|
@@ -68,7 +68,7 @@ watershed basin model. Overland flow units represent the amount of
|
|
|
overland flow each cell contributes to surface flow. If omitted, a
|
|
|
value of one (1) is assumed. The algorithm is D8 flow accumulation.
|
|
|
|
|
|
-<dt><em>disturbed.land</em>
|
|
|
+<dt><em>disturbed_land</em>
|
|
|
|
|
|
<dd>Raster map input layer or value containing the percent of disturbed
|
|
|
land (i.e., croplands, and construction sites) where the raster or input
|
|
@@ -86,11 +86,11 @@ for the RUSLE. Any non-zero values indicate blocking terrain.
|
|
|
<dd>The minimum size of an exterior watershed basin in cells, if no flow
|
|
|
map is input, or overland flow units when a flow map is given.
|
|
|
Warning: low threshold values will dramactically increase run time and
|
|
|
-generate difficult too read basin and half.basin results.
|
|
|
+generate difficult too read basin and half_basin results.
|
|
|
This parameter also controls the level of detail in the <em>stream</em>
|
|
|
segments map.
|
|
|
|
|
|
-<dt><em>max.slope.length</em>
|
|
|
+<dt><em>max_slope_length</em>
|
|
|
|
|
|
<dd>Input value indicating the maximum length of overland surface flow
|
|
|
in meters. If overland flow travels greater than the maximum length,
|
|
@@ -134,7 +134,7 @@ in the current geographic region.
|
|
|
<dd>Output map: stream segments. Values correspond to the watershed
|
|
|
basin values.
|
|
|
|
|
|
-<dt><em>half.basin</em>
|
|
|
+<dt><em>half_basin</em>
|
|
|
|
|
|
<dd>Output map: each half-basin is given a unique value. Watershed
|
|
|
basins are divided into left and right sides. The right-hand side
|
|
@@ -151,7 +151,7 @@ modified to provide for easy display. All negative accumulation values
|
|
|
are changed to zero. All positive values above the basin threshold
|
|
|
are given the value of the <em>threshold</em> parameter.
|
|
|
|
|
|
-<dt><em>length.slope</em>
|
|
|
+<dt><em>length_slope</em>
|
|
|
|
|
|
<dd>Output map: slope length and steepness (LS) factor. Contains the LS
|
|
|
factor for the Revised Universal Soil Loss Equation. Equations taken
|
|
@@ -160,7 +160,7 @@ from <em>Revised Universal Soil Loss Equation for Western Rangelands</em>
|
|
|
Since the LS factor is a small number, it is multiplied by 100 for the
|
|
|
GRASS output map.
|
|
|
|
|
|
-<dt><em>slope.steepness</em>
|
|
|
+<dt><em>slope_steepness</em>
|
|
|
|
|
|
<dd>Output map: slope steepness (S) factor for RUSLE.
|
|
|
Contains the revised S factor for the Universal Soil
|
|
@@ -185,7 +185,7 @@ Kinner et al. (2005), for example, used SRTM and IFSAR DEMs to compare
|
|
|
valleys while <em>r.watershed</em> performed much better. Thus, if forest
|
|
|
canopy exists in valleys, SRTM, IFSAR, and similar data products will cause
|
|
|
major errors in <em>r.terraflow</em> stream output. Under similar conditions,
|
|
|
-<em>r.watershed</em> will generate better <b>stream</b> and <b>half.basin</b>
|
|
|
+<em>r.watershed</em> will generate better <b>stream</b> and <b>half_basin</b>
|
|
|
results. If watershed divides contain flat to low slope, <em>r.watershed</em>
|
|
|
will generate better basin results than <em>r.terraflow</em>.
|
|
|
(<em>r.terraflow</em> uses the same type of algorithm as ESRI's ArcGIS
|