What is Geostrophy and its role in the Earth's core-mantle boundary?

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In summary, geostrophy refers to the balance of forces in a fluid that results in a stable flow pattern. This concept is important in understanding the dynamics of the core-mantle boundary and its implications for Earth's geophysical processes. Several articles and studies have been conducted on this subject, but some may not have considered all relevant factors, such as the precession of the equinoxes.
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Cunicultor
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Geostrophy---> what is it?

Can someone leave some hints about this subject?...

What is in fact geostrophy, and what are the implications of a geostrophic flow at the core-mantle boundary?

Are there any articles available?
 
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  • #2
http://www.agu.org/revgeophys/talley01/node5.html
 
  • #3
Here is more, http://www.iers.org/iers/publications/tn/tn30/tn30_216.pdf
http://www.iers.org/iers/publications/reports/2001/ar2001_074.pdf
http://www.blackwell-synergy.com/links/doi/10.1046/j.1365-246X.2001.00535.x/abs/;jsessionid=c91sulqOtXYg
http://www.dsri.dk/~nio/papers/22.html


however it may seem that the authors overlooked some forces like the precession of the equinoxes.
 
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FAQ: What is Geostrophy and its role in the Earth's core-mantle boundary?

What is geostrophy and why is it important?

Geostrophy is a concept in fluid dynamics that describes the balance of forces in a rotating system. It is important because it helps us understand large-scale atmospheric and oceanic circulation patterns.

How is geostrophy related to the Earth's rotation?

Geostrophy is related to the Earth's rotation through the Coriolis effect, which is the force that causes objects in motion to deviate to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This effect is a result of the Earth's rotation.

What are the two types of geostrophic balance?

The two types of geostrophic balance are thermal wind balance and gradient wind balance. Thermal wind balance occurs when the Coriolis force balances the horizontal pressure gradient force, while gradient wind balance occurs when both the Coriolis force and the centrifugal force balance the horizontal pressure gradient force.

What are some examples of geostrophic flow?

Some examples of geostrophic flow include large-scale atmospheric circulation patterns such as the jet stream and oceanic circulation patterns such as the Gulf Stream.

How is geostrophy used in weather forecasting?

Geostrophy is used in weather forecasting to understand and predict large-scale atmospheric circulation patterns, which can have a significant influence on local weather conditions. It is also used in oceanography to study ocean currents and their impacts on marine ecosystems.

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