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cyclonic. anti-cyclonic. geostrophic circulation with relative vorticity. leads to. frictional boundary layer flow from high to low pressure. y.  divergence!!!  vertical velocity. x. http://paoc.mit.edu/labweb/lab9/gfd_9.htm.

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slide1

cyclonic

anti-cyclonic

geostrophic

circulation with

relative vorticity

leads to

frictional boundary

layer flow from

high to low pressure

y

 divergence!!!

 vertical velocity

x

http://paoc.mit.edu/labweb/lab9/gfd_9.htm