The Role of Argus in the NCEX Field Experiment Rob Holman SECNAV/CNO Chair in Oceanography
Argus I
Argus II
Argus III
Pixel Instrument Coverage (early test example)
shoreline NCEX Tessellation Array Resolution limited (5 m) 1842 pixels tile
Tessellation Array Locations
Example Directional Spectra
Tessellation Arrays Produce wave directional “spectrum” at any location Extract simple statistics (peak direction?) Use same lag array for depth estimation
NCEX Array, 09/03
NCEX Array, 09/03 (blow-up) Runup “Old” Bathy Line Vbar Tess (alpha and bathy
Longshore Currents (Chris Chickadel)
Orientation for Next Slide
10/31/03, 0700 Variance Image Happy Halloween Rip current
Radiation Stress Gradients where: S xy = Radiation Stress = mean dissipation due to wave breaking = local incident wave angle c = celerity Components in both the longshore and cross-shore directions Concentration on diagonal component S xy Optical techniques necessary for all parameters to allow remote sensing Work of Jason Killian
Fusion with Numerical Models Based on: Wave direction Surf zone width
California Fires, 10/28/03 Mid-afternoon view Southern California
Estimation of Swash Velocities Runup transect from NCEX exp’t, 2004
Two-minute Time Stack NCEX stack, 2003
Band-pass Isolation of Foam
Consecutive Intensity Transects
Analysis Band-pass to isolate foam Hilbert transform to extract phase and wavenumber U = d(phase)/dt * 1/k
Example Sub-stack Results
Example Sub-stack
Example Sub-stack Overlay
Two-minute Sub-stack Example 17 minute run takes 9 seconds
Application of Hilbert Approach to Longshore Currents? (and rips?) Longshore velocity = = 0.60 m/ sec yy tt Duck, NC 0 40 Time (sec) t = 18.7 s y =11.3 m Longshore Distance (m)
Questions? Dr. Aarninkhof Distinguished Argus Scientist Costas Synolakis Oregon State University Wave Tank, 2003