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to the f plane, but including the β term will not increase the mathematical complexity. Fig . 2. Schematic map of the incidence and reflection of an offshore pressure signal and the definition of variables; θ is the angle between the wave crest line and the isobath, i.e., the incidence angle toward the coast. For an offshore signal in the form of a single Fourier component, η ^ in ( y ) e − i ω t , a solution of (2) can be sought of the form: (3) η ( x , y , t ) = η ^ ( x , y ) e
to the f plane, but including the β term will not increase the mathematical complexity. Fig . 2. Schematic map of the incidence and reflection of an offshore pressure signal and the definition of variables; θ is the angle between the wave crest line and the isobath, i.e., the incidence angle toward the coast. For an offshore signal in the form of a single Fourier component, η ^ in ( y ) e − i ω t , a solution of (2) can be sought of the form: (3) η ( x , y , t ) = η ^ ( x , y ) e
