rsaga.local.morphometry
.
rsaga.slope.asp.curv(in.dem, out.slope, out.aspect, out.cgene, out.cprof, out.cplan, out.ctang, out.clong, out.ccros, out.cmini, out.cmaxi, out.ctota, out.croto, method = "poly2zevenbergen", unit.slope = "radians", unit.aspect = "radians", env = rsaga.env(), ...)
.sgrd
)"maxslope"
)
"maxtriangleslope"
)
"lsqfitplane"
)
"poly2evans"
)
"poly2heerdegen"
)
"poly2bauer"
)
"poly2zevenbergen"
)
"poly3haralick"
)"radians"
):
"radians"
"degrees"
"percent"
"radians"
):
"radians"
"degrees"
rsaga.env
rsaga.geoprocessor
intern
argument passed to the rsaga.geoprocessor
. For intern=FALSE
it is a numerical error code (0: success), or otherwise (default) a character vector with the module's console output.
out.cprof
, out.cplan
) changed in SAGA GIS 2.1.1+ compared to earlier versions. See the following thread on sourceforge.net for an ongoing discussion: http://sourceforge.net/p/saga-gis/discussion/354013/thread/e9d07075/#5727
Jones KH (1998) A comparison of algorithms used to compute hill slope as a property of the DEM. Computers and Geosciences. 24 (4): 315-323.
References on specific methods:
Maximum Slope:
Travis, M.R., Elsner, G.H., Iverson, W.D., Johnson, C.G. (1975): VIEWIT: computation of seen areas, slope, and aspect for land-use planning. USDA F.S. Gen. Tech. Rep. PSW-11/1975, 70 p. Berkeley, California, U.S.A.
Maximum Triangle Slope:
Tarboton, D.G. (1997): A new method for the determination of flow directions and upslope areas in grid digital elevation models. Water Ressources Research, 33(2): 309-319.
Least Squares or Best Fit Plane:
Beasley, D.B., Huggins, L.F. (1982): ANSWERS: User's manual. U.S. EPA-905/9-82-001, Chicago, IL, 54 pp.
Costa-Cabral, M., Burges, S.J. (1994): Digital Elevation Model Networks (DEMON): a model of flow over hillslopes for computation of contributing and dispersal areas. Water Resources Research, 30(6): 1681-1692.
Fit 2nd Degree Polynomial:
Evans, I.S. (1979): An integrated system of terrain analysis and slope mapping. Final Report on grant DA-ERO-591-73-G0040. University of Durham, England.
Bauer, J., Rohdenburg, H., Bork, H.-R. (1985): Ein Digitales Reliefmodell als Vorraussetzung fuer ein deterministisches Modell der Wasser- und Stoff-Fluesse. Landschaftsgenese und Landschaftsoekologie, H. 10, Parameteraufbereitung fuer deterministische Gebiets-Wassermodelle, Grundlagenarbeiten zur Analyse von Agrar-Oekosystemen, eds.: Bork, H.-R., Rohdenburg, H., p. 1-15.
Heerdegen, R.G., Beran, M.A. (1982): Quantifying source areas through land surface curvature. Journal of Hydrology, 57.
Zevenbergen, L.W., Thorne, C.R. (1987): Quantitative analysis of land surface topography. Earth Surface Processes and Landforms, 12: 47-56.
Fit 3.Degree Polynomial:
Haralick, R.M. (1983): Ridge and valley detection on digital images. Computer Vision, Graphics and Image Processing, 22(1): 28-38.
For a discussion on the calculation of slope by ArcGIS check these links:
http://forums.esri.com/Thread.asp?c=93&f=1734&t=239914
http://webhelp.esri.com/arcgisdesktop/9.2/index.cfm?topicname=how_slope_works
rsaga.local.morphometry
, rsaga.parallel.processing
, rsaga.geoprocessor
, rsaga.env
## Not run:
# # Simple slope, aspect, and general curvature in degrees:
# rsaga.slope.asp.curv("lican.sgrd", "slope", "aspect", "curvature",
# method = "maxslope", unit.slope = "degrees", unit.aspect = "degrees")
# # same for ASCII grids (default extension .asc):
# rsaga.esri.wrapper(rsaga.slope.asp.curv,
# in.dem="lican", out.slope="slope",
# out.aspect = "aspect", out.cgene = "curvature",
# method="maxslope", unit.slope = "degrees", unit.aspect = "degrees")
# ## End(Not run)
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