“…The sea surface elevation, q(x, t), of a linear, partially reflected, unidirectional wave on a flat bottom can be expressed as (Dean and Dalrymple 1984) 7(x, t) = a cos(kx -ut) + aK, cos(kx + ot + 0) (1) where a = amplitude of the incident wave, k = wave number, (= 27r/L, where L is wave length) x = horizontal position, a = angular wave frequency (= 27r/T, where T is wave period), t = time, K, = reflection coefficient (= aincident/areflect,•d), and 9 = phase shift due to reflection.…”