The regular rise and fall of the water level in the earth’s oceans as a result of the gravitational forces between the earth, moon, and sun. The detailed theory of tides is complex. The moon is approximately twice as effective as the sun in causing tides. In illustration (a) the resultant gravitational forces between the moon and various points on the earth (solid lines) are shown as the vector sums of the tide-generating forces (broken lines) and a constant force (dotted lines) that is the same at all points on the earth and is equal to the moon’s attraction on the earth’s centre. The resultant force when the moon is in zenith (Z in the illustration) is greater than that at nadir (N) because Z is closer to the moon than N and the force is inversely proportional to the square of the distance according to Newton’s law of gravitation. Illustration (b) shows how at full and new moon the sun and moon act together to produce the high-range spring tides, while at quarter moon the forces are at right angles to each other causing the low-range neap tides.
The use of tidal energy, estimated at some 4 × 1018 J per annum at known tidal sites, dates back to medieval tidal mills. Modern tidal power stations use specially designed turbines, operated by tidal waters, to drive generators.
Tidal forces due to Jupiter have large effects on many of its moons.
Tides.
The rise and fall of the Earth’s oceans, caused by the gravitational attractions of the Moon and Sun. At the Earth’s centre, centrifugal force due to the motion of the Earth about the barycentre of the Earth–Moon system is balanced by gravitational force. On the side of the Earth nearest the Moon, the Moon’s gravitational pull is greater than centrifugal force, while on the opposite side the centrifugal force is greater. In both cases a tidal bulge is produced in the oceans. The Sun’s tide-raising power is about one-third that of the Moon, as a result of its greater distance from the Earth. The Sun and Moon act together at new or full Moon to produce extra-high and extra-low tides; these are the so-called spring tides. When the Moon is at first or third quarter the Sun and Moon are acting in different directions. The high tides are then at their lowest and the low tides are at their highest; these are the so-called neap tides. The Moon and Sun also raise measurable tides in the solid Earth and its atmosphere. The Earth raises tides in the Moon, its force being a maximum when the Moon is at perigee.
tides:
(a) neap tide; (b) spring tide
- time-series data
- time sharing
- time-slice
- time slicing
- time stamp
- timestamp
- time-stratigraphic unit
- time to flashover
- time to puncture
- time to trip
- time travel
- time zone
- time–distance curve
- time–space compression
- time–space convergence
- time–space geography
- time’s arrow
- timing analysis
- timing attack
- timing diagram
- Timon of Phlius (c.320–230)
- Timor‐Leste
- Timur
- tin
- Tinbergen, Nikolaas