Tides are the periodic rise and fall of sea level caused primarily by the gravitational pull of the Moon and the Sun. The highest level reached during a spring tide is called Mean High Water Springs (MHWS) and the lowest level during the same cycle is Mean Low Water Springs (MLWS).
The tidal range is the vertical distance between MHWS and MLWS. It is a key parameter for navigation, coastal engineering, and ecological studies because it determines the extent of intertidal zones and the energy available for tidal power generation.
By subtracting the MLWS height from the MHWS height, mariners can quickly assess the usable water depth for a given location and time. The simple linear relationship is expressed in the formula below.
What is tidal range?
How do I calculate tidal range?
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What is the difference between spring tide and neap tide?
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Results are for informational purposes only and do not constitute professional advice.
