OceanSprint
Well-Known Member
The 2 lumps of water with the earth spinning below them creates 2 OCEAN tides each day. For the uk continental shelf, these 2 tides occur along the shelf edge. These in turn drive the co-oscilating tides of our shelf waters with the sea on the continental shelf oscillating like a guitar string, with nodes (places with small tidal range) and antinodes (places with large tidal range) trouble is the guitar string us actually a 2d sheet. Coriollis is then involved in placing the nodes and antinodes.
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