Content
Introduction to Raster GIS
The basic concept of raster GIS data model
Raster database
Characteristics of raster
Raster resolution
Map Algebra Methods
Local functions
Focal functions
Neighbourhood functions
Zonal functions
School of Computing and Information Systems,
Singapore Management University
2022-08-12
Introduction to Raster GIS
The basic concept of raster GIS data model
Raster database
Characteristics of raster
Raster resolution
Map Algebra Methods
Local functions
Focal functions
Neighbourhood functions
Zonal functions
All raster formats are basically the same
Content is more important than format: data or picture?
Map algebra is a simple and an elegant set based algebra for manipulating geographic data, proposed by Dr. Dana Tomlin in the early 1980s.
It is a set of primitive operations in a GIS which allows one or more raster layers (“maps”) of similar dimensions to produce a new raster layer (map) using algebraic operations such as addition, subtraction etc.
Local function – characterising individual locations
Neighbourhood function – characterising locations within neighbourhood
Zonal function – characterising location within a zone
Local functions use only the data in a single cell to calculate an output value.
Potential operators fall into five categories:
trigonometric (i.e. sine, cosine, tangent, arcsine)
transformation (i.e. sqrt, exp, log)
relational operations (>, <, =)
statistical (i.e. mean, median, mode)
arithmetic (i.e. absolute value of x)
These are also called focal functions.
Local neighbourhood functions examine the target cell and immediate neighbours.
A value is returned based on their combined evaluation.
Neighbourhood scan be defined by rectangles, circles, wedges, doughnut shapes (annulus) etc.
A doughnut shape can be drawn around a focal cell, and the values of the surrounding shape (referred to an annulus neighbourhood) are used to reclassify the focal cell.
A zonal operation is employed on groups of cells of similar value or like features, not surprisingly called zones.
These zones could be conceptualized as raster versions of polygons. Zonal rasters are often created by reclassifying an input raster into just a few categories.
Zonal operations may be applied to a single raster or two overlaying rasters.
Given a single input raster, zonal operations measure the geometry of each zone in the raster, such as area, perimeter, thickness, and centroid.
Global operations are similar to zonal operations whereby the entire raster dataset’s extent represents a single zone.
Typical global operations include determining basic statistical values for the raster as a whole.
For example, the minimum, maximum, average, range, and so forth can be quickly calculated over the entire extent of the input raster and subsequently be output to a raster in which every cell contains that calculated value.
The Euclidean distance functions describe each cell’s relationship to a source or a set of sources.
The Euclidean distance output raster contains the measured distance from every cell to the nearest source.
Simple proximity is generated by summing a series of orthogonal and diagonal steps emanating from a starting location.
Terrain models
Slope and Aspect
Hillshading
Terrain Profile
Visibility Analysis
Mathematics of slope
Aspect is the direction that a slope faces. It identifies the steepest downslope direction at a location on a surface.
Usage of aspect:
Find all west-facing slopes on a mountain as part of a search for the best slopes for building resort residential units.
Calculate the solar illumination for each location in a region as part of a study to determine the diversity of life at each.
Casts shadows with an imaginary light source.
Azimuth is the compass direction of the light source.
Altitude is the angle of the light source above the horizon.
A line of sight is a line between two points that shows the parts the surface along the line that are visible to or hidden from an observer.
Viewsheds are regions of visibility observable from one or more observation points.