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The tidal flow of both inlets pass through this narrow and shallow passage that creates a fast moving (approximately 9 kn or 17 km/h) and strong tidal rapids during the peak flows. At slack tide, the entrance is virtually flat calm similar to the Skookumchuck Narrows near the entrance of the Jervis Inlet.
The water stops rising, reaching a local maximum called high tide. Sea level falls over several hours, revealing the intertidal zone; ebb tide. Oscillating currents produced by tides are known as tidal streams or tidal currents. The moment that the tidal current ceases is called slack water or slack tide. The tide then reverses direction and is ...
The British Columbia Shore Station Oceanographic Program is a sea surface temperature and salinity monitoring program on the Canadian coast of the northeast Pacific Ocean. [1] The program is administered by Fisheries and Oceans Canada , and regroups 12 lighthouse stations in British Columbia .
Location: British Columbia: Coordinates: 1]: Type: Fjord lake and Tidal lake: Primary inflows: Pitt River: Primary outflows: Pitt River: Basin countries: Canada: Max. length: 24 km (15 mi): Max. width: 4.5 km (2.8 mi): Surface area: 53.5 km 2 (20.7 sq mi): Max. depth: 150 m (490 ft): Surface elevation: 3 m (9.8 ft) [2]: Islands: Goose, Little Goose, Gosling: References: [1]: Pitt Lake is the ...
Skookumchuck Narrows [1] is a strait forming the entrance of Sechelt Inlet on British Columbia's Sunshine Coast in Canada. Before broadening into Sechelt Inlet, all of its tidal flow together with that of Salmon Inlet and Narrows Inlet must pass through Sechelt Rapids. At peak flows, standing waves, whitecaps, and whirlpools form at the rapids ...
Tidal range is the difference in height between high tide and low tide. Tides are the rise and fall of sea levels caused by gravitational forces exerted by the Moon and Sun, by Earth's rotation and by centrifugal force caused by Earth's progression around the Earth-Moon barycenter. Tidal range depends on time and location.
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Tide tables, sometimes called tide charts, are used for tidal prediction and show the daily times and levels of high and low tides, usually for a particular location. [1] Tide heights at intermediate times (between high and low water) can be approximated by using the rule of twelfths or more accurately calculated by using a published tidal ...