Known Discrepancies and Changes

This is a non-exclusive list of known differences between LITAP and R. A. (Bob) MacMillan’s original LandMapR. Some differences reflect differences in the programming techniques, some reflect deliberate changes.

General differences

Missing variables

Some variables are not included in LITAP if they are not necessary. For example, the inverted DEMs originally included Vol2Fl, MM2Fl and PArea, but LITAP does not include these values because they aren’t calculated specifically for the inverted DEM, but are identical to those in the non-inverted DEM.

Renamed variables

Some variables have been renamed in LITAP for consistency. See the variables article for an overview

Flat areas (where all cells are the same elevation)

When we have an area with flat cells, LITAP uses a different way of assigning the direction of flow than the original program (in order to speed things up). This results in small differences in flow directions over flat areas.

Rounding error

Sometimes, rounding error on very small numbers can result in quite large differences especially when looking at percentages, etc.

Compounding differences

Adding changes in flow direction to small differences in rounding error can result in larger differences when adding up measures over all cells in a watershed. These should be considered stochastic differences. However if things look really different, contact us and let us know!

`flow_mapper()` and FlowMapR

Pond/Fill/Pit files

PitAreas sometimes larger because of LITAP works with elevation slices. PitArea is all cells upto PourElev. LandMapR worked by spiralling up the cells. PitArea is total area up to PourPoint cell (not necessarily all cells at the PourElev)
Nextpit is often incorrect for Pond Data (not sure why)
DrainsTo isn’t always updated in original LandMapR (not sure if represents something missing in LITAP or bug in LandMapR)
Exact location of pour point between two watersheds is sometimes off by a cell or two (out rec and in rec) due to tie breaking
PitRecs in big patches of equal elevation are in the centre of the patch in LITAP, but at the bottom of the patch in FlowMapR
Sometimes rounding difference on the InElev and/or PourElev.

Dem file

The calculations for Vol2Fl/mm2fl/parea are sometimes off, if the upslope calculations are slightly different (generally due to tie breaking)

idem/ipit

DrainsTo in LITAP is a real shed, whereas in FlowMapR it is often 0, not sure of why the differences

`form_mapper()` and FormMapR

Underlying differences in upslope area can have cascade effects on form_mapper() calculations
The total area of a given cell can sometimes be off between LITAP and FormMapR due to in tie-breaking determining which cell is evaluated first.

`wepp_mapper()` and WeppMapR

In the original WeppMapR, there was a bug resulting in some pit cells being marked as belonging to channels they were nowhere near. This may result in some differences between the output of the two programs.

Note also that the use of “top”, “left”, and “right” is consistent between LITAP and FlowMapR, but its usage isn’t quite consistent within the programs. “Top” refers to coming in from the top to the cell (direction of flow is downwards). Whereas “right” and “left” refer to the direction of flow (towards the right, coming in to the cell from the left and vice versa). We leave this as is to be consistent with FlowMapR but may change this in future.

Further, there are still some discrepancies in the exactly how different segments and hillslopes are named which has yet to be figured out.