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Tides are combined with the northerly Norwegian Sea currents and with storm-induced flow to result in a significant stream, with a reported speed varying between the sources from about 11 to 20 kilometres per hour (6.8 to 12.4 mph) and above. [3] [6] [11] This flow occurs at the significant depths of about 500 metres (1,600 ft).
Tidal energy can be extracted by two means: inserting a water turbine into a tidal current, or building ponds that release/admit water through a turbine. In the first case, the energy amount is entirely determined by the timing and tidal current magnitude. However, the best currents may be unavailable because the turbines would obstruct ships.
Small environmental variations within a mangal may lead to greatly differing methods for coping with the environment. Therefore, the mix of species is partly determined by the tolerances of individual species to physical conditions, such as tidal flooding and salinity, but may also be influenced by other factors, such as crabs preying on plant ...
Mangroves range in size from small bushes to the 60-meter giants found in Ecuador. Within a given mangrove forest, different species occupy distinct niches. Those that can handle tidal soakings grow in the open sea, in sheltered bays, and on fringe islands. Trees adapted to drier, less salty soil can be found farther from the shoreline.
Vortices known as whirlpools or maelstroms up to 10 m (33 ft) in diameter and 5 m (16 ft) in depth are formed when the current is at its strongest. At this point, one source claims that the tidal current can reach 40 km/h (25 mph). [7] Saltstraumen has existed for about two to three thousand years.
Of these global tidal wetland losses and gains, 39% of losses and 14% of gains were attributed to direct human activities. [ 263 ] Approximately 40% of the global mangrove has been lost since the 1950's [ 264 ] with more than 9,736 km 2 of the world's mangroves continuing to be degraded in the 20 years period between 1996 and 2016. [ 265 ]
The strongest rips and associated feeder currents occur in association with intermediate transverse bar and rip topographies. Transitions between beach states are often caused by changes in wave energy , with storms causing reflective beach profiles to flatten (offshore movement of sediment under steeper waves), thus adopting a more dissipative ...
The tides received relatively little attention in the civilizations around the Mediterranean Sea, as the tides there are relatively small, and the areas that experience tides do so unreliably. [ 3 ] [ 4 ] [ 5 ] A number of theories were advanced, however, from comparing the movements to breathing or blood flow to theories involving whirlpools ...