Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific

Even though the maximum wind radius (<i>R</i><sub><mo>max</mo></sub>) is an important parameter in determining the intensity and size of tropical cyclones, it has been overlooked in previous storm surge studies. This study reviews the existing estimation methods f...

Full description

Bibliographic Details
Main Authors: H. Takagi, W. Wu
Format: Article
Language:English
Published: Copernicus Publications 2016-03-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/16/705/2016/nhess-16-705-2016.pdf
id doaj-69b433974c8d431ab95dd15255f96542
record_format Article
spelling doaj-69b433974c8d431ab95dd15255f965422020-11-24T22:47:08ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812016-03-0116370571710.5194/nhess-16-705-2016Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North PacificH. Takagi0W. Wu1Tokyo Institute of Technology, Graduate School of Science and Engineering, 2-12-1 Ookayama, Meguro-ku, Tokyo 152-8550, JapanTokyo Institute of Technology, Graduate School of Science and Engineering, 2-12-1 Ookayama, Meguro-ku, Tokyo 152-8550, JapanEven though the maximum wind radius (<i>R</i><sub><mo>max</mo></sub>) is an important parameter in determining the intensity and size of tropical cyclones, it has been overlooked in previous storm surge studies. This study reviews the existing estimation methods for <i>R</i><sub><mo>max</mo></sub> based on central pressure or maximum wind speed. These over- or underestimate <i>R</i><sub><mo>max</mo></sub> because of substantial variations in the data, although an average radius can be estimated with moderate accuracy. As an alternative, we propose an <i>R</i><sub><mo>max</mo></sub> estimation method based on the radius of the 50 kt wind (<i>R</i><sub>50</sub>). Data obtained by a meteorological station network in the Japanese archipelago during the passage of strong typhoons, together with the JMA typhoon best track data for 1990–2013, enabled us to derive the following simple equation, <i>R</i><sub><mo>max</mo></sub>  =  0.23 <i>R</i><sub>50</sub>. Application to a recent strong typhoon, the 2015 Typhoon Goni, confirms that the equation provides a good estimation of <i>R</i><sub><mo>max</mo></sub>, particularly when the central pressure became considerably low. Although this new method substantially improves the estimation of <i>R</i><sub><mo>max</mo></sub> compared to the existing models, estimation errors are unavoidable because of fundamental uncertainties regarding the typhoon's structure or insufficient number of available typhoon data. In fact, a numerical simulation for the 2013 Typhoon Haiyan as well as 2015 Typhoon Goni demonstrates a substantial difference in the storm surge height for different <i>R</i><sub><mo>max</mo></sub>. Therefore, the variability of <i>R</i><sub><mo>max</mo></sub> should be taken into account in storm surge simulations (e.g., <i>R</i><sub><mo>max</mo></sub>  =  0.15 <i>R</i><sub>50</sub>–0.35 <i>R</i><sub>50</sub>), independently of the model used, to minimize the risk of over- or underestimating storm surges. The proposed method is expected to increase the predictability of major storm surges and to contribute to disaster risk management, particularly in the western North Pacific, including countries such as Japan, China, Taiwan, the Philippines, and Vietnam.http://www.nat-hazards-earth-syst-sci.net/16/705/2016/nhess-16-705-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H. Takagi
W. Wu
spellingShingle H. Takagi
W. Wu
Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific
Natural Hazards and Earth System Sciences
author_facet H. Takagi
W. Wu
author_sort H. Takagi
title Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific
title_short Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific
title_full Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific
title_fullStr Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific
title_full_unstemmed Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific
title_sort maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western north pacific
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2016-03-01
description Even though the maximum wind radius (<i>R</i><sub><mo>max</mo></sub>) is an important parameter in determining the intensity and size of tropical cyclones, it has been overlooked in previous storm surge studies. This study reviews the existing estimation methods for <i>R</i><sub><mo>max</mo></sub> based on central pressure or maximum wind speed. These over- or underestimate <i>R</i><sub><mo>max</mo></sub> because of substantial variations in the data, although an average radius can be estimated with moderate accuracy. As an alternative, we propose an <i>R</i><sub><mo>max</mo></sub> estimation method based on the radius of the 50 kt wind (<i>R</i><sub>50</sub>). Data obtained by a meteorological station network in the Japanese archipelago during the passage of strong typhoons, together with the JMA typhoon best track data for 1990–2013, enabled us to derive the following simple equation, <i>R</i><sub><mo>max</mo></sub>  =  0.23 <i>R</i><sub>50</sub>. Application to a recent strong typhoon, the 2015 Typhoon Goni, confirms that the equation provides a good estimation of <i>R</i><sub><mo>max</mo></sub>, particularly when the central pressure became considerably low. Although this new method substantially improves the estimation of <i>R</i><sub><mo>max</mo></sub> compared to the existing models, estimation errors are unavoidable because of fundamental uncertainties regarding the typhoon's structure or insufficient number of available typhoon data. In fact, a numerical simulation for the 2013 Typhoon Haiyan as well as 2015 Typhoon Goni demonstrates a substantial difference in the storm surge height for different <i>R</i><sub><mo>max</mo></sub>. Therefore, the variability of <i>R</i><sub><mo>max</mo></sub> should be taken into account in storm surge simulations (e.g., <i>R</i><sub><mo>max</mo></sub>  =  0.15 <i>R</i><sub>50</sub>–0.35 <i>R</i><sub>50</sub>), independently of the model used, to minimize the risk of over- or underestimating storm surges. The proposed method is expected to increase the predictability of major storm surges and to contribute to disaster risk management, particularly in the western North Pacific, including countries such as Japan, China, Taiwan, the Philippines, and Vietnam.
url http://www.nat-hazards-earth-syst-sci.net/16/705/2016/nhess-16-705-2016.pdf
work_keys_str_mv AT htakagi maximumwindradiusestimatedbythe50ktradiusimprovementofstormsurgeforecastingoverthewesternnorthpacific
AT wwu maximumwindradiusestimatedbythe50ktradiusimprovementofstormsurgeforecastingoverthewesternnorthpacific
_version_ 1725682756919230464