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Neap tides

Figure 6.9 Theoretical diagram of fluid mud formation and disruption at the frontal zone showing (a) neap tide stratified fluid mud formation—with strong vertical salinity gradient and (b) spring tide mixed or mobile fluid mud formation—with strong horizontal salinity gradient. (Modified from Kineke et al., 1996.)... Figure 6.9 Theoretical diagram of fluid mud formation and disruption at the frontal zone showing (a) neap tide stratified fluid mud formation—with strong vertical salinity gradient and (b) spring tide mixed or mobile fluid mud formation—with strong horizontal salinity gradient. (Modified from Kineke et al., 1996.)...
Station Mean values Spring tide Neap tide Maximal tide... [Pg.156]

Fig. 1.4 Every two weeks, the Sun and Moon are aligned with Earth so that the gravitational forces of both heavenly bodies create very high tides called spring tides. When the Moon and Sun are at right angles to Earth, lower, or neap, tides result. Fig. 1.4 Every two weeks, the Sun and Moon are aligned with Earth so that the gravitational forces of both heavenly bodies create very high tides called spring tides. When the Moon and Sun are at right angles to Earth, lower, or neap, tides result.
When the sun and moon are aligned either on one or both sides of the Earth, as during the full and new moons, tidal fluctuations are greatest (called spring tides). When the moon and sun are at right angles to each other, as during the first and third quarters of the moon, tidal fluctuations are at a minimum (called neap tides). [Pg.438]

The construction programme was based around spring and neap tidal cycles, working seaward on spring tides and landward on neap tides. Dismantling started in the middle of the pier with the existing decks lifted off and disposed. [Pg.125]

Figure 2.2 Distribution of the coastal fringes (according to Liining, 1990 and Lallier and Toulmond, 2006) 1, Highest level of the high tides (level 120 on the sea charts) 2, Mean level of the sea at the site considered 3, Lowest level of the neap tides (level 0 on the sea charts) the interval 1-3 represents the range of the tides at the site considered 4, Benthic zone (close to the bottom) 5, Pelagic zone (far out at sea). Figure 2.2 Distribution of the coastal fringes (according to Liining, 1990 and Lallier and Toulmond, 2006) 1, Highest level of the high tides (level 120 on the sea charts) 2, Mean level of the sea at the site considered 3, Lowest level of the neap tides (level 0 on the sea charts) the interval 1-3 represents the range of the tides at the site considered 4, Benthic zone (close to the bottom) 5, Pelagic zone (far out at sea).
Fig. 7. Ranges of elevation in which different plant species occur on a salt marsh near Guilford, Connecticut. Datum is mean sea level (MSL). The tidal ranges shown are the highest astronomical tide (HAT), mean high-water springs (MHWS), and mean high-water neaps (MHWN). Fig. 7. Ranges of elevation in which different plant species occur on a salt marsh near Guilford, Connecticut. Datum is mean sea level (MSL). The tidal ranges shown are the highest astronomical tide (HAT), mean high-water springs (MHWS), and mean high-water neaps (MHWN).
King et al. collected wave setup data at Woolacombe Beach in North Devon, U.K. which faces the North Atlantic Ocean. The beach face slope varied between 1 on 40 at high tide and 1 on 70 at mid-tide level with a tidal range of 3 m at neap and as much as 9 m at springs. Beach face material consisted of fine sand with... [Pg.14]


See other pages where Neap tides is mentioned: [Pg.893]    [Pg.115]    [Pg.116]    [Pg.454]    [Pg.230]    [Pg.16]    [Pg.17]    [Pg.184]    [Pg.80]    [Pg.174]    [Pg.822]    [Pg.55]    [Pg.60]    [Pg.237]    [Pg.111]    [Pg.793]    [Pg.893]    [Pg.115]    [Pg.116]    [Pg.454]    [Pg.230]    [Pg.16]    [Pg.17]    [Pg.184]    [Pg.80]    [Pg.174]    [Pg.822]    [Pg.55]    [Pg.60]    [Pg.237]    [Pg.111]    [Pg.793]    [Pg.17]    [Pg.72]    [Pg.76]    [Pg.87]    [Pg.29]    [Pg.43]    [Pg.44]    [Pg.46]    [Pg.47]    [Pg.211]    [Pg.9]   
See also in sourсe #XX -- [ Pg.16 , Pg.17 ]




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