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Chapter 9: Tides

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Term
Definition
Tide   periodic rise & fall of ocean resulting from gravitational interactions of moon, sun, & earth  
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Tidal range   difference between high & low tide water lines  
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Ebb flow   Seaward tidal flow from high to low tide  
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Flood flow   Landward tidal flow from low to high tide  
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Slack water   Time of no flow between ebb and flood  
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Diurnal tide   one high & one low tide are experienced each day  
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Semidiurnal tide   two high & two low tides of approximately equal altitudes occur daily  
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Mixed tide   two strongly unequal high & low tides occur daily  
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Spring tide   tide occurring twice a month in which greatest tidal range is experienced (occurs during new & full moon)  
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Neap tide   tide occurring twice a month when the tidal range is the smallest  
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Microtidal   coast with <2m tidal range  
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Mesotidal   Type of coast with 2-4m tidal range  
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Macrotidal   Type of coast w/ >4m tidal range  
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Gravitational force   force of attraction between masses  
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Centrifugal force   An apparent "center-fleeing force" felt by objects experiencing uniform circular motion as a result of inertial resistance to centripetal acceleration  
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Coriolis force   Apparent force caused by rotation of the earth, responsible for the deflection of surface currents to the right in the northern hemisphere & to the left in southern hemisphere  
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Equilibrium theory of tide formation   Two tidal bulges are produced on opposite sides of the earth; the bulge facing the moon is produced largely by the moon's gravitational effect, whereas the bulge on the opposite side is produced by centripetal acceleration (centrifugal force)  
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Apogee   when distance between the moon & the earth is 407,000km; causes slightly lower tides  
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Perigee   when distance between the moon & the earth is 357,000km; causes higher tides  
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Equinoxes   Sept. 21, March 21. Spring tides are highest b/c moon, earth, and sun are in straight line  
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Solstices   June 21, Dec. 21; spring tides are lower b/c moon, earth, and sun are NOT aligned  
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Perihelon   Location of sun during winter (for northern hemisphere); 148,500,000km from earth  
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Aphelion   location of sun during summer (for northern hemisphere); 152,200,000km from earth  
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Amphidromic system   Region under the influence of a single rotating kelvin wave  
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Amphidromic point   Nodal point around which the kelvin wave rotates  
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Cotidal lines   lines connecting points experiencing high tide at the same time  
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Corange lines   lines connecting points having the same tidal range  
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Harmonic method of tide prediction   The observed tide is produced from a number of components (partial tides) having a given period, amplitude, & phase that can be represented by a sine wave  
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M2   Principal lunar tidal component (12.42 hrs)  
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S2   Principal solar tidal component (12.00 hrs)  
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K1   Luni-solar diurnal tidal component (11.00 hrs)  
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