Waves approaching shore & cross-shore sediment transport Flashcards

1
Q

Why do large wavelengths travel faster?

A

Rate = distance/ time
Wave velocity = wavelength/ period
Keeping velocity constant…
If wavelength goes down, then T must get really small (less time between crests).
If wavelength goes up, then T must get big (more time between crests).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Define deep water

A

Depth is greater than half a wavelength

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Define shallow water

A

Depth is less than half a wavelength

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Why does wave motion get distorted in shallow water and not deep water?

A

In deep water (depth > half a wavelength), seabed is far below motion so no interaction between wave and bed.
In a fully “shallow water wave” wave motion constant over full depth.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

What happens when a wave enters shallower water?

A

There is less depth for water motions.
If there’s less depth it means there is less room for that squeezing to happen in front of the wave = slower wave propagation (can’t move itself forward as fast).

HOWEVER wave energy must be conserved…
The number of crests is therefore the same.

Velocity is going down (less squeezing) but the wave period (number of crests/ min) is staying the same = wavelength MUST decrease, to conserve energy H must go up (only space available is up).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

What is shoaling?

A

Number of crests stays the same (period is constant)
Propagation velocity decreases
Means wavelength has to decrease
Energy conserved, but changed wave shape means
Wave height has to increase
Meanwhile…
Orbital velocity goes up

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Why does orbital velocity increase during shoaling?

When do you get wave breaking?

A

At the trough (bottom of the wave) there is a frictional drag on the bed (more and more).
This means the trough is slowing down more than the crest is.
The crest gets squeezed into a sharper wall as H increases = more and more distorted.
Forward velocity increases.

When the orbital velocity is greater than the wave velocity.
When H > 1/7 wavelength

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What is a plunging wave?

A

The crest is moving too fast to keep the wave form together.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What is a spilling wave?

A

The crest is too steep to keep the wave form together.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

The kind of wave you get (plunging vs spilling) depends on what?

A

The relative difference between wave wavelength vs bed slope (big range).

Gradual bed slopes = more spilling
Steep (or abrupt) slopes = more plunging
Steep slope, long wavelength = BIG plunge
Bigger wavelength -> different parts of the wave feel the effects of the bed differently.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Velocity asymmetry is hugely important to…

A

sediment transport

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

What is a force?

A

A change in momentum.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Why do breaking waves shrink?

A

Momentum transferred into water (rather passing through it)
Same as a person when a wave knocks you over, momentum is getting transferred from the wave to you.
Momentum also transferred into bed, losing energy (dissipation -> not conserving it anymore)
Means H goes down

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Cross shore forcing diagram

A

Waves always approach shore at an angle.

Angle of approach is represented by dark blue arrow- three hash lines represent wave crests.
Different lengthed light blue arrows represent angle (alongshore and cross shore component).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

What cross shore (onshore) components drive sediment transport?

A
Piles water against shore
Until gravity (pressure gradient) = wave force
Waves, even with refraction (bending), often look parallel but almost never are; even a small angle can have a major long term effect.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

What is the set up?

A

The difference between the water at a perfect calm and how the water gets piled up coming onshore.

17
Q

Onshore piling vs pressure gradient

A

Balance can’t be perfect
Drift rollers always transporting more toward shore; increases slope past balance -> set up (wave forcing stronger near surface).
Result = increasing the slope
(wave forcing stronger near surface)
So -> set up -> get return flow (undertow) near bed (a net offshore movement)
Undertow is a residual net effect (averaged) out over wave forcing