(from the article `ocean`) ...where g is the acceleration of gravity, is the density of seawater, which increases with depth, and z is the depth below the sea surface. This is ...
Found on
http://www.britannica.com/eb/a-z/h/89
In the vector equation of motion, the form assumed by the vertical component when all Coriolis, earth-curvature, frictional, and vertical-acceleration terms are con- sidered negligible compared with those involving the vertical pressure force and the force of gravity. The error in applying the hydrostatic equation to the atmosphere for cyclonic-sca...
Found on
https://www.encyclo.co.uk/local/20128
No exact match found.
