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...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-03-01
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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 |
Summary: | 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. |
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ISSN: | 1561-8633 1684-9981 |