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Coastal Flood Forecasting at TAMU-CC/TCOON. Dr. Philippe Tissot ptissot@cbi.tamucc.edu. Dr. Patrick R. Michaud pmichaud@sci.tamucc.edu. Collaborators:. Dr. Daniel Cox, Dr. Alex Sadovski, Scott Duff, Jessica Tishmack, Deidre Williams, Zack Bowles,
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Coastal Flood Forecastingat TAMU-CC/TCOON Dr. Philippe Tissot ptissot@cbi.tamucc.edu Dr. Patrick R. Michaud pmichaud@sci.tamucc.edu Collaborators: Dr. Daniel Cox, Dr. Alex Sadovski, Scott Duff, Jessica Tishmack, Deidre Williams, Zack Bowles, Aimee Mostella, Jeremy Stearns, Kelly Torres, Alex Drikitis January 30, 2003
TCOON overview • Started 1988 • Over 50 stations • Primary Sponsors • General Land Office • Water Devel. Board • US Corps of Eng • Nat'l Ocean Service Gulf of Mexico
TCOON overview • Measurements • Precise Water Levels • Wind • Temperature • Barometric Pressure • Follows NOAA/NOS standards • Real-time, online database
Wind anemometer Radio Antenna Satellite Transmitter Solar Panels Data Collector Water Level Sensor Water Quality Sensor Current Meter Typical TCOON station
Other real-time observing systems • Real-time Navigation • Port of Corpus Christi • Port Freeport • NOAA PORTS • Water-Quality • Nueces Bay Salinity • Oso Creek Dissolved Oxygen • Offshore Weather
Data management design principles • Preserve source data • Annotate instead of modify • Automate as much as possible • Maintain a standard interchange format • Avoid complex or proprietary components • Emphasize long-term reliability over short-term costs
Uses of observation data • Tidal Datums • Littoral Boundaries • Oil-Spill Response • Navigation • Storm Preparation/ Response • Research
Water-level prediction …what will happen next?
Tide predictions tide: The periodic rise and fall of a body of water resulting from gravitational interactions between Sun, Moon, and Earth. Tide and Current Glossary, National Ocean Service, 2000 According to NOS, changes in water level from non-gravitational forces are not “tides”.
Harmonic analysis • Standard method for tide predictions • Represented by constituent cosine waves with known frequencies based on gravitational (periodic) forces • Elevation of water is modeled as h(t) = H0 + Hc fy,c cos(act + ey,c – kc) h(t) = elevation of water at time t H0 = datum offset ac = frequency (speed) of constituent t fy,c ey,c = node factors/equilibrium args Hc = amplitude of constituent c kc = phase offset for constituent c
Harmonic tide predictions To predict tides using harmonic analysis: • Obtain amplitudes and phases of harmonic constituents from trusted sources (e.g., NOS) or • Perform a least-squares analysis on observations to determine amplitudes and phases of harmonic constituents
Harmonic prediction Apply the amplitudes/phases to get:
Prediction vs. observation It’s nice when it works…
Prediction vs. observation …but it often doesn’t work in Texas
Water level != tide In Texas, meteorological factors have a significant effect on water elevations
Uses of harmonic predictions However, harmonic predictions can still be useful! Consider… Isidore begins to (re-)enter the Gulf… …what will happen next?
Uses of harmonic predictions If we add harmonic prediction… …what will happen next?
Uses of harmonic prediction landfall
Isidore & JFK Causeway • Effect of Isidore at JFK causeway
Harmonic WL prediction -present capabilities • Automated system for computing harmonic constituent values from observations database • Harmonic predictions available via query page for many TCOON stations
Harmonic WL prediction –(near) future capabilities • Persistent model forecast • Apply difference between latest observation and harmonic prediction to future predictions • Forecasts page on DNR web site • Obtain forecasts from different models • Harmonic predictions • Persistent model • Neural-network model • Linear-regression/statistical model • Hybrid models • Information about water-level forecasting methods • Statistics on previous forecasts
Neural-network forecasts Dr. Philippe Tissot