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Data files for some examples
Example pages containing:
NCL version 4.2.0.a033 is required to use omega_ccm_driver
This example shows how to compute omega from CCM output using the contributed.ncl
. The CCM computed omega is also read in,
and both omegas are overlaid on the plot. As one can see, they are identical. Due to
the fact that the CCM model computes omega in double precision, and the default CCM model
output precision is single precision, the omega output by the CCM model and omega_ccm_driver will
agree to at least the 5th significant digit.
The special resource gsnXRefLine is used
to draw a vertical line at x=0.0.
The contributed.ncl library must be loaded prior to the use of
This example shows how to calculate omega using the kinematic method outlined in
Atmospheric Science, An Introductory Survey by Wallace and Hobbs
(eqn 8.20), as well as by using the O'Brian adjusted method outlined in
Synoptic-Dynamic Meteorology in Midlatitudes by Bluestein (Volume I: pp315-316).
The output from these two methods is compared to the omega calculated in the same fashion as
in Example 1
The main difference between the kinematic method and the O'Brian adjusted method is that the O'Brian
method insures that omega goes to 0 at the top of the atmosphere.