On Monday 07 January 2008 22:28, Curtis Olson wrote:
> On Jan 7, 2008 3:51 PM, Frederic Bouvier <> wrote:
> > If we keep the same triangle budget for every tile, we will
> > have sparse data and
> > features at the equator and much more than what is really
> > needed at the poles,
> > just because the area covered by each tile will vary greatly (
> > proportional to
> > 1/cos( lat ) if my math is ok )
>
> My gut feeling is that once you get up (or down) into the
> latittudes where the tiles get significantly skinny, the
> resolution of the available data drops of significantly.  We
> really don't have a per-tile triangle budget anyway.  The only
> place where I see this making a difference is the concentration
> of terrain elevation points would increase, but this is up in an
> area where we only have very low res terrain data anyway.  SRTM
> drops out beyond +/- 60 degrees latitude.
>
> Regards,
>
> Curt.

Yup - I downloaded lots of SRTM data to play with in GRASS and 
above/below +/- 60 lat it isn't there.

There doesn't seem to be any alternative source of suitable data 
either so I don't see how FG can cover the poles.

(the reason I was looking was because I was interested in the Mt 
Erebus volcano - FG is quite good for looking at volcanos and other 
large scale geological features from the air - at some point I'll 
get together a list of volcanos and astroblemes for the 'places to 
fly' section of the FG docs/wiki)

LeeE

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