I'm using Breach_depression_least_cost to fix a DTM. I am accessing it via the latest version of the python API (not workflows).
I apologies in advance here because I've been unable to produce a small dataset that replicates the problem. For this reason, I suspect that the issue may lie with the dataset itself, but if so I haven't been able to work out exactly how.
There are two issues. Firstly the breach depressions gives different results every time. Wildly different. Is this expected?
The other, more pressing issue, is that it creates high plateaus over topographic highs. I've included an image of several versions of the breach depressions output as seen by the profile tool in QGIS. The black line is the input DEM, all other profiles are output from breach depressions.
The output of some of them look as expected in places - e.g. filling lakes and other depressions. But why would it create these very high plateaus over the topo highs? In this example adding almost 150m of elevation.
This profile is a very small section of a very large DTM - the section was chosen entirely at random, the issue occurs everywhere.
I appreciate that there isn't a huge amount that you can do without data to work on. But perhaps can you tell me whether the variability between runs is expected? And possibly suggest some kind of data error that could prompt this behaviour.
Many thanks,
Rick
I'm using Breach_depression_least_cost to fix a DTM. I am accessing it via the latest version of the python API (not workflows).
I apologies in advance here because I've been unable to produce a small dataset that replicates the problem. For this reason, I suspect that the issue may lie with the dataset itself, but if so I haven't been able to work out exactly how.
There are two issues. Firstly the breach depressions gives different results every time. Wildly different. Is this expected?
The other, more pressing issue, is that it creates high plateaus over topographic highs. I've included an image of several versions of the breach depressions output as seen by the profile tool in QGIS. The black line is the input DEM, all other profiles are output from breach depressions.
The output of some of them look as expected in places - e.g. filling lakes and other depressions. But why would it create these very high plateaus over the topo highs? In this example adding almost 150m of elevation.
This profile is a very small section of a very large DTM - the section was chosen entirely at random, the issue occurs everywhere.
I appreciate that there isn't a huge amount that you can do without data to work on. But perhaps can you tell me whether the variability between runs is expected? And possibly suggest some kind of data error that could prompt this behaviour.
Many thanks,
Rick