Hi Kevin-
Kevin L. Manross wrote:
I have a couple questions regarding isosurfacing in the IDV. We are
using it to look at isosurfaces of radar reflectivity and we're noticing
several discontinuities in the vertical when viewing Level II data. Can
anyone tell me what type of interpolation is being used for the
isosurfacing? Is this technique something that can be modified via the
IDV? If not, is it possible for a user (me) to write some sort of
plugin to change this interpolation?
When you say discontinuities, what do you mean? We just fixed a bug
in the 2.2 release where some of the levels were shifted and it made
for some weird isosurfaces. Try out the 2.3 release and see if that
works better for you.
Since radar sweeps in a volume do not have a standard pattern for the
scans (e.g. each sweep starts at a different azimuth and the number
of azimuths may vary by sweep), we normalize the sweeps to a 0-360 set
of azimuths, putting the closest radial to each azimuth in for the data.
This gives us a "rectified" domain which makes the isosurface alogrithm
work better (but maybe not perfect). As to the details, it uses the
standard VisAD algorithm, the details of which I'm not sure of. But
that could be answered by someone on the VisAD list.
Also, I've played around a little with the vertical scaling widget and
it doesn't seem to have any appreciable effect. (I changed my vertical
scale from 16000m to 20000m.) When viewing a radar domain, it would be
great to have the vertical scale of a storm more proportional to its
horizontal scale.
Stu's response is how I do it - use the Range and Bearing tool to
calculate the width of the box, set the vertical aspect to 1 and
set the vertical range accordingly.
Don
*************************************************************
Don Murray UCAR Unidata Program
dmurray@xxxxxxxxxxxxxxxx P.O. Box 3000
(303) 497-8628 Boulder, CO 80307
http://www.unidata.ucar.edu/staff/donm
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