Rm. Wakimoto et Pg. Black, DAMAGE SURVEY OF HURRICANE-ANDREW AND ITS RELATIONSHIP TO THE EYEWALL, Bulletin of the American Meteorological Society, 75(2), 1994, pp. 189-200
A damage map documenting Hurricane Andrew's destructive landfall over
southern Florida is presented. Vectors that represent the direction of
winds causing damage to trees and structures are shown along with an
F-scale rating in order to assess the strength of the near-surface win
ds. It is hypothesized that increased surface roughness once the hurri
cane made landfall may have contributed to a surface wind enhancement
resulting in the strongest winds ever estimated (F3) for a landfall hu
rricane. This intense damage occurred primarily during the 'second' pe
riod of strong winds associated with the east side of the eyewall. For
the first time, a well-defined circulation in the damage pattern by t
he second wind was documented. A superposition of radar data from Miam
i and Key West on top of the damage map provides the first detailed ex
amination of the relationship between the eyewall and the surface flow
field as estimated from the damage vectors.