[OSM-talk] The long tail - lowest common denominator
Nick Black
nickblack1 at gmail.com
Mon Jul 10 09:17:29 BST 2006
On 7/9/06, Lars Aronsson <lars at aronsson.se> wrote:
> Nick Black wrote:
>
> > I'm not sure that I am following you Lars - do you mean that we could
> > use automatic feature detection to detect the edges of water features?
>
> Yes, that's what I was philosophizing about. But I haven't tried
> it or even planned to try it. I'm far too lazy for that.
One of the most significant features of the SRTM as a global dataset
is that it is self-consistent and internal errors fall within
specified and documneted thresholds. This was acheived by a lot of
post-processing work. Part of the work involved created a global
water bodies mask at the same scale (1 arc-second/3 arc-sec) as the
complete topographic dataset.
The mask is called the SWBD. It is supplied in ESRI shapefile format
and is downloadable from the same ftp site as the SRTM data:
ftp://e0srp01u.ecs.nasa.gov/srtm/version2/
So thats cool - Free 3-arc-sec water body data. Well, its only as
cool as the one degree tiles that it is supplied in. If someone could
process this data to derive a complete water-bodies mask it would be
invaluable to OSM and to other projects. A derived version of the UK
SWBD is already up on Chris's OSM freemap site, where is really shows
up the VMAP data (shows how coarse it is).
Nick
>
> The Landsat images are not perfect, of course, but they do show
> rivers and lakes in some greater detail than the VMap0 data.
> Except where white clouds hide every detail (such as over
> Trondheim), and except where some other dark features appear (such
> as railroads), the dark blue is water and the rest is land. Just
> filter out the dark blue, and you have a rough estimate of where
> the water is. Combine this rough estimate with the one given by
> VMap0, and you should be able to arrive at something better.
>
>
> --
> Lars Aronsson (lars at aronsson.se)
> Aronsson Datateknik - http://aronsson.se
>
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