Hence, a more phenomological approach is usually applied to classify wave shape (e.g., elevated, leading depressed, N-wave etc). In the context of previous work, I2I2 has been evaluated numerically but not experimentally (e.g., Klettner and Eames, 2012). In this study it is proposed to obtain experimental measures of I2I2. The main purpose of this paper is to describe a new experimental study that analyses the correlation between runup and wave shape, characterised in terms of energy, amplitude, and wavelength.

This experimental methodology is described in Section 3. This is followed by a comprehensive description of the statistical tools used to analyse the datasets and explore the dependence of Sirolimus purchase runup on wavelength and shape. Within this study it is argued that the submerged beach length is a more appropriate parameter than water depth

for the normalisation of the wavelength for wave classification – as also noted in the theoretical work from Madsen and Schaffer (2010), prior to the analysis and determination of runup regimes. Such a parameter provides an indication of the level of interaction of the wave with the beach. Indeed, processes such as shoaling, reflections, selleck inhibitor and relative bottom friction will be affected by the relative length of the wave, therefore it is expected that the dynamics of runup will also be. The outcomes of the experimental runup study, in terms of empirical closures, are described in Section 4 along with a supporting physical explanation of the correlation groups. Conclusions are drawn in Section 5. Early studies attempted

to find a relationship between runup, wave height and wavelength for periodic waves incident on a beach (Kaplan, 1955, Shuto, 1967 and Togashi, 1981), but no consistent trend developed, as highlighted by Synolakis (1986). The runup of propagating waves has been investigated analytically and numerically by using the momentum equations (Carrier and Greenspan, 1958, Kobayashi et al., 1990 and Zelt, 1991), and also in the laboratory. The most widely used runup relationships found in the literature (Eqs. (2)–(6)), are listed in Table 1. These studies focus specifically on run up over impermeable beds and are discussed in greater detail below. In this paper, h STK38   refers to water depth, H   refers to the wave height (trough-to-peak), and cotβcotβ refers to the slope of the beach ( Fig. 1). Most runup studies have considered a single positively elevated wave running-up a beach with a constant slope, and have looked at the influence of wave amplitude on runup. This is because many of these waves are weakly dispersive and do not significantly change shape as they propagate along a flume to the beach. The experimental waves generated in past studies tend to resemble solitary waves, are unidirectional, and propagate over a constant depth region.