amphidromic point sentence in Hindi
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- This is a result of its close proximity to the amphidromic point outside Eigersund.
- A point within a tidal system where the tidal range is almost zero is called an amphidromic point.
- High water rotates about the amphidromic point once every 12 hours in the direction of rising cotidal lines, and away from ebbing cotidal lines.
- Oceanic tides actually rotate around the ocean basins as vast " gyres " around several " amphidromic points " where no tide exists.
- 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.
- 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.
- 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.
- 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.
- 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.
- 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.
- The amphidromic point is at once cotidal with high and low waters, which is satisfied by " zero " tidal motion . ( The rare exception occurs when the tide encircles an island, as it does around New Zealand, Iceland and Madagascar . ) Tidal motion generally lessens moving away from continental coasts, so that crossing the cotidal lines are contours of constant " amplitude " ( half the distance between high and low water ) which decrease to zero at the amphidromic point.
- The amphidromic point is at once cotidal with high and low waters, which is satisfied by " zero " tidal motion . ( The rare exception occurs when the tide encircles an island, as it does around New Zealand, Iceland and Madagascar . ) Tidal motion generally lessens moving away from continental coasts, so that crossing the cotidal lines are contours of constant " amplitude " ( half the distance between high and low water ) which decrease to zero at the amphidromic point.
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