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- Tidal_range abstract "The tidal range is the vertical difference between the high tide and the succeeding low tide. Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon and the Sun and the rotation of the Earth. The tidal range is not constant, but changes depending on where the sun and the moon are.The most extreme tidal range occurs around the time of the full or new moons, when the gravitational forces of both the Sun and Moon are in phase, reinforcing each other in the same direction (new moon), or are exactly the opposite phase (full). This type of tide is known as a spring tide. During neap tides, when the Moon and Sun's gravitational force vectors act in quadrature (making a right angle to the Earth's orbit), the difference between high and low tides is smaller. Neap tides occur during the first and last quarters of the moon's phases. The largest annual tidal range can be expected around the time of the equinox, if coincidental with a spring tide.Tidal data for coastal areas is published by the national hydrographic service of the country concerned. Tidal data is based on astronomical phenomena and is predictable. Storm force winds blowing from a steady direction for a prolonged time interval combined with low barometric pressure can increase the tidal range, particularly in narrow bays. Such weather-related effects on the tide, which can cause ranges in excess of predicted values and can cause localized flooding, are not calculable in advance.".
- Tidal_range thumbnail Tidal_Range.jpg?width=300.
- Tidal_range wikiPageID "3895284".
- Tidal_range wikiPageLength "4271".
- Tidal_range wikiPageOutDegree "30".
- Tidal_range wikiPageRevisionID "698580867".
- Tidal_range wikiPageWikiLink Amphidromic_point.
- Tidal_range wikiPageWikiLink Baltic_Sea.
- Tidal_range wikiPageWikiLink Bay_of_Fundy.
- Tidal_range wikiPageWikiLink Canada.
- Tidal_range wikiPageWikiLink Caribbean_Sea.
- Tidal_range wikiPageWikiLink Category:Oceanography.
- Tidal_range wikiPageWikiLink Category:Tides.
- Tidal_range wikiPageWikiLink Earth.
- Tidal_range wikiPageWikiLink England.
- Tidal_range wikiPageWikiLink Equinox.
- Tidal_range wikiPageWikiLink Full_moon.
- Tidal_range wikiPageWikiLink Funnel.
- Tidal_range wikiPageWikiLink Mediterranean_Sea.
- Tidal_range wikiPageWikiLink Moon.
- Tidal_range wikiPageWikiLink National_Oceanic_and_Atmospheric_Administration.
- Tidal_range wikiPageWikiLink New_moon.
- Tidal_range wikiPageWikiLink Severn_Estuary.
- Tidal_range wikiPageWikiLink Sun.
- Tidal_range wikiPageWikiLink Tide.
- Tidal_range wikiPageWikiLink United_Kingdom.
- Tidal_range wikiPageWikiLink United_States.
- Tidal_range wikiPageWikiLink Wales.
- Tidal_range wikiPageWikiLink File:Tidal_Range.jpg.
- Tidal_range wikiPageWikiLinkText "MLT".
- Tidal_range wikiPageWikiLinkText "Tidal range".
- Tidal_range wikiPageWikiLinkText "tidal movements".
- Tidal_range wikiPageWikiLinkText "tidal range".
- Tidal_range wikiPageUsesTemplate Template:Citation_needed.
- Tidal_range wikiPageUsesTemplate Template:Physical_oceanography.
- Tidal_range wikiPageUsesTemplate Template:Reflist.
- Tidal_range subject Category:Oceanography.
- Tidal_range subject Category:Tides.
- Tidal_range hypernym Difference.
- Tidal_range type Disease.
- Tidal_range type Geophysic.
- Tidal_range type Science.
- Tidal_range comment "The tidal range is the vertical difference between the high tide and the succeeding low tide. Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon and the Sun and the rotation of the Earth.".
- Tidal_range label "Tidal range".
- Tidal_range sameAs Q1398201.
- Tidal_range sameAs Tidenhub.
- Tidal_range sameAs Carrera_de_marea.
- Tidal_range sameAs Hauteur_de_marée.
- Tidal_range sameAs Julat_pasang_surut.
- Tidal_range sameAs m.0b5mnj.
- Tidal_range sameAs Q1398201.
- Tidal_range sameAs 潮差.
- Tidal_range wasDerivedFrom Tidal_range?oldid=698580867.
- Tidal_range depiction Tidal_Range.jpg.
- Tidal_range isPrimaryTopicOf Tidal_range.