken from long-term tide gauges. Unfortunately, this is not possible for several reasons:
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1. The record length of most tide gauges is not long enough to capture more than several decades of data (there are a few exceptions)
2. Large storm surges exceeding 10 ft (3.05 m) often destroy tide gauges
3. Storm surge is a localized phenomenon, with surge heights often changing considerably over several miles. Therefore, tide gauges usually do not pick up the peak storm surge because the network of gauges is not dense enough

Considering these problems, U-Surge utilizes a circle with a 10-mile (16-km) radius for data capture. This area is optimal, as larger circles capture more data but decrease data homogeneity, but smaller circles do not capture enough observations.

Sea Level Rise 

Sea-Level Rise Scenarios Table from U.S. Army Corps of Engineers
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Table of SLR scenarios for St. Petersburg, Florida from CorpsClimate web-tool developed by U.S. Army Corps of Engineers. Data from this table revised August 15, 2017. Available on the Web at: http://corpsclimate.us/ccaceslcurves.cfm.
Sea-Level Rise Graphic from U.S. Army Corps of Engineers
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Graph of SLR scenarios for St. Petersburg, Florida, from CorpsClimate web-tool developed by U.S. Army Corps of Engineers. Data from this table revised August 15, 2017. Available on the Web at: http://corpsclimate.us/ccaceslcurves.cfm.
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​Combined Sea-Level Rise Scenarios with 100-year Storm Tide Level

Data Sources 


Missing Data

Local Partnership 


​Resources

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​Storm Surge Multimedia


​Hurricane Isaac (2012)

Check out this "negative" storm surge from Hurricane Isaac in Tampa Bay. A "negative" surge occurs when a hurricane pushes water offshore and coastal locations observe water levels below normal. Such conditions can cause problems for industries that rely on water intake or for marinas and ports that rely on water to float ships. Negative surges can also be dangerous for people who wander onto mudflats, only to find water levels rush back to normal, or above normal levels with a shift in the wind.


​Tropical Storm Debby (2012)

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Unnamed Hurricane (1921)

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​Tampa/ St Petersburg U-Surge Team

Hal Needham
Nick McIntyre
Shanna Haley
© 2017 Marine Weather & Climate. All rights reserved.
  • Home
  • About
  • U.S. Cities
    • US Atlantic Coast (North) >
      • Rhode Island >
        • Newport
        • Providence
      • Massachusetts >
        • Boston
      • Connecticut >
        • New London/ Groton
      • New Jersey >
        • Cape May
        • Atlantic_City
        • Sandy Hook/ North Jersey
      • New York >
        • New York City
    • U.S. Gulf Coast >
      • Texas >
        • South Padre Island
        • Corpus Christi
      • Mississippi
      • Alabama
      • Florida
  • Contact