A revised hurricane pressure-wind model

A new technique for relating central pressure and maximum winds in tropical cyclones is presented, together with a method of objectively determining a derivative of the Holland b parameter, bs, which relates directly to surface winds and varies with the pressure drop into the cyclone center, intensi...

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Published in:Monthly Weather Review
Other Authors: Holland, Greg (author)
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2008
Subjects:
Online Access:http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-119
https://doi.org/10.1175/2008MWR2395.1
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spelling ftncar:oai:drupal-site.org:articles_6547 2023-07-30T04:05:18+02:00 A revised hurricane pressure-wind model Holland, Greg (author) 2008-09-01 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-119 https://doi.org/10.1175/2008MWR2395.1 en eng American Meteorological Society Monthly Weather Review http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-119 doi:10.1175/2008MWR2395.1 ark:/85065/d7g44qgb Copyright 2008 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be "fair use" under Section 107 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Law (17 USC, as revised by P.L. 94-553) does not require the Society's permission. Republication, systematic reproduction, posting in electronic form on servers, or other uses of this material, except as exempted by the above statements, requires written permission or license from the AMS. Additional details are provided in the AMS Copyright Policies, available from the AMS at 617-227-2425 or amspubs@ametsoc.org. Permission to place a copy of this work on this server has been provided by the AMS. The AMS does not guarantee that the copy provided here is an accurate copy of the published work. Model evaluation/performance Text article 2008 ftncar https://doi.org/10.1175/2008MWR2395.1 2023-07-17T18:37:29Z A new technique for relating central pressure and maximum winds in tropical cyclones is presented, together with a method of objectively determining a derivative of the Holland b parameter, bs, which relates directly to surface winds and varies with the pressure drop into the cyclone center, intensification rate, latitude, and translation speed. By allowing this bs parameter to vary, a realistic scatter in maximum winds for a given central pressure is obtained. This provides an improvement over traditional approaches that provide a unique wind for each central pressure. It is further recommended that application of the Dvorak satellite-interpretation technique be changed to enable a direct derivation of central pressure. The pressure-wind model derived here can then provide the maximum wind estimates. The recent North Atlantic data archive is shown to be largely derived from the use of the Dvorak technique, even when hurricane reconnaissance data are available and Dvorak overestimates maximum winds in this region for the more intense hurricanes. Application to the full North Atlantic hurricane archive confirms the findings by Landsea (1993) of a substantial overestimation of maximum winds between 1950 and 1980; the Landsea corrections do not completely remove this bias. Article in Journal/Newspaper North Atlantic OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Monthly Weather Review 136 9 3432 3445
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
topic Model evaluation/performance
spellingShingle Model evaluation/performance
A revised hurricane pressure-wind model
topic_facet Model evaluation/performance
description A new technique for relating central pressure and maximum winds in tropical cyclones is presented, together with a method of objectively determining a derivative of the Holland b parameter, bs, which relates directly to surface winds and varies with the pressure drop into the cyclone center, intensification rate, latitude, and translation speed. By allowing this bs parameter to vary, a realistic scatter in maximum winds for a given central pressure is obtained. This provides an improvement over traditional approaches that provide a unique wind for each central pressure. It is further recommended that application of the Dvorak satellite-interpretation technique be changed to enable a direct derivation of central pressure. The pressure-wind model derived here can then provide the maximum wind estimates. The recent North Atlantic data archive is shown to be largely derived from the use of the Dvorak technique, even when hurricane reconnaissance data are available and Dvorak overestimates maximum winds in this region for the more intense hurricanes. Application to the full North Atlantic hurricane archive confirms the findings by Landsea (1993) of a substantial overestimation of maximum winds between 1950 and 1980; the Landsea corrections do not completely remove this bias.
author2 Holland, Greg (author)
format Article in Journal/Newspaper
title A revised hurricane pressure-wind model
title_short A revised hurricane pressure-wind model
title_full A revised hurricane pressure-wind model
title_fullStr A revised hurricane pressure-wind model
title_full_unstemmed A revised hurricane pressure-wind model
title_sort revised hurricane pressure-wind model
publisher American Meteorological Society
publishDate 2008
url http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-119
https://doi.org/10.1175/2008MWR2395.1
genre North Atlantic
genre_facet North Atlantic
op_relation Monthly Weather Review
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-119
doi:10.1175/2008MWR2395.1
ark:/85065/d7g44qgb
op_rights Copyright 2008 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be "fair use" under Section 107 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Law (17 USC, as revised by P.L. 94-553) does not require the Society's permission. Republication, systematic reproduction, posting in electronic form on servers, or other uses of this material, except as exempted by the above statements, requires written permission or license from the AMS. Additional details are provided in the AMS Copyright Policies, available from the AMS at 617-227-2425 or amspubs@ametsoc.org. Permission to place a copy of this work on this server has been provided by the AMS. The AMS does not guarantee that the copy provided here is an accurate copy of the published work.
op_doi https://doi.org/10.1175/2008MWR2395.1
container_title Monthly Weather Review
container_volume 136
container_issue 9
container_start_page 3432
op_container_end_page 3445
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