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| | Hurricanes and the U.S. Gulf Coast: Storm Surge and Flooding |
 | | Storm surge is determined primarily by meteorological forcing (storm intensity, path, and spatial and temporal scales) and topographic parameters (width and slope of the continental shelf, geometry and character of local coastal and shelf features such as barrier islands, headlands, bays, sounds, inlets, marshes, channels, levees, and barriers). |
 | | Storm surge estimates in the 1950s and 1960s were obtained assuming a steady force balance between the onshore wind stress, the water surface slope, and bottom friction. |
 | | Finally, interactions between storm surge and wind wave models are being pursued to allow inclusion of the water surface setup due to gradients in the radiation stress associated with wave breaking, the influence of wave conditions on the air-water drag, and the influence of waves on bottom friction. |
| www.agu.org /report/hurricanes/storm_surge.html (1719 words) |
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