FORMATION AND EVOLUTION OF BEACH CUSPS UNDER OBLIQUE WAVE CONDITIONS

Author(s):  
ANURAK SRIARIYAWAT ◽  
NICHOLAS DODD
Author(s):  
Arthur Mouragues ◽  
Philippe Bonneton ◽  
Bruno Castelle ◽  
Vincent Marieu

We present field measurements of nearshore currents at a high-energy mesotidal beach with the presence of a 500-m headland and a submerged reef. Small changes in wave forcing and tide elevation were found to largely impact circulation patterns. In particular, under 4-m oblique wave conditions, our measurements indicate the presence of an intense low-frequency fluctuating deflection rip flowing against the headland and extending well beyond the surf zone. An XBeach model is further set up to hindcast such flow patterns.Recorded Presentation from the vICCE (YouTube Link): https://youtu.be/EiqnjBIkWJE


Author(s):  
Nicolas Napp ◽  
Jonathan Pearson ◽  
Tom Bruce ◽  
William Allsop
Keyword(s):  

2008 ◽  
Vol 55 ◽  
pp. 856-860
Author(s):  
Masaya MORI ◽  
Yasuji YAMAMOTO ◽  
Katsutoshi KIMURA ◽  
Shinya WATANABE

2018 ◽  
Vol 85 ◽  
pp. 1236-1240 ◽  
Author(s):  
Woo-Sun Park ◽  
Deokhee Won ◽  
Jihye Seo ◽  
Byeong Wook Lee

Author(s):  
NICOLAS NAPP ◽  
TOM BRUCE ◽  
JONATHAN PEARSON ◽  
WILLIAM ALLSOP
Keyword(s):  

Author(s):  
O.L. Krivanek ◽  
J. TaftØ

It is well known that a standing electron wavefield can be set up in a crystal such that its intensity peaks at the atomic sites or between the sites or in the case of more complex crystal, at one or another type of a site. The effect is usually referred to as channelling but this term is not entirely appropriate; by analogy with the more established particle channelling, electrons would have to be described as channelling either through the channels or through the channel walls, depending on the diffraction conditions.


Author(s):  
Michael W. Bench ◽  
Jason R. Heffelfinger ◽  
C. Barry Carter

To gain a better understanding of the surface faceting that occurs in α-alumina during high temperature processing, atomic force microscopy (AFM) studies have been performed to follow the formation and evolution of the facets. AFM was chosen because it allows for analysis of topographical details down to the atomic level with minimal sample preparation. This is in contrast to SEM analysis, which typically requires the application of conductive coatings that can alter the surface between subsequent heat treatments. Similar experiments have been performed in the TEM; however, due to thin foil and hole edge effects the results may not be representative of the behavior of bulk surfaces.The AFM studies were performed on a Digital Instruments Nanoscope III using microfabricated Si3N4 cantilevers. All images were recorded in air with a nominal applied force of 10-15 nN. The alumina samples were prepared from pre-polished single crystals with (0001), , and nominal surface orientations.


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