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123:(or "half moon"). Also, in addition to the relative position of the moon and the elliptical pattern of the sun, the tide can be affected to some degree by wind and atmospheric pressure. All of these variables have less impact on the tide at the time of the full moon, so this is usually the best time to set a tide clock. If the tide clock is mounted on a moving boat, it will need to be reset more frequently. The best time to set the clock is at the new moon or the full moon, which is also when the clock can most reliably indicate the actual combined tide. A simple tide clock will always be least reliable near the quarter moon.
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Coast, tides can be irregular. The
Pacific Ocean is so vast that the moon cannot control the entire ocean at once. The result is that parts of the Pacific Coast can have 3 low tides a day. Similarly, there are areas in the world like the Gulf of Mexico or the South China Sea that have only one high tide a day. Mechanical tide clocks used on the Pacific Coast must be adjusted frequently, often as much as weekly, and are not useful in diurnal areas (those with one tide per day).
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shape of the local bay or estuary. Along some shorelines, the solar tide is the only important tide, and ordinary 12-hour clocks suffice since the high and low tides come at nearly the same time every day. Because ordinary tidal clocks only track a part of the tidal effect, and because the relative size of the combined effects is different in different places, they are in general only partially accurate for tracking the tides. Consequently, all navigators use
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along the left side it points to the number of hours "until" the (lunar) high tide. The right hand side of the clock is marked "hours until low tide" and has a count-down of hours from 5 to 1. The number pointed to by the hand gives the time "until" the (lunar) low tide. Some tide clocks incorporate time (using standard quartz movement) and even humidity and temperature in the same instrument.
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169:'s astronomical clock has twelve dials surrounding a central clockface. The dial at position X indicates the tides at Lier: the flag without a pennant, at the top of the dial, indicates high water; the flag with a pennant above indicates rising water, the flag with a pennant below indicates ebbing water. The size of the ships indicates the level of the tide.
79:, it takes a particular point on the Earth (on average) 24 hours and 50.5 minutes to rotate under the Moon, so the time between high lunar tides fluctuates between 12 and 13 hours. A tide clock is divided into two roughly 6 hour tidal periods that show the average length of time between high and low tides in a
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Analog tide clocks are most accurate for use on the
Atlantic coasts of America and Europe. This is because along the Atlantic coastline the moon controls the tides predictably, ebbing and flowing on a regular (12- to 13-hour) schedule. However, in other parts of the world such as along the Pacific
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Some tide clocks count down the number of hours from high or low tide, as in "one hour past high or low tide". When the clock reaches the halfway point ("half-tide"), it then counts the hours up to high tide or low tide, as in "one hour until high or low tide". Generally, there is an adjustment knob
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The bottom of the tide clock dial (6 o'clock position) is marked "low tide" and the top of the tide clock dial (12 o'clock position) is marked "high tide." The left side of the dial is marked "hours until high tide" and has a count-down of hours from 5 to 1. There is one hand on the clock face, and
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houses a tide clock, a 20th-century restoration of the original installed by Thomas Tue in 1681, which shows the moon phase and the time of local high tide, indicated by a dragon hand. The dial reads "LYNN HIGH TIDE" clockwise, but is to be interpreted as a 24-hour dial, with "L" at the top of the
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Digital tide clocks are not married to the 24 hour 50.5 minute tide cycle and thus track tides beyond the
Atlantic coast. Smart digital tide clocks can work across all locations in North America without any adjustments. This is achieved by storing all the variations of tides at numerous locations.
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Tide range is the vertical distance between the highest high tide and lowest low tide. The size of the lunar tide compared to the solar tide (which comes once every 12 hours) is generally about 2 to 1, but the actual proportion along any particular shore depends on the location, orientation, and
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Given a particular location and date/time, a digital tide clock can display the previous tide, next tide and current absolute tide height. Thus, they are able to track semi-diurnal, diurnal and mixed diurnal tides.
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107:, that is different at every location, so tidal clocks are set for the time when the local lunar high tide occurs. This is often complicated because the lead or lag varies during the course of the
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shows the time of local high tide, and the present state of the sea by means of a disc with a quarter-circle aperture which rotates with the lunar phase, revealing a green background at the
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is a tide clock designed by Laura
Williams, installed in 2010, which indicates the lunar phase, lunar day and tide cycle using a graphical notation of lights.
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on the back on the instrument which may be used to set the tide using official tide tables for a specific location at either high or low tide.
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was installed in 1996. Despite the clock's traditional dial, it is computer-controlled, and accounts for 94 waves in its tidal timekeeping.
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is most extreme ("spring tides"), and a black background at times of smaller tidal range ("neap tides").
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Specially designed clock that keeps track of the Moon's apparent motion around the Earth
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67:. The exact interval between tides is influenced by the position of the Moon and
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Administration, US Department of
Commerce, National Oceanic and Atmospheric.
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Why are Time and Tide Clocks Best Used on the
Atlantic Coast?
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dial as midday and "G" at the bottom of the dial as midnight.
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213:. Jacob Venker's tide clock on the exterior of the
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103:Tides have an inherent lead or lag, known as the
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407:WeND : Digital Tide Clock - North America
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367:: CS1 maint: multiple names: authors list (
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428:"L'horloge de la Sainte-Trinité à Fécamp"
345:"NOAA's National Ocean Service: Low tide"
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83:tide region, such as most areas of the
846:one-dimensional Saint-Venant equations
481:. Cambridge University Press. p.
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190:(at new moon and full moon), when the
450:Nationaal Sleepvaart Museum Maassluis
426:Decressain, Abbé Georges (May 1899).
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403:"Digital Tide Clock - North America"
152:Public clocks with tide indications
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988:Global Ocean Data Analysis Project
91:Traditional mechanical tide clocks
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694:Luke's variational principle
477:Tides: A Scientific History
434:(in French) (512): 259–262.
215:Nationaal Sleepvaart Museum
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1381:Mohorovičić discontinuity
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614:Boussinesq approximation
51:that keeps track of the
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1718:Outline of oceanography
913:Atmospheric circulation
851:shallow water equations
841:Waves and shallow water
734:Significant wave height
471:Cartwright, David Edgar
325:Tide predicting machine
182:. The clock of 1667 at
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1730:Sea surface microlayer
1095:Wind generated current
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1545:World Geodetic System
1053:Princeton Ocean Model
933:Coriolis–Stokes force
583:Physical oceanography
549:at Wikimedia Commons
349:oceanservice.noaa.gov
237:. The south tower of
131:either in a booklet,
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1583:Underwater acoustics
1143:Perigean spring tide
1008:Langmuir circulation
719:Rossby-gravity waves
432:Revue chronométrique
1745:Science On a Sphere
1351:Convergent boundary
1023:Modular Ocean Model
983:Geostrophic current
699:Mild-slope equation
239:King's Lynn Minster
143:Digital tide clocks
1401:Seafloor spreading
1391:Outer trench swell
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1256:Continental margin
1241:Carbonate platform
1138:Lunitidal interval
518:Trinity Buoy Wharf
388:2015-06-03 at the
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105:lunitidal interval
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37:Trinity Buoy Wharf
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1770:World Ocean Atlas
1760:Underwater glider
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1236:Bathymetric chart
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545:Media related to
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289:Zimmertoren, Lier
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998:Humboldt Current
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1028:Ocean current
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1014:
1011:
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826:Wave shoaling
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786:Ursell number
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669:Internal wave
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619:Breaking wave
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492:9780521621458
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1765:Water column
1713:Oceanography
1688:Observations
1683:Explorations
1653:Marginal sea
1646:
1604:OSTM/Jason-2
1436:Volcanic arc
1411:Slab suction
1128:Head of tide
1018:Loop Current
958:Ekman spiral
744:Stokes drift
654:Gravity wave
629:Cnoidal wave
539:
522:. Retrieved
517:
508:
496:. Retrieved
476:
465:
453:. Retrieved
449:
446:"Tide clock"
440:
431:
421:
410:. Retrieved
406:
397:
377:
352:. Retrieved
348:
338:
301:FĂ©camp Abbey
184:FĂ©camp Abbey
167:Zimmer tower
146:
137:
125:
121:quarter moon
102:
98:
94:
81:semi-diurnal
44:
42:
32:
1755:Thermocline
1472:Mesopelagic
1445:Ocean zones
1416:Slab window
1281:Hydrography
1221:Abyssal fan
1188:Tidal range
1178:Tidal power
1173:Tidal force
1058:Rip current
993:Gulf Stream
953:Ekman layer
943:Downwelling
918:Baroclinity
905:Circulation
801:Wave height
791:Wave action
774:megatsunami
754:Stokes wave
714:Rossby wave
679:Kelvin wave
659:Green's law
547:tide clocks
514:"Alunatime"
313:King's Lynn
235:King's Lynn
218: [
199:Netherlands
192:tidal range
129:tide tables
109:lunar month
59:around the
31:Tide clock
1693:Reanalysis
1592:Satellites
1573:Sofar bomb
1421:Subduction
1396:Ridge push
1291:Ocean bank
1271:Contourite
1198:Tide gauge
1183:Tidal race
1168:Tidal bore
1158:Slack tide
1123:Earth tide
1043:Ocean gyre
863:Wind setup
858:Wind fetch
821:Wave setup
816:Wave radar
811:Wave power
709:Rogue wave
639:Dispersion
412:2018-09-18
354:2018-09-18
331:References
265:Arnemuiden
205:Arnemuiden
45:tide clock
23:Tide clock
1555:Acoustics
1507:Sea level
1406:Slab pull
1343:tectonics
1251:Cold seep
1213:Landforms
1090:Whirlpool
1085:Upwelling
868:Wind wave
796:Wave base
724:Sea state
644:Edge wave
634:Cross sea
277:Maassluis
211:Maassluis
113:full moon
33:Alunatime
1825:Category
1788:Category
1740:Seawater
1467:Littoral
1462:Deep sea
1321:Seamount
1203:Tideline
1148:Rip tide
1078:shutdown
1048:Overflow
781:Undertow
624:Clapotis
524:26 March
498:26 March
473:(1999).
455:26 March
386:Archived
363:cite web
319:See also
188:syzygies
133:computer
117:new moon
115:and the
39:, London
1798:Commons
1668:Mooring
1618:Related
1609:Jason-3
1599:Jason-1
1482:Pelagic
1477:Oceanic
1452:Benthic
769:Tsunami
739:Soliton
157:Belgium
1831:Clocks
1487:Photic
1316:Seabed
729:Seiche
520:. 2013
489:
246:London
180:FĂ©camp
174:France
165:. The
1678:Ocean
1647:Alvin
1497:Swash
1341:Plate
1286:Knoll
1276:Guyot
1231:Atoll
1110:Tides
873:model
759:Swell
591:Waves
222:]
73:Earth
65:tides
61:Earth
49:clock
1645:DSV
1630:Argo
1492:Surf
948:Eddy
526:2020
500:2020
487:ISBN
457:2020
369:link
163:Lier
53:Moon
69:Sun
55:'s
35:at
1827::
516:.
485:.
483:20
448:.
430:.
405:.
384:,
365:}}
361:{{
347:.
220:nl
87:.
43:A
575:e
568:t
561:v
528:.
502:.
459:.
415:.
371:)
357:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
