Does Atmospheric Viscous Drag Affect Upper Atmosphere Rotation and Air Movement?

In summary, the Earth's surface pulls the lower atmosphere with viscous drag effects, while the upper atmosphere rotates with a slower absolute tangential velocity. This difference in velocities causes a pressure difference that can result in significant movement of air towards the Earth, known as the Bernoulli effect. However, according to Newton's 1st law, no force is required to keep the atmosphere rotating with the Earth. The direction of wind, whether easterlies or westerlies, is determined by the Coriolis effect acting on vertical convection.
  • #1
the4thamigo_uk
47
0
I guess the Earth's surface pulls around the lower atmosphere with viscous drag effects? What about the upper atmosphere? Does it rotate with a slower absolute tangential velocity? If so, is there any pressure difference that caused by the difference in velocities that would cause any significant movement of air towards the Earth (i.e. bernoulli effect).
 
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  • #2
Based-on Newton's 1st law, no force is required to keep the atmosphere rotating with the earth.
 
  • #3
There are "easterlies" (trade winds) that flow in the direction of the Earth's rotation, or "westerlies" that flow opposite, depending on the distance from the equator.

http://en.wikipedia.org/wiki/Trade_wind
 
  • #4
Those are caused by the coriolis effect acting on vertical convection.
 
  • #5


Atmospheric viscous drag is the force that opposes the motion of an object through a fluid, in this case, the Earth's atmosphere. This drag is caused by the interaction between the object and the molecules of the fluid. In the case of the Earth, the surface does indeed pull the lower atmosphere with viscous drag effects. However, the upper atmosphere is also affected by this drag, although to a lesser extent due to its lower density.

The rotation of the Earth does indeed result in a difference in tangential velocity between the lower and upper atmosphere. This is known as the Coriolis effect and it causes the upper atmosphere to rotate with a slower absolute tangential velocity compared to the lower atmosphere. This difference in velocities can lead to pressure differences, which in turn can cause air to move towards the Earth's surface. This is known as the Bernoulli effect.

However, it is important to note that this movement of air towards the Earth's surface is not solely caused by the difference in velocities. Other factors such as temperature, humidity, and air pressure also play a role in the movement of air in the atmosphere. Additionally, the Earth's rotation and the Coriolis effect also play a significant role in the movement of air masses in the atmosphere.

In summary, atmospheric viscous drag is an important force that affects the movement of air in the Earth's atmosphere. It is caused by the interaction between the Earth's surface and the molecules of the atmosphere. The rotation of the Earth does result in a difference in velocities between the lower and upper atmosphere, which can lead to pressure differences and the movement of air towards the Earth's surface. However, other factors and forces also play a significant role in the overall dynamics of the Earth's atmosphere.
 

1. What is atmospheric viscous drag?

Atmospheric viscous drag is the resistance force that acts on an object as it moves through a fluid, such as air. It is caused by the friction between the object's surface and the molecules of the fluid.

2. How does atmospheric viscous drag affect the movement of objects?

Atmospheric viscous drag slows down the movement of objects by exerting a force in the opposite direction of the object's motion. This force increases as the speed of the object increases.

3. What factors affect the magnitude of atmospheric viscous drag?

The magnitude of atmospheric viscous drag is affected by the shape and size of the object, the density and viscosity of the fluid, and the speed at which the object is moving through the fluid.

4. How is atmospheric viscous drag calculated?

The calculation of atmospheric viscous drag involves the use of fluid dynamics equations, which take into account the aforementioned factors, as well as the Reynolds number, which is a dimensionless value that describes the ratio of inertial forces to viscous forces.

5. How can atmospheric viscous drag be reduced?

Atmospheric viscous drag can be reduced by minimizing the surface area of the object, streamlining its shape, and reducing its speed. Additionally, using materials with lower drag coefficients can also help reduce atmospheric viscous drag.

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