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AGU: Geophysical Research Letters

 

Index Terms

  • Biogeosciences: Climate dynamics
  • Global Change: Impacts of global change
  • Atmospheric Processes: Climate change and variability
  • Atmospheric Processes: Tropical meteorology
  • Nonlinear Geophysics: Probability distributions, heavy and fat-tailed

Abstract

Estimated return periods for Hurricane Katrina

J. B. Elsner

Department of Geography, Florida State University, Tallahassee, Florida, USA

T. H. Jagger

Department of Geography, Florida State University, Tallahassee, Florida, USA

A. A. Tsonis

Atmospheric Sciences Group, Department of Mathematical Sciences, University of Wisconsin-Milwaukee, Milwaukee, Wisconsin, USA

Hurricane Katrina is one of the most destructive natural disaster in U.S. history. The infrequency of severe coastal hurricanes implies that empirical probability estimates of the next big one will be unreliable. Here we use an extreme-value model together with interpolated best-track (HURDAT) records to show that a hurricane of Katrina's intensity or stronger can be expected to occur, on average, once every 21 years somewhere along the Gulf coast from Texas through Alabama and once every 14 years somewhere along the entire coast from Texas through Maine. The model predicts a 100-year return level of 83 ms−1 (186 mph) during globally warm years and 75 ms−1 (168 mph) during globally cool years. This difference is consistent with models predicting an increase in hurricane intensity with increasing greenhouse warming.

Received 10 December 2005; accepted 9 March 2006; published 19 April 2006.

Citation: Elsner, J. B., T. H. Jagger, and A. A. Tsonis (2006), Estimated return periods for Hurricane Katrina, Geophys. Res. Lett., 33, L08704, doi:10.1029/2005GL025452.

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