Chapter 4 - Energy from Waves and Tides Flashcards

1
Q

How are waves created?

A

By friction of wind with water surface.

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2
Q

What is the Bernoulli equation?

A

It says that an increase in wave speed will mean a decrease in air pressure. p_air + 1/2 rho v_wind^2 = const (+ impact pressure of additional wind).

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3
Q

Draw a deep ocean wave.

A

Sinusoidal form. Water moves in circles with radius R = amplitude of the wave. Speed on top is v_wave - v_circle. Speed on bottom is v_wave + v_circle.

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4
Q

Does the water molecules of a wave move laterally?

A

Not averaged over time.

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5
Q

Calculate the wave speed.

A

The speed of the circle:

vcircle = 2πRfw
∆Ekin = 1/2 m ( v2bottom + v2top) = 1/2 m * (4vw vcircle) = 2m vw 2πRfw

This is equal to the change in potential energy ∆Epot = 2mgR

g = 2vwπfw => vw = g/2πfw

Using fw = vw/lambdaw

=> vw = sqrt(lambdaw g / 2π)

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6
Q

What can be said about the dispersion of deep ocean waves?

A

They have a large dispersion. The longer the wave lengths, the faster they move.

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7
Q

What is the wave speeds dependence on surface tension?

A

The surface tension leads to an additional restoring force of a wave, trying to minimize the water surface.

This means that the wave velocity gets an additional term:

vw = sqrt(g*lambdaw/2π + 2πσ/rho *lambdaw)

This means that we have two regimes:

When lambdaw < 1cm, we get capillary waves and vw scales with sqrt(1/lambda).

When lambdaw > 10 cm, we get gravitational waves, and vw scales with sqrt(lambda).

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8
Q

How does the speed of gravitational waves scale? What is the condition for gravitational waves?

A

Condition: lambda > 10cm. Scales with sqrt(lambda).

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9
Q

How does the speed of capillary waves scale? What is the condition for capillary waves?

A

Condition: lambda < 1 cm. Scales with sqrt(1/lambda).

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10
Q

How does the equation for wave velocity look for shallow water waves?

A

vw = sqrt(g*lambda/2π * tanh(2πd/lambda)).

For d << lambda, tanh x -> x and we get

vw = sqrt(gd), that is the speed is independent on the wavelength.

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11
Q

What is the condition for shallow water waves?

A

d < lambda/4.

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12
Q

What is the reason for the destructive effect of tsunamis?

A

When the wave comes in to shallow waters, the speed of the water scales with sqrt(d), where d is the water depth. This means that it ever decreases its speed, and compensates with amplitude heigth to maintain energy conservation.

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13
Q

Estimate the energy of a wavefront of breadth b = 1km, with an amplitude A = 2.5 m, and wavelength lambdaw = 50m. Assume sinusoidal shape.

A

Calculate the mass of the top:

Mtop = rho*V = rho*b*A * ∫ sin(2πx / lambda) dx from 0 to lambda/2 = rho * b * A * lambda/π.

The potential energy of this wavefront is then:

∆Epot = M*g*2∆h_sp, where ∆h_sp is the center of gravity, which is π/32*A.

In this example, ∆Epot = 2*1018J

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14
Q

Derive the expression for the power per meter of a wave.

A

dP/dx = ∆Epot/b * fw = MgAπfw/16b

= rho*A2*g*lambda*fw / 16

Using lambda = g/2πfw2

=> dP/dx = 1/32π * rho * g2 * A2/fw

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15
Q

Describe the origin of the solar tide in the global ocean model.

A

This is caused by a local equilibrium of gravitational force and centrifugal force on the earth while moving around the sun. At the bright-side the gravitational pull is stronger than the centrifugal force, and we have a tide. On the dark side the centrifugal force is stronger than the gravitational pull, and we also have a tide here.

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16
Q

What is the average centrifugal acceleration of the earth in its orbit?

A

acf = rSE*omega2

With omega = 2π/1 year = 2*10-7 s-1 and rSE = 1.5 * 1011 m

we get acf = 6*10-3 m s-2

17
Q

What is the variation of the centrifugal acceleration from the sun?

A

∆acf = 2Rearthomega2 = 2.5 * 10-7 m s-2

18
Q

What is the average gravitational acceleration on the earth by the sun?

A

g = G msun / rSE2

19
Q

What is the variation in gravitational acceleration from the sun through the earth?

A

∆g = |dg/dr| * 2Rearth = 2Gmsun/rSE3 * 2Rearth ≈ 10-6

20
Q

Which of the changes of centrifugal acceleration and gravitational acceleration contributes most to the solar tides?

A

The changes in gravitational acceleration is the highest, and contribues the most to the solar tides.

21
Q

What is the expected tidal period?

A

12h.

22
Q

Describe the origin of the lunar tides.

A

Similar to the solar tides. Here the Earth rotates around center of gravity, which lies inside the earth, with a period of 27.3 days.

23
Q

From the models we have learned about lunar and solar tides, how big tidal waves can we expect based on a global ocean model?

A

50 cm.

24
Q

How can tidal heights be amplified?

A

By coasts and by so-called lambda/4 resonances.

25
Q

What is lambda/4-resonances when talking about waves?

A

A lambda/4-resonance is an effect we get if we have bays that have a length which are a fourth of the wavelength. Then we have a phase shift of π of the ingoing and outgoing waves. Due to the phase shift of π from reflection, we get a total phase shift of 2π. We get a constructive interference between incoming and reflected tidal waves, and we can get tidal amplitudes up to 10 m.

26
Q

Why has the Earth’s rotation slowed over the years?

A

Due to mechanical energy from the Earth-moon system being lost to friction (water towards coastlines etc). Similar effects of the sun.

27
Q

Name two systems of harnessing wave power.

A

Tapered channel: Bring waves into a tapered channel, and extract energy when water is returned into ocean.

Oscillating water column: waves causes air to flow up through a turbine. When water receeds, the turbine continues to go the same way due to clever design (Wells turbine).

28
Q

Name one way of harnessing tidal power.

A

By having a turbine in a bay. When the tide comes in, the turbine is run, and when the tide goes out the turbine is run again.

29
Q

Name one big advantage of wave power compared to for example solar power.

A

The available energy corresponds to our demand for energy.