hello,
i was using '1D linear interpolation' to generate constant-head boundary conditions along a river (FeFlow Classic). after river elevations at start point A and B were assigned, a*.shp (or *.lin) was used to join and the method of '1D linear interpolation' was used to generate the values for those nodes along the river between A and B. i checked the interpolated values after interpolation and found at some nodes the interpolated values were actually greater than the values at either A or B. in another word, the interpolated river elevations were 'mounded' somewhere between A and B. i was wondering what may cause this problem. were those node elevations (i.e. river bed topography) considered during the interpolation? your help is greatly appreciated!
thanks in advance
b