Observations and simulation of winds, surge, and currents on Florida's east coast during hurricane Jeanne (2004)

• Published in: Coastal engineering (Amsterdam) Vol. 60; pp. 84 - 94
• Main Authors: Bacopoulos, Peter, Dally, William R., Hagen, Scott C., Cox, Andrew T.
• Format: Journal Article
• Language: English
• Published: Kidlington Elsevier B.V 01-02-2012; Elsevier
• Subjects: Beaches; Computational fluid dynamics; Computer simulation; Currents; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Engineering geology; Exact sciences and technology; Florida's east coast; Fluid flow; Hurricanes; Hydrodynamics; Marine and continental quaternary; Mathematical models; Modeling; Natural hazards: prediction, damages, etc; Observations; Surficial geology; Surge; Surges; Winds; Florida; United States; Winds; Florida's east coast; Currents; Observations; Modeling; Surge; meteorology; hydrodynamics; digital simulation; North America; tides; coastal environment; beaches; hurricanes; winds; numerical models; piers; prediction; longshore currents; storms
• ISSN: 0378-3839; 1872-7379
• DOI: 10.1016/j.coastaleng.2011.08.010

A novel set of measurements of winds, water levels, and currents recorded in September of 2004 captured the landfall of Hurricane Jeanne. The dataset provides a full picture of the meteorology and hydrodynamics associated with Hurricane Jeanne and are used to test the state-of-the-art in numerical modeling of storm surge. A shallow water equations model (ADCIRC) is driven by rigorously modeled winds and astronomic tides to replicate continuous hydrodynamic records at two stations, one in Melbourne Beach (Spessard) and the other inside Port Canaveral (Trident Pier), where instrumentation was located by happenstance. Simulation results represent the time-series of water surface elevations measured in the open coast off Melbourne Beach (Spessard) within 0.05m root mean square error and within 12% of observed maximum surge elevation (1.35m simulated vs. 1.52m measured) and exhibit details induced by a ‘loop’ performed by the hurricane before it made landfall. Prediction of water levels inside Port Canaveral (Trident Pier) is to within 0.06m root mean square error and includes the observed forerunner and peak surge of the hurricane. In regard to nearshore currents off Melbourne Beach (Spessard), the timing of a sudden switch in the direction of the measured (longshore) current is replicated well with the magnitude of the peak current simulated to within 14% of observation (0.96m/s modeled vs. 1.11m/s measured). The capability to accurately simulate the tidal and storm surge hydrodynamics during Hurricane Jeanne provides confidence in using this class of shallow water equations models in coastal engineering practice.
► Winds, water levels, and currents were measured and modeled for September 2004. ► Observation records for two recording stations included Hurricane Jeanne. ► Wind forcing was provided by rigorously modeled IOKA wind fields. ► Hydrodynamics were modeled by solving the shallow water equations with wind forcing. ► The observations and model results offer an exclusive picture of Hurricane Jeanne.