How Does the Coriolis Effect Influence Object Displacement at 31.3°S?

In summary, the object is dropped from rest at height H = 40m above the ground at latitude 31.3^{o}S. The Coriolis effect causes the object to move towards the north and upward.
  • #1
QuanticEnigma
34
0

Homework Statement


An object is dropped from rest at height H = 40m above the ground at latitude 31.3[tex]^{o}[/tex]S. Calculate the final displacement, in magnitude and direction, due to the Coriolis effect.


Homework Equations


[tex]
\Omega = \omega \left(
\begin{array}{cc}
0\\
\cos{\varphi}\\
\sin{\varphi}
\end{array}
\right),
v = \left(
\begin{array}{cc}
v_{east}\\
v_{north}\\
v_{upward}
\end{array}
\right),
a_{C} = -2\Omega \times v =
\left(
\begin{array}{cc}
v_{north}\sin{\varphi}-v_{upward}\cos{\varphi}\\
-v_{east}\sin{\varphi}\\
v_{east}\cos{\varphi}
\end{array}
\right)


[/tex]


The Attempt at a Solution



I know that [itex]\omega[/itex] = angular velocity of rotating reference frame (in this case, the earth), and that [itex]\varphi[/itex] = 31.3 degrees, but could someone please give me a few pointers to get started, I'm kind of confused with all this Coriolis business...
 
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  • #2
You forgot a factor of 2Ω in your expression for the acceleration, but otherwise it is OK. To make things simpler, say x = "East", y = "North" and z = "upward". This question is best answered by successive approximations, here to first order will probably be OK.

First write out three differential equations in the form

[tex]\frac{dv_i}{dt}=a_i[/tex]

where i = x, y, and z.

Do that, and I will guide you to the next step.
 
Last edited:
  • #3
[tex]\frac{dv_{x}}{dt} = 2\omega (v_{y}\sin{\varphi} - v_{z}\cos{\varphi})[/tex]


[tex]\frac{dv_{y}}{dt} = 2\omega (-v_{x}\sin{\varphi})[/tex]


[tex]\frac{dv_{z}}{dt} = 2\omega (v_{x}\cos{\varphi})[/tex]

Ok, so I suppose this will give me a velocity vector dependent on time t ... is this correct?

Also, when I integrate the above expressions, what will the limits of integration be?
 
  • #4
What you show is just the Coriolis acceleration, not the acceleration of the free falling mass. You need to add -g to the z-equation and you will have the equations of motion. Let's call these "the original equations of motion". When you integrate, you do so to successively increasing orders of approximation.

Zeroth order
Since the mass is released from rest, to zeroth order, you set vx=0, vy=0 and vz=0. What do the equations become then? Integrate once to get the components of the velocity vector and once again to get the components of the position vector. The limits of integration must be from t = 0 to t = t and the result is something extremely familiar. Use the z-equation to find the time of flight tf.

Do this first and then I will tell you how to move on to the first order correction which is where the effects of the Coriolis acceleration come in.
 
  • #5


The Coriolis effect is a phenomenon that occurs due to the rotation of the Earth. As the Earth rotates, objects that are moving on its surface appear to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This is due to the Coriolis force, which is caused by the Earth's rotation.

To solve this problem, we can use the equations provided in the homework statement. First, we need to calculate the angular velocity of the Earth, \omega. This can be done using the equation \omega = 2\pi/T, where T is the period of rotation of the Earth. The period of rotation of the Earth is approximately 24 hours, so \omega \approx 7.27 \times 10^{-5} rad/s.

Next, we can use the equation for the Coriolis acceleration, a_C, to calculate the final displacement of the object. We know that the object is dropped from rest, so its initial velocity, v, is zero. Therefore, we can simplify the equation to a_C = -2\Omega \times v = -2\Omega \times 0 = 0.

Since the Coriolis acceleration is zero, there is no deflection due to the Coriolis effect. Therefore, the final displacement of the object will be in the same direction as its initial displacement, which is downward. The magnitude of the displacement will be equal to the initial height, H, which is 40m. So, the final displacement is 40m downward.

In summary, the Coriolis effect does not have any effect on the final displacement of the object in this scenario. The object will simply fall straight down with a magnitude of 40m.
 

1. What is the Coriolis effect problem?

The Coriolis effect problem refers to the apparent deflection of moving objects on the surface of the Earth due to the rotation of the Earth. This phenomenon is caused by the difference in rotational speeds between different latitudes.

2. How does the Coriolis effect impact weather patterns?

The Coriolis effect plays a crucial role in the formation of weather patterns. It causes winds to deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This deflection leads to the formation of global wind patterns, such as the trade winds and westerlies, which play a significant role in the distribution of heat and moisture across the Earth's surface.

3. Does the Coriolis effect impact the direction of ocean currents?

Yes, the Coriolis effect also affects the direction of ocean currents. In the Northern Hemisphere, ocean currents are deflected to the right, while in the Southern Hemisphere, they are deflected to the left. This deflection is responsible for the formation of circular ocean currents, such as the Gulf Stream in the Atlantic Ocean and the Kuroshio Current in the Pacific Ocean.

4. How does the Coriolis effect affect the trajectory of projectiles?

The Coriolis effect has a significant impact on the trajectory of projectiles, such as missiles and artillery shells. In the Northern Hemisphere, the deflection of these objects is to the right, while in the Southern Hemisphere, it is to the left. This deflection must be taken into account when aiming these projectiles to ensure accuracy.

5. Is the Coriolis effect responsible for the direction of rotation of hurricanes?

Yes, the Coriolis effect is responsible for the direction of rotation of hurricanes. In the Northern Hemisphere, hurricanes rotate counterclockwise, while in the Southern Hemisphere, they rotate clockwise. This is due to the deflection caused by the Coriolis effect on the winds that drive the rotation of the storm.

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