Tides Flashcards
are daily changes in the elevation of the ocean surface
tides
occurs when the sun and the moon are aligned causing larger tidal bulges(higher high tides) and deeper tidal troughs (lower low tides) thus, producing a large tidal range.
spring tide
occurs when the gravitational pull of the sun and the moon acts upon earth at right angles at a right angle therefore they are partially offsets the gravitational forces of each other producing producing less tidal range
Neap Tide
Horizontal flow of water accompanying the rise and fall of the tide
tidal currents
tidal currents that advance into the coastal zone as the tide rises
Flood current
tidal current genertaed by seaward moving water as the falls
ebb current
periods of little to no current
slack water
area affecyed by alternating tidal currents
tidal flats
deltas created by tidal currents
tidal deltas
formed at the landward inlet
flood delta
formed at the seaward side of delta
ebb delta
wave ction can maintain a barrier system that can be more or less continous for tens of kilometers
microtidal coast
with the increased tidal range in mesotidal conditions, more exchange of water between the lagoon and the sea is required, resulting in more inlets forming, breaking up the barrier into a series of islands
mesotidal coast
coast that have a high tidal ranges do not develop barrier systems because the ebb and flood tidal currents are stronger controls on the distribution of sediment than wave action
Macrotidal Coast
water that is closest to the moon experiences the largest gravitational attraction and this creates a bulge of water
tidal bulge
any point on the surface the level of the water will rise and fall twice a day as the two bulges are passed in each rotation
diurnal tides
a point on the earth willpass under one high bulge and a slightly lower bulge 12 hrs or so later
Diurnal tide inequality
sun and moon are in line with the earth
syzygy
during the four weeks of the moon’s orbit, it is twice in line and twice perpendicular
near spring tidal cycles (spring and neap tides)
occuring when the three bodies are in line.
The highest tidal range, occurs near the times of the new and full moons.
spring tide
the lowest tidal range occuring near three times of the first and third quarters of the moon
neap tides
cycle cased by the elliptical nature of the earths orbit around the sun. At the sprimg (vernal) and autumn (fall) equinoxes, the earth is closest to the Sun and the gravitational effect is strongest.
Annual Tidal Cycle
high tides and low tides
tidal Ranges
point of zero amplitude of one harmonic constituent of the tide.
Amphidromic cells