EM 1110-2-1100 (Part II)
30 Apr 02
Figure II-6-11. Wave refraction pattern in the vicinity of the Merrimack River Estuary entrance, just
south of the Merrimack Inlet (from Hayes (1971))
(3) To account for a non-sinusoidal character of the prototype flow, Keulegan determined
T Qmax
T Vm Aavg
/ P'
P'
(II-6-14)
πC
πC
and found C varying between 0.81 and 1.0 for K, the filling coefficient, varying between 0.1 and 100. For
practical application, if 0.1 < K < 1.8, use C = 0.86, and for K > 1.8, use C = 1.0.
II-6-14
Hydrodynamics of Tidal Inlets