The smallest tidal ranges, known as neap tides, occur during the first and third quarters of the moon when the sun and moon are at right angles to each other. This alignment causes their gravitational forces to partially cancel each other out, resulting in weaker tides.
Tidal ranges are typically largest on coasts with funnel-shaped bays or estuaries that amplify the tide. Additionally, coasts with narrow channels, shallow depths, and a resonant natural period that matches the tide-generating forces can also experience significant tidal ranges.
A tidal bore is most likely to occur on a coastal area with a funnel-shaped bay or estuary, such as in rivers or estuaries that have a narrow inlet opening onto a broad bay. The narrowing of the waterway causes the incoming tide to create a wave that can travel upstream, forming a tidal bore.
Whirlpools most often occur in the late summer and early fall when the water temperature is warmer and there is strong tidal or current activity.
Mountain ranges occur when two techtonic plates collide and both force each other up. These often happen along the entire border of the plate, which can be thousands of kilometers long.
waves occur all the time but after an earthquake tidal waves occur. Tidal waves are the cause of the tectonic plates colliding underwater. After the collision over time the wave goes form a small bump in the water to growing bigger and bigger into giant super wave capable of destroying towns.
Tidal ranges are typically largest on coasts with funnel-shaped bays or estuaries that amplify the tide. Additionally, coasts with narrow channels, shallow depths, and a resonant natural period that matches the tide-generating forces can also experience significant tidal ranges.
The daily tidal range is greatest during the Spring tide. This is when the moon and the sun are either together in the sky or they are on opposite sides of the heavens.
the combined forces of the sun and the moon on Earth produces tidal ranges.
how do tidal movements happen
Spring and neap currents are influenced by the alignment of the Earth, moon, and sun, affecting tidal ranges. Spring tides occur during full and new moons when tidal ranges are at their maximum, resulting in stronger currents. Perigean currents happen when the moon is closest to Earth (perigee), which can enhance tidal effects, while apogean currents occur when the moon is farthest from Earth (apogee), leading to weaker tidal influences. Thus, the primary difference lies in the moon's position and its impact on tidal strength and current intensity.
The biggest changes in tides typically occur in areas with large tidal ranges, such as the Bay of Fundy in Canada, which has the highest tides in the world reaching up to 16 meters (53 feet). Other locations with significant tidal ranges include the Gulf of Khambhat in India and the Severn Estuary in the UK.
Rivers don't have tidal ranges. Inlets, bays, estuaries, etc. do. are you really asking where on earth we observe the second highest coastal tidal range? That would be in the Severn Estuary in England, with Turnagain Arm in Alaska a close third. The Bay of Fundy in Canada has the highest tides.
A spring tide has the greatest tidal range. A neap tide has a smaller tidal range.
The tidal range varies due to the positions of the Earth, Moon, and Sun, typically cycling through a pattern of spring and neap tides. Spring tides, which have the highest tidal range, occur approximately every two weeks during the full and new moons. Neap tides, which have the lowest tidal range, occur about a week after the spring tides. Therefore, roughly 7 to 14 days pass between the lowest and highest tidal ranges.
The type of coast that a tidal bore would most likely occur is a coast with narrow bays and inlets. Tidal bores also occur on a coast that has river channels.
The typical tidal range in the open ocean is about 0.6 meters (2 feet). As you get closer to the coast, however, this range gets much greater. Coastal tidal ranges vary globally and can differ anywhere from 1.8 meters to 3 meters (6–10 feet). The world's biggest tidal differential occurs in the Bay of Fundy in Eastern Canada, where the sea level changes by up to 17 meters (55 feet) during the day. Ungava Bay in Northern Quebec, north eastern Canada, is believed by some experts to have higher tidal ranges than the Bay of Fundy (about 17 metres or 56 ft), but it is free of pack ice for only about four months every year, whereas the Bay of Fundy rarely freezes. What is generally regarded as the next highest tidal range occurs in the Bristol Channel in the UK, where sea levels change by some 15 meters (49 feet). The smallest tidal ranges occur in the Mediterranean, Baltic, and Caribbean Seas. A point within a tidal system where the tidal range is almost zero is called an amphidromic point.
The significant difference in tidal ranges between the Gulf of Mexico and the Bay of Fundy is primarily due to the unique geography and bathymetry of each region. The Bay of Fundy features a funnel shape that amplifies incoming tides, leading to some of the highest tidal ranges in the world, sometimes exceeding 50 feet. In contrast, the Gulf of Mexico has a broad and shallow continental shelf that dampens tidal effects, resulting in much lower tidal ranges, typically around 1 to 3 feet. Additionally, the tidal dynamics and oceanic currents in each area contribute to these variations.