2008/02/07 by Jennifer L. Irish, Donald T. Resio, Jay J. Ratcliff +1 · 479 citations
Earth and Planetary Sciences · Environmental Science · #Climatology #Environmental science #Flood Risk Assessment and Management #Flood myth #Geography #Geology #Hurricane katrina #Landfall #Meteorology #Natural disaster #Ocean Waves and Remote Sensing #Storm #Storm surge #Surge #Tropical and Extratropical Cyclones Research #Tropical cyclone #Wind speed
paper · pdf · doi:10.1175/2008jpo3727.1
published in Journal of Physical Oceanography 38(9), 2003-2013 (American Meteorological Society)
openalex publication_date 2008/02/07 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/06
Abstract Over the last quarter-century, hurricane surge has been assumed to be primarily a function of maximum storm wind speed, as might be estimated from the Saffir–Simpson hurricane scale. However, Hurricane Katrina demonstrated that wind speed alone cannot reliably describe surge. Herein it is shown that storm size plays an important role in surge generation, particularly for very intense storms making landfall in mildly sloping regions. Prior to Hurricane Katrina, analysis of the historical hurricane record evidenced no clear correlation between surge and storm size, and consequently little attention was given to the role of size in surge generation. In contrast, it is found herein that, for a given intensity, surge varies by as much as 30% over a reasonable range of storm sizes. These findings demonstrate that storm size must be considered when estimating surge, particularly when predicting socioeconomic and flood risk.