A Reanalysis of Hurricane Andrew's IntensitySource: Bulletin of the American Meteorological Society:;2004:;volume( 085 ):;issue: 011::page 1699Author:Landsea, Christopher W.
,
Franklin, James L.
,
McAdie, Colin J.
,
Beven, John L.
,
Gross, James M.
,
Jarvinen, Brian R.
,
Pasch, Richard J.
,
Rappaport, Edward N.
,
Dunion, Jason P.
,
Dodge, Peter P.
DOI: 10.1175/BAMS-85-11-1699Publisher: American Meteorological Society
Abstract: Hurricane Andrew of 1992 caused unprecedented economic devastation along its path through the Bahamas, southeastern Florida, and Louisiana. Damage in the United States was estimated to be $26 billion (in 1992 dollars), making Andrew one of the most expensive natural disasters in U.S. history. This hurricane struck southeastern Florida with maximum 1-min surface winds estimated in a 1992 poststorm analysis at 125 kt (64 m s?1). This original assessment was primarily based on an adjustment of aircraft reconnaissance flight-level winds to the surface. Based on recent advancements in the understanding of the eyewall wind structure of major hurricanes, the official intensity of Andrew was adjusted upward for five days during its track across the Atlantic Ocean and Gulf of Mexico by the National Hurricane Center Best Track Change Committee. In particular, Andrew is now assessed by the National Hurricane Center to be a Saffir?Simpson Hurricane Scale category-5 hurricane (the highest intensity category possible) at its landfall in southeastern Florida, with maximum 1-min winds of 145 kt (75 m s?1). This makes Andrew only the third category-5 hurricane to strike the United States since at least 1900. Implications for how this change impacts society's planning for such extreme events are discussed.
|
Collections
Show full item record
contributor author | Landsea, Christopher W. | |
contributor author | Franklin, James L. | |
contributor author | McAdie, Colin J. | |
contributor author | Beven, John L. | |
contributor author | Gross, James M. | |
contributor author | Jarvinen, Brian R. | |
contributor author | Pasch, Richard J. | |
contributor author | Rappaport, Edward N. | |
contributor author | Dunion, Jason P. | |
contributor author | Dodge, Peter P. | |
date accessioned | 2017-06-09T16:42:24Z | |
date available | 2017-06-09T16:42:24Z | |
date copyright | 2004/11/01 | |
date issued | 2004 | |
identifier issn | 0003-0007 | |
identifier other | ams-72649.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4214675 | |
description abstract | Hurricane Andrew of 1992 caused unprecedented economic devastation along its path through the Bahamas, southeastern Florida, and Louisiana. Damage in the United States was estimated to be $26 billion (in 1992 dollars), making Andrew one of the most expensive natural disasters in U.S. history. This hurricane struck southeastern Florida with maximum 1-min surface winds estimated in a 1992 poststorm analysis at 125 kt (64 m s?1). This original assessment was primarily based on an adjustment of aircraft reconnaissance flight-level winds to the surface. Based on recent advancements in the understanding of the eyewall wind structure of major hurricanes, the official intensity of Andrew was adjusted upward for five days during its track across the Atlantic Ocean and Gulf of Mexico by the National Hurricane Center Best Track Change Committee. In particular, Andrew is now assessed by the National Hurricane Center to be a Saffir?Simpson Hurricane Scale category-5 hurricane (the highest intensity category possible) at its landfall in southeastern Florida, with maximum 1-min winds of 145 kt (75 m s?1). This makes Andrew only the third category-5 hurricane to strike the United States since at least 1900. Implications for how this change impacts society's planning for such extreme events are discussed. | |
publisher | American Meteorological Society | |
title | A Reanalysis of Hurricane Andrew's Intensity | |
type | Journal Paper | |
journal volume | 85 | |
journal issue | 11 | |
journal title | Bulletin of the American Meteorological Society | |
identifier doi | 10.1175/BAMS-85-11-1699 | |
journal fristpage | 1699 | |
journal lastpage | 1712 | |
tree | Bulletin of the American Meteorological Society:;2004:;volume( 085 ):;issue: 011 | |
contenttype | Fulltext |