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Tides are felt as far north as the federal dam at Troy, where the mean tidal range is 4.7 feet (1.4 metres).
The study area is subject to semi-diurnal tides, with a mean tidal range of 5.15 m.
These processes can be illustrated with an example from a microtidal (mean tidal range = 1.2 m) low marsh site in coastal Virginia, USA (Christiansen et al. 2000).
The mean high and low tides increased at a rate of 0.08 and 0.52 cm per year, respectively, whereas the mean tidal range decreased at a rate of 0.44 cm per year.
A coastal vulnerability index (CVI) was constructed to estimate the level of vulnerability of a coastline approximately 48.68 km in length using seven physical variables, namely, land subsidence, relative sea level change, coastal geomorphology, coastal slope, shoreline change, mean tidal range, and significant wave height.
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Particular attention is given to the temporal evolution of various parameters characterizing the M2 tide, especially the mean largest tidal range (MLTR), the mean highest high water (MHHW), the mean lowest low water (MLLW), and the mean sea level (MSL).
The tidal range means that the legs of the pier are largely exposed at low tide and hidden at high tide.
The tidal range means that the legs of the pier are largely exposed at low tide and hidden at high tide and the landing stage at the end of the pier has several levels to allow boats to dock at all stages of the tide.
The southern GBR is tidally dominated, with tidal range up to 10 m in places, causing extreme tidal currents.
However, control group ventilation strategies did not achieve the full range of traditional tidal volumes; mean tidal volumes were consistently at the lower end of the traditional range.
The greatest tidal range in the British Isles at mean spring tide more than 36 feet (11 metres)—occurs near Portishead.
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