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...
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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 |
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