[Metcal-devel] The inverted wind field from the PV inversion subroutine

[Charles T. <zho...@gm...>]

Dear all,
I've been trying to use the PV inversion subroutine independently from the
whole SPA package.
I was curious about why the calculations of the wind fields from the
inverted stream functions were multiplied by the gravitational constant and
divided by the Coriolis parameter.
Is this the reason that I got enormous values in wind fields?
I'll appreciated any help.
Thank you!
Sincerely,
                                                 Charles Tai