Tides Flashcards
Overview
Regular and consistent inputs of energy
UK experiences 2 high and 2 low tides each day
The moon
Moon has greatest influence, pulls water towards it creating a high tide
Compensatory bulge on opposite side
In areas between the 2 bulges its the low tide
Spring tides
When Earth, moon and sun are aligned the gravitational pull is strongest High tides become higher Low tides lower Creates larger tidal range Happens 2x a month
Neap tides
Earth, moon and sun form a right angle this lessens gravitational pull
High tides lower
Low tides higher
Smaller tidal range
Factors influencing tides
Morphology of seabed
Proximity of land masses
Coriolis force (spin of Earth) Eg at equator there is no Coriolis force so around the world tidal range differs
Small tidal range
Power of waves concentrated on narrow part of coastline for long period of time such as cliff base
Creates features such as wave cut notch
Large tidal range
Power of waves is spread out means the zone of erosion is wide
Waves will break out on specific part for short period of time
High tidal range
create powerful currents as tides rise and fall
Found in spring tides
Important transfer mechanisms in transporting sediment as an output