jeff wrote:The following is a paragraph from my post Katrina Report detailing surge effects. You can apply it to Rita as well.
On a personal note, I have been 3 times to SW LA and fully agree cat 1-2 winds were the norm. The surge was impressive however.
Katrina made landfall as a category 3 hurricane yet produced a "category 5" storm surge. Why? The Saffir Simpson scale is based on sustained wind speeds with an indirect correlation with respect to storm surge. Storm surge inundation forecast are compiled from a number of factors and each hurricane landfall is unique. The factors that control storm surge include: the size of the wind field, the intensity of the storm, the duration of the event, the angle of approach to the coast, the depth of the offshore coastal shelf, concavity of the coastline, and special conditions such as storm surge run-up into smaller bays and rivers.
Katrina’s large wind field and category 5 intensity while over the open Gulf of Mexico created a large water level bulge that arrived as a catastrophic storm surge when the hurricane made landfall. The rapid sustained wind speed weakening a few hours before landfall and reduction in Saffir Simpson category did not represent the impending storm surge effectively to the public although preparations were made for a category 5 event. The concavity of the coastal area impacted, the size of the wind field, and the built up water level bulge when Katrina was a category 5 over the open Gulf of Mexico is why Katrina produced such an extreme surge.
Education of the public should be addressed to inform persons in the inundation zones of the different factors involved in storm surge forecast and the potential failures of the Saffir Simpson scale to appropriately predict storm surge levels. Prior to a hurricane landfall, residents should base evacuation and preparation decisions on local NWS forecast of storm surge inundation using computer modeling and experience and not the general Saffir Simpson scale values assigned per category. Large rapidly weakening hurricanes are still likely to bring a large and destructive surge ashore. Additionally, residents at the heads of bays, the mouths of rivers and creeks, and small inlets can receive a substantially higher surge due to water level run-up into an increasingly smaller area. Such affects are unique to a certain coastal location and usually depend heavily on the exact track (ie. MRGO and IHNC surge effects due to track).
Great post, thank you!!!