Chapter 4 - Energy from Waves and Tides Flashcards
How are waves created?
By friction of wind with water surface.
What is the Bernoulli equation?
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).
Draw a deep ocean wave.
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.
Does the water molecules of a wave move laterally?
Not averaged over time.
Calculate the wave speed.
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)
What can be said about the dispersion of deep ocean waves?
They have a large dispersion. The longer the wave lengths, the faster they move.
What is the wave speeds dependence on surface tension?
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).
How does the speed of gravitational waves scale? What is the condition for gravitational waves?
Condition: lambda > 10cm. Scales with sqrt(lambda).
How does the speed of capillary waves scale? What is the condition for capillary waves?
Condition: lambda < 1 cm. Scales with sqrt(1/lambda).
How does the equation for wave velocity look for shallow water waves?
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.
What is the condition for shallow water waves?
d < lambda/4.
What is the reason for the destructive effect of tsunamis?
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.
Estimate the energy of a wavefront of breadth b = 1km, with an amplitude A = 2.5 m, and wavelength lambdaw = 50m. Assume sinusoidal shape.
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
Derive the expression for the power per meter of a wave.
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
Describe the origin of the solar tide in the global ocean model.
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.