the periodic motions of waters of the sea due to differences in the attractive forces of various celestial bodies, principally the moon and sun, upon different parts of the rotating earth
tidal phenomenon
a periodic horizontal movement of the water
tidal current
British usage of tidal current is
tidal stream
the change in the water level the water moves toward the shore
flood tide
the change in the water level when the water moves away from the shore
ebb tide
rise and fall of the water level
tide
the periodic rise and fall of water in the ocean accompanying the tidal phenomenon.
tide
the maximum height reached by the ascending tide.
high water or high tide
the minimum level reached by the descending tide.
low tide or low water
the period at high or low water during which there is no sensible change of level
stand of the tide
when there is no more horizontal movement of the water, occurs between the flood and ebb
slack water
the difference in height between consecutive high and low waters
Range of the tide
the vertical distance at any time of the tide from the chart-sounding
datum (charted depth)
height of the tide
the vertical distance from the chart-sounding datum to a high tide reference point
rise of the tide
there are two high and two low waters each tidal day, with relatively small inequality in high and low water heights
Semidiurnal type of tide
single high and single low water occur each tidal day
Diurnal type of tide
both diurnal and semidiurnal and the tide is characterized by a large inequality in high water heights, low water heights, or in both
Mixed type of diurnal
occur when the moon is at the point in its orbit nearest to the earth (at perigee), the lunar semidiurnal range is increased
Perigean tides
occur when the moon is at the point in its orbit farthest from the earth (at apogee)
Apogean tides
tides with higher high water and lower low water
Spring tides
Occur when the moon and the sun are in line and pulling together at new and full moon
Spring tides
tides with lower high water and higher low water
Neap tides
Occurs when the moon and the sun oppose each other, as at quadratures; at first quarter or last quarter
Neap tides
occur when the moon is at its maximum semi- monthly declination either north or south; the diurnal effect is at a maximum
Tropic tides
occur when the moon crosses the equator, the diurnal effect is at a minimum
Equatorial tides
when high and low tides occur at about the same time everyday because of the effect of the sun
Solar tide
occur in few estuaries, the advance of low water trough is so much retarded that the crest of the rising tide overtakes the low, and advances as a churning, foaming wall of water
bore
there is a slight fall in the middle of the high water period, the effect is to create a longer period of stand during high tide
Double low water
there is a slight rise in the middle of the low water period, the effect is to create a longer period of stand during low tide
Double high water
the time between consecutive transits of moon, or 24 hours and 50
minutes on the average
Tidal day or Lunar day
the interval between the moon’s meridian transit and a particular phase of tide
Lunitidal interval
the average elapsed time between the moon’s transit and the next high water
Establishment of the port
the establishment of the port during new or full moon
Vulgar establishment
shortening of time interval between successive high waters
Priming
the periodic retardation in time of occurrence of high and low waters
Lagging
shortest cycle for a tidal cycle
12 hours and 25 minutes for semidiurnal
it is completed at about 24 hours and 50 minutes.
Lunar day or tidal day
occurs when the moon revolves around the earth with respect to the
sun
Synodical month or lunar month
it is completed at about 29 ½ days
Synodical month or lunar month
the phase variation of the moon as it varies from new to full or full to new