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James G. Herterich

Other affiliations: University of Oxford
Bio: James G. Herterich is an academic researcher from University College Dublin. The author has contributed to research in topics: Breaking wave & Bathymetry. The author has an hindex of 8, co-authored 18 publications receiving 123 citations. Previous affiliations of James G. Herterich include University of Oxford.

Papers
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Journal ArticleDOI
TL;DR: In this paper, the authors describe mechanisms by which hydraulic fracture creates boulders from cliffs and bedrock platforms, and determine a condition for fracture, relating the fluid pressure, loaded area, fracture stress, microcrack position and geometry.

32 citations

Journal ArticleDOI
TL;DR: In this article, the authors show that the Nott-approach wave-height calculations are unreliable and that direct relationships cannot be established between boulder measurements and wave heights. And they further demonstrate that Nott Approach equations are incapable of distinguishing storm waves from tsunami transport and that wave heights hindcast from boulder masses are not meaningful.
Abstract: Coastal boulder deposits (CBD), transported by waves at elevations above sea level and substantial distances inland, are markers for marine incursions. Whether they are tsunami or storm deposits can be difficult to determine, but this is of critical importance because of the role that CBD play in coastal hazard analysis. Equations from seminal work by Nott (1997), here referred to as the Nott Approach, are commonly employed to calculate nominal wave heights from boulder masses as a means to discriminate between emplacement mechanisms. Systematic review shows that this approach is based on assumptions that are not securely founded and that direct relationships cannot be established between boulder measurements and wave heights. A test using an unprecedented dataset of boulders moved by storm waves (with associated sea-state data) shows a lack of agreement between calculations and actual wave heights. The equations return unrealistically large heights, many of which greatly exceed sea states occurring during the boulder-moving storms. This underscores the finding that Nott-Approach wave-height calculations are unreliable. The result is general, because although the field data come from one region (the Aran Islands, Ireland), they represent a wide range of boulder masses and topographic settings and present a valid test of hydrodynamic equations. This analysis demonstrates that Nott Approach equations are incapable of distinguishing storm waves from tsunami transport and that wave heights hindcast from boulder masses are not meaningful. Current hydrodynamic understanding does not permit reliable computation of wave height from boulder measurements. A combination of field, numerical, and experimental approaches is required to quantify relationships between wave power and mass transport onshore. Many CBD interpreted as tsunami deposits based on Nott-Approach analysis may in fact have been emplaced during storms and should therefore be re-evaluated. This is especially important for CBD that have been incorporated into long-term coastal risk assessments, which are compromised if the CBD are misinterpreted. CBD dynamics can be better determined from a combination of detailed field measurements, modeling, and experiments. A clearer understanding of emplacement mechanisms will result in more reliable hazard analysis.

30 citations

Journal ArticleDOI
TL;DR: Analysis of nearshore waves observed during two major North–East Atlantic storms in 2015 and 2017 reveals that modulational instabilities are ineffective, third-order resonances negligible and the largest waves observed here have characteristics quite similar to those displayed by rogue waves for which second order bound nonlinearities are the principal factor that enhances the linear dispersive focusing of extreme waves.
Abstract: We present a statistical analysis of nearshore waves observed during two major North–East Atlantic storms in 2015 and 2017. Surface elevations were measured with a 5-beam acoustic Doppler current profiler (ADCP) at relatively shallow waters off the west coast of Ireland. To compensate for the significant variability of both sea states in time, we consider a novel approach for analyzing the non-stationary surface-elevation series and compare the distributions of crest and wave heights observed with theoretical predictions based on the Forristall, Tayfun and Boccotti models. In particular, the latter two models have been largely applied to and validated for deep-water waves. We show here that they also describe well the characteristics of waves observed in relatively shallow waters. The largest nearshore waves observed during the two storms do not exceed the rogue thresholds as the Draupner, Andrea, Killard or El Faro rogue waves do in intermediate or deep-water depths. Nevertheless, our analysis reveals that modulational instabilities are ineffective, third-order resonances negligible and the largest waves observed here have characteristics quite similar to those displayed by rogue waves for which second order bound nonlinearities are the principal factor that enhances the linear dispersive focusing of extreme waves.

22 citations

Journal ArticleDOI
TL;DR: In this paper, the authors investigated the evolution of wave packets towards a vertical wall over a varying bathymetry with a one-dimensional conformal-mapping spectral code, and highlighted wave breaking, runup and reflection, wave interference and bathymetric effects.
Abstract: Recent modelling work has shown that abrupt bathymetric transitions can produce dramatic amplifications of long waves, under the influence of both nonlinearity and dispersion. Here, the evolution of wave packets towards a vertical wall over a varying bathymetry is investigated with a one-dimensional conformal-mapping spectral code. In this system, wave breaking, runup and reflection, wave interference and bathymetric effects are highlighted. Wave breaking is examined with respect to geometric, kinematic and energetic conditions, with consistent results. The breaking strength is characterized for spilling and plunging based on initial wave period and amplitude. Non-breaking waves are amplified by reflection, interference and the bathymetry leading to large runups. In a typical example inspired by a real-world bathymetry, the maximum runup amplification approaches a factor of 12 – large enough for a 3 m amplitude wave to overtop a 30 m cliff.

16 citations

Journal ArticleDOI
TL;DR: In this paper, the authors analyze the transport of a dilute suspension of particles through a channel with porous walls accounting for the concentration dependence of the viscosity and show that a pessimal distribution width exists that maximizes the required hydrodynamic pressure for a constant fluid influx.
Abstract: We analyse the transport of a dilute suspension of particles through a channel with porous walls accounting for the concentration dependence of the viscosity. Two cases of leakage flow of fluid through the porous channel walls are studied: (i) constant flux, and (ii) dependent on the pressure drop across the wall. The effect of mixing the suspension first compared with point injection is examined by considering inlet concentration distributions of different widths. We find that a pessimal distribution width exists that maximizes the required hydrodynamic pressure for a constant fluid influx. We also show that the presence of an osmotic pressure may lead to fluid being sucked into the channel. We consider how the application of an external hydrodynamic pressure affects this observation and discuss the significance of our results for water filtration.

11 citations


Cited by
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Book
01 Sep 1992

119 citations

Book
17 Apr 2007
TL;DR: The first Applied Solid Mechanics Conference as mentioned in this paper was held in Glasgow, UK, 26-27 March 1985, with a focus on the application of solid mechanics to the aerospace domain, and
Abstract: Proceedings of the first Applied Solid Mechanics Conference, Glasgow, UK, 26-27 March 1985.

57 citations

Journal ArticleDOI
TL;DR: In this paper, the progress made since the first wave energy control systems were suggested in the 1970s, and examines current outstanding challenges for the control community, and discusses the potential of wave energy to provide a carbon-free solution to the world's increasing appetite for energy.

34 citations