A coordinate reference system (CRS) provides a framework for defining real-world locations. Represent latitude-longitude data using a geographic CRS or x-y map data using a projected CRS.
Transform coordinates between systems using various projection methods. Though all projection methods cause distortion, you can preserve attributes such as area, shape, or direction by choosing an appropriate projection method.
|Geographic coordinate reference system object|
|Projected coordinate reference system object|
|Well-known text string|
|Initialize or reset map projection structure|
|Convert GeoTIFF information to map projection structure|
|Map projection support for map axes and map projection structures|
|List map projections for map axes and map projection structures|
|GeoTIFF info structure support for |
|Select ellipsoids for given UTM zone|
|Select UTM zone given latitude and longitude|
|Choose or identify UTM zone by clicking map|
Learn about the map projections supported by the toolbox, and their families and properties.
Most map projections can be categorized into three families based on the cylinder, cone, and plane geometric shapes.
Map projections are influenced and constrained by five characteristic properties: shape, distance, direction, scale, and area.
Variable projection parameters control the appearance of map projections. Projection parameters include aspect, origin, and scale.
Transform coordinates from a projected CRS to a different projected CRS that uses the same geographic CRS.
Project or unproject raster data by referencing the coordinates to a grid, then display the data.
Create a map for a zone in the Universal Transverse Mercator (UTM) system.
You can interact with a map of the world to select a UTM zone and adjust map settings, such as the limits, origin, parallels, and aspect.
This example shows how to select a UTM zone by specifying the coordinate of a location. You can then create a UTM coordinate system using the suggested ellipsoid vector of the zone.
This example shows how to display areas that extend across more than one UTM zone by using the Mercator projection in a transverse aspect.
A map projection transforms a curved surface such as the Earth onto a two-dimensional plane. All map projections introduce distortions compared to maps on globes.
A standard method of visualizing map projection distortion is to project small circles spaced at regular intervals across the globe.
This example shows how to visualize map projection distortions using contour lines of constant map distortion.
You can calculate quantitative position-specific map error statistics, such as area scale, angular deformation of right angles, and directional scale distortions along meridians and parallels.
A projection aspect is the orientation of a map on the page or display screen. An orientation vector controls the map projection aspect.
You can redefine a coordinate system and transform all points to the new coordinate system. The transformation can be useful independent of map displays.