Provided by: grass-doc_7.8.2-1build3_all 
NAME
v.generalize - Performs vector based generalization.
KEYWORDS
vector, generalization, simplification, smoothing, displacement, network generalization, topology,
geometry
SYNOPSIS
v.generalize
v.generalize --help
v.generalize [-lt] input=name [layer=string] [type=string[,string,...]] output=name [error=name]
method=string threshold=float [look_ahead=integer] [reduction=float] [slide=float]
[angle_thresh=float] [degree_thresh=integer] [closeness_thresh=float] [betweeness_thresh=float]
[alpha=float] [beta=float] [iterations=integer] [cats=range] [where=sql_query] [--overwrite]
[--help] [--verbose] [--quiet] [--ui]
Flags:
-l
Disable loop support
Do not modify end points of lines forming a closed loop
-t
Do not copy attributes
--overwrite
Allow output files to overwrite existing files
--help
Print usage summary
--verbose
Verbose module output
--quiet
Quiet module output
--ui
Force launching GUI dialog
Parameters:
input=name [required]
Name of input vector map
Or data source for direct OGR access
layer=string
Layer number or name (’-1’ for all layers)
A single vector map can be connected to multiple database tables. This number determines which table
to use. When used with direct OGR access this is the layer name.
Default: -1
type=string[,string,...]
Input feature type
Options: line, boundary, area
Default: line,boundary,area
output=name [required]
Name for output vector map
error=name
Error map with failed generalizations
Lines and boundaries causing errors (collapsed to a point or topology errors)
method=string [required]
Generalization algorithm
Options: douglas, douglas_reduction, lang, reduction, reumann, boyle, sliding_averaging,
distance_weighting, chaiken, hermite, snakes, network, displacement
douglas: Douglas-Peucker Algorithm
douglas_reduction: Douglas-Peucker Algorithm with reduction parameter
lang: Lang Simplification Algorithm
reduction: Vertex Reduction Algorithm eliminates points close to each other
reumann: Reumann-Witkam Algorithm
boyle: Boyle’s Forward-Looking Algorithm
sliding_averaging: McMaster’s Sliding Averaging Algorithm
distance_weighting: McMaster’s Distance-Weighting Algorithm
chaiken: Chaiken’s Algorithm
hermite: Interpolation by Cubic Hermite Splines
snakes: Snakes method for line smoothing
network: Network generalization
displacement: Displacement of lines close to each other
threshold=float [required]
Maximal tolerance value
Options: 0-1000000000
look_ahead=integer
Look-ahead parameter
Default: 7
reduction=float
Percentage of the points in the output of ’douglas_reduction’ algorithm
Options: 0-100
Default: 50
slide=float
Slide of computed point toward the original point
Options: 0-1
Default: 0.5
angle_thresh=float
Minimum angle between two consecutive segments in Hermite method
Options: 0-180
Default: 3
degree_thresh=integer
Degree threshold in network generalization
Default: 0
closeness_thresh=float
Closeness threshold in network generalization
Options: 0-1
Default: 0
betweeness_thresh=float
Betweeness threshold in network generalization
Default: 0
alpha=float
Snakes alpha parameter
Default: 1.0
beta=float
Snakes beta parameter
Default: 1.0
iterations=integer
Number of iterations
Default: 1
cats=range
Category values
Example: 1,3,7-9,13
where=sql_query
WHERE conditions of SQL statement without ’where’ keyword
Example: income < 1000 and population >= 10000
DESCRIPTION
v.generalize is a module for the generalization of GRASS vector maps. This module consists of algorithms
for line simplification, line smoothing, network generalization and displacement (new methods may be
added later).
The cats and where options are used only if a layer > 0 is specified, otherwise, those options are
ignored. Be aware that the default is layer=-1, meaning that all layers are processed, ignoring the cats
and where options.
If type=area is selected, boundaries of selected areas will be generalized, and the options cats, where,
and layer will be used to select areas.
NOTES
(Line) simplification is a process of reducing the complexity of vector features. The module transforms a
line into another line consisting of fewer vertices, that still approximate the original line. Most of
the algorithms described below select a subset of points on the original line.
(Line) smoothing is a "reverse" process which takes as input a line and produces a smoother approximate
of the original. In some cases, this is achieved by inserting new vertices into the original line, and
can total up to 4000% of the number of vertices in the original. In such an instance, it is always a good
idea to simplify the line after smoothing.
Smoothing and simplification algorithms implemented in this module work line by line, i.e.
simplification/smoothing of one line does not affect the other lines; they are treated separately. For
isolated loops formed by a single line/boundary, he first and the last point of each line/boundary can be
translated and/or deleted, unless the -l flag is used to disable loop support.
Lines and boundaries are not translated if they would collapse to a single point. Boundaries are not
translated if they would intersect with themselves or other boundaries. Such erroneous features are
written to an optional error vector map. Overlaying the error map over the generalized map indicates the
kind of error. Lines/boundaries collapsing to a point are written out as points, boundaries violating
topology are written out as boundaries. The error map can be overlaid over the generalized map to
understand why some features were not generalized.
SIMPLIFICATION
Simplification can fail for many boundaries if the simplification parameters would result in a large
reduction of vertices. If many lines/boundaries could not be simplified, try different parameters that
would cause a lower degree of simplification.
v.generalize contains following line simplification algorithms:
• Douglas-Peucker Algorithm
• Douglas-Peucker Reduction Algorithm
• Lang Algorithm
• Vertex Reduction
• Reumann-Witkam Algorithm
• Remove Small Lines/Areas
Different algorithms require different parameters, but all the algorithms have one parameter in common:
the threshold parameter, given in map units (for latitude-longitude locations: in decimal degree). In
general, the degree of simplification increases with the increasing value of threshold.
ALGORITHM DESCRIPTIONS
• Douglas-Peucker - "Quicksort" of line simplification, the most widely used algorithm. Input
parameters: input, threshold. For more information, see:
http://geomalgorithms.com/a16-_decimate-1.html.
• Douglas-Peucker Reduction Algorithm is essentially the same algorithm as the algorithm above, the
difference being that it takes an additional reduction parameter which denotes the percentage of
the number of points on the new line with respect to the number of points on the original line.
Input parameters: input, threshold, reduction.
• Lang - Another standard algorithm. Input parameters: input, threshold, look_ahead. For an
excellent description, see:
http://www.sli.unimelb.edu.au/gisweb/LGmodule/LGLangVisualisation.htm.
• Vertex Reduction - Simplest among the algorithms. Input parameters: input, threshold. Given a
line, this algorithm removes the points of this line which are closer to each other than
threshold. More precisely, if p1 and p2 are two consecutive points, and the distance between p2
and p1 is less than threshold, it removes p2 and repeats the same process on the remaining
points.
• Reumann-Witkam - Input parameters: input, threshold. This algorithm quite reasonably preserves
the global characteristics of the lines. For more information, see for example:
http://psimpl.sourceforge.net/reumann-witkam.html.
Douglas-Peucker and Douglas-Peucker Reduction Algorithm use the same method to simplify the lines. Note
that
v.generalize input=boundary_county output=boundary_county_dp20 method=douglas threshold=20
is equivalent to
v.generalize input=boundary_county output=boundary_county_dp_red20_100 \
method=douglas_reduction threshold=20 reduction=100
However, in this case, the first method is faster. Also observe that douglas_reduction never outputs more
vertices than douglas, and that, in general, douglas is more efficient than douglas_reduction. More
importantly, the effect of
v.generalize input=boundary_county output=boundary_county_dp_red0_30 \
method=douglas_reduction threshold=0 reduction=30
is that ’out’ contains approximately only 30% of points of ’in’.
SMOOTHING
The following smoothing algorithms are implemented in v.generalize:
• Boyle’s Forward-Looking Algorithm - The position of each point depends on the position of the
previous points and the point look_ahead ahead. look_ahead consecutive points. Input parameters:
input, look_ahead.
• McMaster’s Sliding Averaging Algorithm - Input Parameters: input, slide, look_ahead. The new
position of each point is the average of the look_ahead points around. Parameter slide is used
for linear interpolation between old and new position (see below).
• McMaster’s Distance-Weighting Algorithm - Takes the weighted average of look_ahead consecutive
points where the weight is the reciprocal of the distance from the point to the currently
smoothed point. The parameter slide is used for linear interpolation between the original
position of the point and newly computed position where value 0 means the original position.
Input parameters: input, slide, look_ahead.
• Chaiken’s Algorithm - "Inscribes" a line touching the original line such that the points on this
new line are at least threshold apart. Input parameters: input, threshold. This algorithm
approximates the given line very well.
• Hermite Interpolation - This algorithm takes the points of the given line as the control points
of hermite cubic spline and approximates this spline by the points approximately threshold apart.
This method has excellent results for small values of threshold, but in this case it produces a
huge number of new points and some simplification is usually needed. Input parameters: input,
threshold, angle_thresh. Angle_thresh is used for reducing the number of the points. It denotes
the minimal angle (in degrees) between two consecutive segments of a line.
• Snakes is the method of minimisation of the "energy" of a line. This method preserves the general
characteristics of the lines but smooths the "sharp corners" of a line. Input parameters input,
alpha, beta. This algorithm works very well for small values of alpha and beta (between 0 and
5). These parameters affect the "sharpness" and the curvature of the computed line.
One of the key advantages of Hermite Interpolation is the fact that the computed line always passes
through the points of the original line, whereas the lines produced by the remaining algorithms never
pass through these points. In some sense, this algorithm outputs a line which "circumscribes" the input
line.
On the other hand, Chaiken’s Algorithm outputs a line which "inscribes" a given line. The output line
always touches/intersects the centre of the input line segment between two consecutive points. For more
iterations, the property above does not hold, but the computed lines are very similar to the Bezier
Splines. The disadvantage of the two algorithms given above is that they increase the number of points.
However, Hermite Interpolation can be used as another simplification algorithm. To achieve this, it is
necessary to set angle_thresh to higher values (15 or so).
One restriction on both McMasters’ Algorithms is that look_ahead parameter must be odd. Also note that
these algorithms have no effect if look_ahead = 1.
Note that Boyle’s, McMasters’ and Snakes algorithm are sometimes used in the signal processing to smooth
the signals. More importantly, these algorithms never change the number of points on the lines; they
only translate the points, and do not insert any new points.
Snakes Algorithm is (asymptotically) the slowest among the algorithms presented above. Also, it requires
quite a lot of memory. This means that it is not very efficient for maps with the lines consisting of
many segments.
DISPLACEMENT
The displacement is used when the lines overlap and/or are close to each other at the current level of
detail. In general, displacement methods move the conflicting features apart so that they do not interact
and can be distinguished.
This module implements an algorithm for displacement of linear features based on the Snakes approach.
This method generally yields very good results; however, it requires a lot of memory and is not very
efficient.
Displacement is selected by method=displacement. It uses the following parameters:
• threshold - specifies critical distance. Two features interact if they are closer than threshold
apart.
• alpha, beta - These parameters define the rigidity of lines. For larger values of alpha, beta
(>=1), the algorithm does a better job at retaining the original shape of the lines, possibly at
the expense of displacement distance. If the values of alpha, beta are too small (<=0.001), then
the lines are moved sufficiently, but the geometry and topology of lines can be destroyed. Most
likely the best way to find the good values of alpha, beta is by trial and error.
• iterations - denotes the number of iterations the interactions between the lines are resolved.
Good starting points for values of iterations are between 10 and 100.
The lines affected by the algorithm can be specified by the layer, cats and where parameters.
NETWORK GENERALIZATION
Used for selecting "the most important" part of the network. This is based on the graph algorithms.
Network generalization is applied if method=network. The algorithm calculates three centrality measures
for each line in the network and only the lines with the values greater than thresholds are selected.
The behaviour of algorithm can be altered by the following parameters:
• degree_thresh - algorithm selects only the lines which share a point with at least degree_thresh
different lines.
• closeness_thresh - is always in the range (0, 1]. Only the lines with the closeness centrality
value at least closeness_thresh apart are selected. The lines in the centre of a network have
greater values of this measure than the lines near the border of a network. This means that this
parameter can be used for selecting the centre(s) of a network. Note that if closeness_thresh=0
then everything is selected.
• betweeness_thresh - Again, only the lines with a betweeness centrality measure at least
betweeness_thresh are selected. This value is always positive and is larger for large networks.
It denotes to what extent a line is in between the other lines in the network. This value is
large for the lines which lie between other lines and lie on the paths between two parts of a
network. In the terminology of road networks, these are highways, bypasses, main roads/streets,
etc.
All three parameters above can be presented at the same time. In that case, the algorithm selects only
the lines which meet each criterion.
Also, the outputed network may not be connected if the value of betweeness_thresh is too large.
EXAMPLES
SIMPLIFICATION EXAMPLE
Simplification of county boundaries with DP method (North Carolina sample dataset), threshold given in
mapset units (here: meters):
v.generalize input=boundary_county output=boundary_county_dp20 \
method=douglas threshold=20 error=boundary_county_dp20_leftover
Figure: Vector simplification example (spatial subset: original map shown in black, simplified map with
26% remaining vertices shown in red)
SMOOTHING EXAMPLE
Smoothing of road network with Chaiken method (North Carolina sample dataset), threshold given in mapset
units (here: meters):
v.generalize input=roads output=roads_chaiken method=chaiken \
threshold=1 error=roads_chaiken_leftover
Figure: Vector smoothing example (spatial subset: original map shown in black, smoothed map with 500%
increased number of vertices shown in red)
SEE ALSO
v.clean, v.dissolve
v.generalize Tutorial (GRASS-Wiki)
AUTHORS
Daniel Bundala, Google Summer of Code 2007, Student
Wolf Bergenheim, Mentor
Partial rewrite: Markus Metz
SOURCE CODE
Available at: v.generalize source code (history)
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