Ekman Surface Pumping in Polar Coordinates?

In summary: Your Name]In summary, the forum member is seeking help in converting the Ekman pumping equation to polar coordinates in order to understand why tea leaves collect in the center of a cup, regardless of the direction in which the tea is stirred. They have provided the equation and necessary variables, and have mentioned that the stress from the bottom of the cup will always be in the angular direction in polar coordinates. The expert has provided the necessary conversion equations and has explained that the sign on the Coriolis parameter will not change in the polar version of the equation, allowing for the upward motion of w to still occur.
  • #1
xtamx
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Hello,

I am working on a question in a GFD textbook about tea leaves collecting in the center of the cup regardless of the direction that the tea is stirred. I have an idea of why this is the case but to prove it I need to convert the equation for Ekman pumping to polar coordinates. Its given as:

w = 1/ρf (∂τy/∂x - ∂τx/∂y)

where w is the fluid velocity in the vertical direction
ρ is the fluid density
f is the Coriolis parameter (or rotation rate in the tea cup)
τx and τy are the stresses on the fluid from the walls of the cup

The stress from the bottom of the cup is always going to be in the angular direction in polar coordinates so the net transport will always be in the radial direction according to Ekman dynamics. If the polar version of the above equation is similar then the sign on f changes to negative then the sign on τθ also changes and w remains upward.

The problem is that I have no idea how to convert that to polar coordinates. Can anyone help?
 
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  • #2




Thank you for your interesting question about tea leaves collecting in the center of a cup. Based on the information provided, it seems that the Ekman pumping equation is relevant in explaining this phenomenon. However, to fully understand and prove this, it is necessary to convert the equation to polar coordinates.

To do this, we can use the following conversion equations:

∂/∂x = cos(θ) ∂/∂r - sin(θ)/r ∂/∂θ
∂/∂y = sin(θ) ∂/∂r + cos(θ)/r ∂/∂θ

Using these equations, we can rewrite the Ekman pumping equation in polar coordinates as:

w = 1/ρf (cos(θ) ∂τy/∂r - sin(θ)/r ∂τy/∂θ - sin(θ) ∂τx/∂r - cos(θ)/r ∂τx/∂θ)

From this equation, we can see that the stress from the walls of the cup, τx and τy, will have both radial and angular components. However, the Coriolis parameter, f, will only have an angular component, as it represents the rotation rate in the tea cup. Therefore, the sign on f will not change in the polar version of the equation and the upward motion of w will still be maintained.

I hope this helps in your understanding and further exploration of this interesting phenomenon. If you have any further questions or need clarification, please do not hesitate to ask. Keep up the great work in your studies!


 

Related to Ekman Surface Pumping in Polar Coordinates?

1. What is Ekman surface pumping in polar coordinates?

Ekman surface pumping in polar coordinates is a phenomenon in fluid dynamics that describes the vertical transport of water due to the combined effects of wind and Earth's rotation. This pumping motion occurs near the Earth's surface and is influenced by the Coriolis force, which is strongest at the poles.

2. How does Ekman surface pumping affect ocean circulation?

Ekman surface pumping plays a crucial role in driving ocean circulation patterns. The pumping motion creates a net transport of water that contributes to the formation of ocean currents. This can have significant impacts on global climate and marine ecosystems.

3. What factors influence Ekman surface pumping?

The strength and direction of the wind, as well as the latitude and Coriolis force, are major factors that influence Ekman surface pumping. In polar coordinates, the Coriolis force is strongest at the poles, which can result in stronger pumping motion in these regions.

4. How is Ekman surface pumping measured?

Ekman surface pumping can be estimated through a variety of methods, including satellite observations, ocean buoys, and numerical models. These measurements can provide valuable data on the patterns and variability of Ekman surface pumping in different regions.

5. What are the potential applications of understanding Ekman surface pumping?

Understanding Ekman surface pumping can have practical applications in fields such as oceanography, meteorology, and climate science. It can also aid in predicting and managing the impacts of ocean currents on coastal regions, shipping routes, and marine ecosystems.

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