This is a result of its close proximity to the amphidromic point outside Eigersund.
2.
A point within a tidal system where the tidal range is almost zero is called an amphidromic point.
3.
High water rotates about the amphidromic point once every 12 hours in the direction of rising cotidal lines, and away from ebbing cotidal lines.
4.
Oceanic tides actually rotate around the ocean basins as vast " gyres " around several " amphidromic points " where no tide exists.
5.
In the North Atlantic, because the cotidal lines circulate counterclockwise around the amphidromic point, the high tide passes New York Harbor approximately an hour ahead of Norfolk Harbor.
6.
Each tidal constituent has a different pattern of amplitudes, phases, and amphidromic points, so the " M " 2 patterns cannot be used for other tide components.
7.
The lines rotate around the amphidromic points counterclockwise in the northern hemisphere so that from Baja California Peninsula to Alaska and from France to Ireland the " M " 2 tide propagates northward.
8.
For an ocean in the shape of a circular basin enclosed by a coastline, the " cotidal lines " point radially inward and must eventually meet at a common point, the amphidromic point.
9.
For a semi-diurnal tide the amphidromic point can be thought of roughly like the center of a clock face, with the hour hand pointing in the direction of the high water cotidal line, which is directly opposite the low water cotidal line.
10.
The islands of Madagascar and New Zealand are amphidromic points in the sense that the tide goes around them ( counterclockwise in both cases ) in about 12 and a half hours, but the amplitude of the tides on their coasts is in some places large.
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