Ap-12 – Furuno CI-68 User Manual

Page 68

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PRINCIPLE OF OPERATION

AP-12

Tide differential calculations in water tracking mode

Tide speeds of layer A (C1) and layer B (C2) relative to near-surface layer (Vw) are
calculated as follows:

Tide differential based on layer A (speed of layer B as viewed from layer A)
D1 = Vw - Vwa (Speed of layer A based on near-surface layer)
D2 = Vw - Vwb (Speed of layer B based on near-surface layer)

The tide differential (Dd) between layers A and layer B is;

Dd = D2 - D1

= (Vw - Vwb) - (Vw - Vwa)

= Vwa - Vwb

= 8 - 5

= 3 (kt)


OR

Tide differential based on layer B (speed of layer A as viewed from layer B)
Dd = D1 - D2

= (Vw - Vwa) - (Vw - Vwb)

= Vwa - Vwb

= 5 - 8

= -3 (kt)

If you compare the results of calculations on this page with the ones on preceding pages,
you will find the tide differential of two layers is identical irrespective of tracking mode.



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