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\(f = 2\Omega\sin(\phi)\), which vanishes at the equator. A grid spanning it would divide by something arbitrarily close to zero, so the band where that happens is returned as NA rather than as a very large Rossby number that looks like a real signal.

Usage

coriolis(rast)

Arguments

rast

a SpatRaster, used for its geometry only

Value

a SpatRaster of f, in s^-1