Gonzalo:

I've added the following 3 files to the /pub/foster directory
on hao.hao.ucar.edu:

-rw-r--r--   1 foster   staff     584066 Feb  9 09:16 tejsmdx_utzp.ps
-rw-r--r--   1 foster   staff     572728 Feb  9 09:16 tejspdx_utzp.ps
-rw-r--r--   1 foster   staff     640140 Feb  9 09:16 tejsxdx_utzp.ps

Each file has 8 frames, all with ut on x-axis and log p on y-axis:

frame 1: tn at lat,lon -82.5,30.
frame 2: tn at lat,lon -82.5,120.
frame 3: tn at lat,lon -82.5,-150.
frame 4: tn at lat,lon -82.5,-60.

frame 5: vn at lat,lon -82.5,30.
frame 6: vn at lat,lon -82.5,120.
frame 7: vn at lat,lon -82.5,-150.
frame 8: vn at lat,lon -82.5,-60.

As you know, Ray's model uses the -180 to +180 longitude scale,
so your request for 210 degrees is -150 on the plots, and 300 deg
is -60.

The top 2 south latitude grid points in the model are -82.5 and
-87.5. I more or less arbitrarilly used -82.5, since I'm not
doing interpolation between grid points.  Note, however, that 
because this is so high in latitude, there won't be much meaningful 
difference around the longitudes for scalar fields like tn. 

Also, remember that the vn convention is +N -S, so a physically 
constant wind will show a sign change across the pole. Thus, the
vn plots which are 180 across from each other (30 and -150 or
120 and -60) will be approximate mirror images of each other in
terms of sign.  As you go around the circle vn (and un) will follow 
a sine curve to describe a physically constant wind.

I'm sure you are aware of all this -- I'm reviewing it partly
for my own clarification.

I would love to see N.Z. some day. I've been thinking about a
temporary house swap with my friend Peter Koons in Otago, but family
matters and expense complicate the issue, as you can imagine.

--Ben