Coastal Engineering 2004 2005
DOI: 10.1142/9789812701916_0292
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Development of Stochastic Typhoon Model for Performance Design of Coastal Structures

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Cited by 3 publications
(3 citation statements)
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“…Among several research on stochastic typhoon models, Hashimoto et al (2004) divided typhoons affecting Japan from 1951 to 1999 into five seasons, (a) June and July, (b) August, (c) September, (d) October, and (e) other months, and estimated the parameters, (a) the location of the typhoon center, (b) the central pressure, (c) the radius of maximum wind speed, and their variation with time, in each season in each rectangular cell with a width of 1.5 degrees in longitude and a height of 1.5 degrees in latitude. On this analysis, the radius of maximum wind speed of each typhoon was estimated from the central pressure and the radius of a constant pressure contour on weather maps, provided from the Japan Meteorological Agency.…”
Section: Stochastic Typhoon Model and Future Typhoon Changementioning
confidence: 99%
“…Among several research on stochastic typhoon models, Hashimoto et al (2004) divided typhoons affecting Japan from 1951 to 1999 into five seasons, (a) June and July, (b) August, (c) September, (d) October, and (e) other months, and estimated the parameters, (a) the location of the typhoon center, (b) the central pressure, (c) the radius of maximum wind speed, and their variation with time, in each season in each rectangular cell with a width of 1.5 degrees in longitude and a height of 1.5 degrees in latitude. On this analysis, the radius of maximum wind speed of each typhoon was estimated from the central pressure and the radius of a constant pressure contour on weather maps, provided from the Japan Meteorological Agency.…”
Section: Stochastic Typhoon Model and Future Typhoon Changementioning
confidence: 99%
“…There are several STMs which artificially generate typhoons that can be applied in coastal engineering studies (e.g. Hatada and Yamaguchi, 1996;Kato et al, 2003;Hashimoto et al, 2004;Kawai et al, 2006Kawai et al, , 2008 because STM is useful by statistically estimating typhoons tracks, the central atmospheric pressures and moving speeds and so on. Their simulation areas typically lie to the north of 23N because most of these studies focused on typhoon characteristics around Japan.…”
Section: Introductionmentioning
confidence: 99%
“…Hatada and Yamaguchi, 1996;Kato et al, 2003;Hashimoto et al, 2004;Kawai et al, 2006Kawai et al, , 2008. Their simulation areas are typically higher than 23°N because most of these studies focused on typhoon characteristics around Japan.…”
Section: Introductionmentioning
confidence: 99%