When considering a new hike, I often want to know the elevation profile of the route. Usually all I have is a 2D elevation track, from OpenStreetMap for instance; clearly this lacks elevation information.
Unrelatedly we have access to gridded elevation data. This primarily comes from the SRTM project: data available here: http://dds.cr.usgs.gov/srtm/version2_1/. The raw SRTM data is pretty good, but there are some gaps. Some people have cleaned up the raw data, to make clean tiles available. One such data source is here: http://www.viewfinderpanoramas.org/dem3/.
So we have 2D track data and topography. We can thus combine these into a full 3D track. This isn't perfect since DEM data is granular, but it's way better than nothing.
I just found out that there's a route to Fish Canyon Falls that goes around the rock quarry, and thus is open year-round. Bypassing the quarry requires climbing up a steep hillside to gain a ridge, then descending the other side of the ridge to the bottom of the canyon behind the quarry. Just how much extra climbing is involved here? To find out, I wrote this:
#!/usr/bin/perl use strict; use warnings; use Getopt::Euclid; use feature ':5.10'; use autodie; use Geo::Gpx; use PDL; my $W = 1201; # I use 3-minute DEMs, so each DEM is 1201 x 1201 my $gpx_fh; if( $ARGV{'<input>'} eq '-' ) { $gpx_fh = \*STDIN; } else { open $gpx_fh, '<', $ARGV{'<input>'}; } my $gpx = Geo::Gpx->new( input => $gpx_fh ); my $iter = $gpx->iterate_points(); while( my $pt = $iter->() ) { say join( ' ', $pt->{lon}, $pt->{lat}, elevation( $pt->{lon}, $pt->{lat} ) ); } sub elevation { my ($lon, $lat) = @_; state %DEMs; my $demfileE = floor $lon; my $demfileN = floor $lat; $DEMs{$demfileE}{$demfileN} //= readDEM($demfileE, $demfileN); my $dem = $DEMs{$demfileE}{$demfileN}; return 0 if( !ref($dem) ); # use PDL::Graphics::Gnuplot; # gplot( with => 'image', $dem ); # sleep(20); # the DEMs start in the NW corner my $ilon = ($lon - $demfileE) * $W; my $ilat = (1 - ($lat - $demfileN)) * $W; return 100.0/2.54/12.0 * $dem->interpND( pdl[$ilon, $ilat] ); } sub readDEM { my ($demfileE, $demfileN) = @_; my $path; if ($demfileN >= 0 && $demfileE >= 0){ $path = sprintf("$ARGV{'--demdir'}/N%.2dE%.3d.hgt", $demfileN, $demfileE); } elsif($demfileN >= 0 && $demfileE < 0){ $path = sprintf("$ARGV{'--demdir'}/N%.2dW%.3d.hgt", $demfileN, -$demfileE); } elsif($demfileN < 0 && $demfileE >= 0){ $path = sprintf("$ARGV{'--demdir'}/S%.2dE%.3d.hgt", -$demfileN, $demfileE); } else { $path = sprintf("$ARGV{'--demdir'}/S%.2dW%.3d.hgt", -$demfileN, -$demfileE); } say STDERR "Reading DEM '$path'"; if( ! -e $path ) { warn "DEM '$path' not found. All of its elevations will read as 0"; return 0; } # I read the DEM on disk into the piddle, then flip the endianness of the # data. I wouldn't have to copy anything if the data was little-endian to # start with; I'd just mmap into the piddle. open my $fd, '<', $path; my $dem = zeros(short, $W, $W); sysread( $fd, ${$dem->get_dataref}, $W*$W*2, 0 ); ${$dem->get_dataref} = pack( "s*", unpack("s>*", ${$dem->get_dataref})); # I also convert to floating point. Turns out the PDL interpolation routines # don't work with integers return $dem->float; } __END__ =head1 NAME gpxSampleDEM.pl - Samples SRTM DEM data to compute elevations for a GPX track =head1 OPTIONAL ARGUMENTS =over =item --demdir <demdir> Directory that contains the DEM files =for Euclid: demdir.type: string, -d demdir && -e demdir demdir.default: '.' =item <input> GPX input. If omitted or '-', the input is read from standard input =for Euclid: input.type: readable input.default: '-' =back =head1 AUTHOR Dima Kogan, C<< <dima@secretsauce.net> >>
The script is fairly straightforward. It examines every track point in the GPX, finds the appropriate elevation using plain bilinear interpolation, and outputs a (lon,lat,ele) tuple on STDOUT. On Debian the dependencies are
libgetopt-euclid-perl
libgeo-gpx-perl
pdl
You need to pre-download 3" DEMs, and pass the directory to the script (1" would certainly work better, but I haven't tried). Given the gpx file scraped from an OpenStreetMap way (itself traced from the satellite imagery), you can do this:
gpxSampleDEM.pl --demdir DEMs FishCanyonFallsTrail.gpx | \ feedgnuplot --domain --3d --lines --square_xy \ --xlabel 'lon(deg)' --ylabel 'lat(deg)' --zlabel 'Elevation(m)'
This makes an interactive 3D plot of the route. For a more traditional elevation profile that's monotonic in distance, you can do something like this:
gpxSampleDEM.pl --demdir DEMs FishCanyonFallsTrail.gpx | \ awk '{print $3}' | \ feedgnuplot --lines \ --xlabel 'Monotonic with distance' --ylabel 'Elevation(m)'
I actually did go see this waterfall today (which is really nice). Here's a plot of the elevation profile I gathered with my GPS unit today overlaid over the elevation profile from the DEM:
Immediately several issues are noticeable1. First of all, while each curve is monotonic with distance, the relationship of the domain with distance is different. This plot assumes they're both linear with distance. It's not really true, but close enough I suppose.
Second, we see that the DEM curve has some high-frequency oscillations. Those are switchbacks that sample the DEM in a way that the DEM data is too coarse to represent. The trail does not really oscillate like that, which is confirmed by the GPS track. This effect would probably be mitigated with finer DEM data (1" DEMs are available), but I haven't attempted this.
Third, we see that during the initial climb the DEM-derived elevation consistently underreports the elevation. I suspect this is another artifact of the coarseness of the DEM. If we're walking on a ridge, a bilinear interpolation would take into account neighboring DEM pixels, which would be lower in elevation (since it's a ridge). So on a ridge I would expect the DEM-derived elevations to be under-reported, and in a canyon I'd expect them to be over-reported. In this particular track, the initial climb and the initial descent are on ridges, while the second climb is in a canyon. This brings us to the next point.
The data in the second climb doesn't match at all. Here it's the GPS data that's at fault. The canyon walls block the GPS signal, so GPS readings are unreliable there.
So the grand conclusion of all this would appear to be that you can use 3" DEM data to derive an elevation profile, but one should not expect this profile to be terribly accurate. Still it's useful. Based purely on the DEM, I can see that a round-trip on this route would entail 2800ft of net elevation gain. Seeing the real track, this probably is an underestimate of ~200ft. Not bad.
Footnotes:
The above analysis assumes that the implementation of the DEM sampler is bug-free and that the DEM data is correct. While I don't know of any bugs, there could be some. Same for the DEM data