I've been looking through some of fishlipsatwork DEMs, spending a significant time on the Mohawk-Albany-Binghamton <kuid2:59012:103143:1> mega-line.
The DEM has around 70 miles of the Mohawk river. While trying to see how to lay prototypical track around this river I noticed that the river is a great calibrating tool to match the DEM data and Tiger lines.
By filling the riverbeds with water I can see how close the Tiger lines indicating the river shore are close to the actual DEM data. This gives a good indication about how far off the track Tiger lines are for the initial placement of track.
I noticed that for the most part the riverbed is perfectly flat. Moving up river the height of the riverbed periodically increases sharply. I assume this is where two DEM datasets were merged and that each had a different height (probably averaged across the dataset). The riverbanks at these points blend seamlessly, but the river itself has a somewhat steep drop.
I cannot see a way to model the river using this DEM data. The land around the Mohawk river slopes gradually downwards across it's length. Over 60 miles this creates quite a height difference. If I use the water level at it's western most point the river would flood the entire tri-city area. If I use it at it's eastern point I would need to create deep chasms in the west for the water to flow in, which doesn't look right at all.
To those of you who are using DEM data with rivers, how do you handle the differing heights of the river?
The DEM has around 70 miles of the Mohawk river. While trying to see how to lay prototypical track around this river I noticed that the river is a great calibrating tool to match the DEM data and Tiger lines.
By filling the riverbeds with water I can see how close the Tiger lines indicating the river shore are close to the actual DEM data. This gives a good indication about how far off the track Tiger lines are for the initial placement of track.
I noticed that for the most part the riverbed is perfectly flat. Moving up river the height of the riverbed periodically increases sharply. I assume this is where two DEM datasets were merged and that each had a different height (probably averaged across the dataset). The riverbanks at these points blend seamlessly, but the river itself has a somewhat steep drop.
I cannot see a way to model the river using this DEM data. The land around the Mohawk river slopes gradually downwards across it's length. Over 60 miles this creates quite a height difference. If I use the water level at it's western most point the river would flood the entire tri-city area. If I use it at it's eastern point I would need to create deep chasms in the west for the water to flow in, which doesn't look right at all.
To those of you who are using DEM data with rivers, how do you handle the differing heights of the river?