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2013
DOI: 10.2112/si65-034.1
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Experimental statistics of long wave runup on a plane beach

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Cited by 9 publications
(11 citation statements)
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“…Pelinovsky [4,8,9], which include the analytical solutions (for non-breaking waves) and the data of laboratory and numerical investigations. The experiments were performed in the Large Wave Flume of the University of Hannover, using a wave flume consisting of a segment with a constant depth h 0 = 3.5 m and length x s = 250 m, adjacent to a plane slope 1 : 6 which was positioned near the right boundary of the flume [3]. The numerical computation in [4] were done using the software package CLAWPACK [10].…”
Section: Numerical Resultsmentioning
confidence: 99%
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“…Pelinovsky [4,8,9], which include the analytical solutions (for non-breaking waves) and the data of laboratory and numerical investigations. The experiments were performed in the Large Wave Flume of the University of Hannover, using a wave flume consisting of a segment with a constant depth h 0 = 3.5 m and length x s = 250 m, adjacent to a plane slope 1 : 6 which was positioned near the right boundary of the flume [3]. The numerical computation in [4] were done using the software package CLAWPACK [10].…”
Section: Numerical Resultsmentioning
confidence: 99%
“…Here the distributions from the work [4] appear to be higher. 2) and |R|/A -in the run-down phases (3,4), computed with the TVD+SPH method (1, 3) and [4] (2, 4); the domain of applicability of the analytical solution [13] is marked by grey color…”
Section: Numerical Resultsmentioning
confidence: 99%
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“…We shall use for clarity the char acteristic sizes of the Large Wave Channel of the Han nover University in Germany with a slope equal to 1 : 6 and a depth of 3.5 m, taking into account that recently a series of experiments on wave run up on a flat beach was performed there [19].…”
Section: Run Up Of a Solitary Wave On A Flat Slope Of The Beachmentioning
confidence: 99%
“…The probabilities of occurrence of different single wave heights are at best approximated either by a Rayleigh (Longuet-Higgins, 1952), Weibull (Forristall, 1978 or Tayfun distribution (Socquet-Juglard et al, 2005). The probability distribution of run-up heights usually follows the relevant distribution for incident wave heights (Denissenko et al, 2011) but can be approximated by a Rayleigh distribution even if the approaching wave field does not represent a Gaussian process (Denissenko et al, 2013). The empirical probabilities of average or significant wave heights in various offshore conditions usually resemble either a Rayleigh or a Weibull distribution (Muraleedharan et al, 2007;Feng et al, 2014), while Pareto-type distributions are more suitable for the analysis of meteotsunami heights (Bechle et al, 2015).…”
Section: Introductionmentioning
confidence: 99%