Where " ? " is the variation of the Coriolis parameter with latitude.
2.
Where f is the Coriolis parameter 2 \ Omega \ sin \ varphi, introduced above ( where \ varphi is the latitude ).
3.
Using a constant Coriolis parameter prevents the formation of beta gyres which are largely responsible for the North-westward direction of most tropical cyclones.
4.
In reality, the Coriolis parameter varies with latitude, and so the f-plane approximation is not appropriate when considering flows over large lengthscales.
5.
Thus the Coriolis parameter, f, is the angular velocity or frequency required to maintain a body at a fixed circle of latitude or zonal region.
6.
Because these waves are equatorial, the Coriolis parameter vanishes at 0 degrees; therefore, it is necessary to use the equatorial beta plane approximation that states:
7.
Diego Garcia is at minimum risk from tropical cyclones due to its proximity to the equator where the coriolis parameter required to organise circulation of the upper atmosphere is minimal.
8.
Where f is the Coriolis parameter, v is the azimuthal ( i . e . rotating ) wind speed, and r is the radius to the axis of rotation.
9.
:: The large-scale oceanic gyres are clockwise in the Northern Hemisphere and counter-clockwise in the Southern Hemisphere, because of the differing sign of the Coriolis parameter.
10.
He also developed a simple theory of the general ocean circulation postulating a dynamical vorticity balance between the wind-stress curl and the meridional gradient of the Coriolis parameter, the Sverdrup balance.
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