Using new large-scale wave-flume experiments we examine the cross-section and planform geometry of wave-formed ripples in coarse sand (median grain size D
50 = 430 μm) under high-energy shoaling and plunging random waves. We find that the ripples remain orbital for the full
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Using new large-scale wave-flume experiments we examine the cross-section and planform geometry of wave-formed ripples in coarse sand (median grain size D
50 = 430 μm) under high-energy shoaling and plunging random waves. We find that the ripples remain orbital for the full range of encountered conditions, even for wave forcing when in finer sand the ripple length λ
r is known to become independent of the near-bed orbital diameter d
s (anorbital ripples). The proportionality between λ
r and d
s is not constant, but decreases from about 0.55 for d
s / D
50 ≈ 1400 to about 0.27 for d
s / D
50 ≈ 11 , 500 . Analogously, ripple height η
r increases with d
s, but the constant of proportionally decreases from about 0.08 for d
s / D
50 ≈ 1400 to about 0.02 for d
s / D
50 > 8000 . In contrast to earlier observations of coarse-grained two-dimensional wave ripples under mild wave conditions, the ripple planform changes with the wave Reynolds number from quasi two-dimensional vortex ripples, through oval mounds with ripples attached from different directions, to strongly subdued hummocky-type features. Finally, we combine our data with existing mild-wave coarse-grain ripple data to develop new equilibrium predictors for ripple length, height and steepness suitable for a wide range of wave conditions and a D
50 larger than about 300 μm.
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