GEOPOTENTIAL HEIGHT VS. GEOMETRIC HEIGHT, 
LATITUDE DEPENDANCE OF CORIOLIS PARAMETER AND GRAVITY


At any latitude height1.jpg , the Coriolis parameter f and the acceleration due to gravity g are :

height2.jpg


height3.jpg


where height4.jpg is the earth's rotation rate (= height5.jpg )

The relationship between geopotential height (H) and geometric height (Z)  is that

height6.jpg


where go is the standard acceleration due to gravity (=9.80665 m s-2), and height7.jpg is the geopotential energy.

The conversion between geometric height (Z) and geopotential height (H) is :

height8.jpg


where G is the gravity ratio

height9.jpg


and Re is the radius of the earth at latitude height10.jpg ,

height11.jpg


where Rmax is the earth's equatorial radius (= 6378.137 kilometers) and Rmin is the earth's polar radius ( = 6356.752 kilometers). 



Reference :

Federal Meteorological Handbook No. 3 : Rawinsonde and Pibal Observatoins. OFCM, May 1997.
http://www.ofcm.gov/fmh3/text/default.htm


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