2000 ◽  
Author(s):  
Hans C. Graber ◽  
Mark A. Donelan ◽  
William M. Drennan ◽  
Fred W. Dobson

2021 ◽  
Vol 9 (2) ◽  
pp. 214
Author(s):  
Adam C. Brown ◽  
Robert K. Paasch

A spherical wave measurement buoy capable of detecting breaking waves has been designed and built. The buoy is 16 inches in diameter and houses a 9 degree of freedom inertial measurement unit (IMU). The orientation and acceleration of the buoy is continuously logged at frequencies up to 200 Hz providing a high fidelity description of the motion of the buoy as it is impacted by breaking waves. The buoy was deployed several times throughout the winter of 2013–2014. Both moored and free-drifting data were acquired in near-shore shoaling waves off the coast of Newport, OR. Almost 200 breaking waves of varying type and intensity were measured over the course of multiple deployments. The characteristic signature of spilling and plunging breakers was identified in the IMU data.


Author(s):  
Suzanne M. Lea ◽  
Matthew Lybanon ◽  
Peter M. Smith
Keyword(s):  

2006 ◽  
Vol 53 (1) ◽  
pp. 81-92 ◽  
Author(s):  
Emanuele Terrile ◽  
Ad J.H.M. Reniers ◽  
Marcel J.F. Stive ◽  
Maarten Tromp ◽  
Henk Jan Verhagen

Author(s):  
John P. Dugan ◽  
Cindy C. Piotrowski ◽  
J. Zandy Williams ◽  
K. Todd Holland
Keyword(s):  

2017 ◽  
Vol 47 (8) ◽  
pp. 2115-2122 ◽  
Author(s):  
Jamie MacMahan

AbstractDrag coefficients Cd obtained through direct eddy covariance estimates of the wind stress were observed at four different sandy beaches with dissipative surfzones along the coastline of Monterey Bay, California. The measured surfzone Cd (~2 × 10−3) is twice as large as open-ocean estimates and consistent with recent estimates of Cd over the surfzone and shoaling region. Owing to the heterogeneous nature of the near shore consisting of nonbreaking shoaling waves and breaking surfzone waves, the surfzone wind stress source region is estimated from the footprint probability distribution derived for stable and unstable atmospheric conditions. An empirical model developed for estimating the Cd for open-ocean foam coverage dependent on wind speed is modified for foam coverage owing to depth-limited wave breaking within the surfzone. A modified empirical Cd model for surfzone foam predicts similar values as the measured Cd and provides an alternative mechanism to describe roughness.


Author(s):  
M. W. Griffiths ◽  
W. J. Easson ◽  
C. A. Greated
Keyword(s):  

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