Universal Transverse Mercator coordinate system
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The Universal Transverse Mercator (UTM) coordinate system is a grid-based method of specifying locations on the surface of the Earth. It is used to identify locations on the earth, but differs from the traditional method of latitude and longitude in several respects.
The UTM system is not a map projection. The system employs a series of sixty zones, each of which is based on a specifically defined Transverse Mercator projection.
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[edit] History
The Universal Transverse Mercator coordinate system was developed by the United States Army in 1947. The system was based on an ellipsoidal model of the Earth. For areas within the conterminous United States, the Clarke 1866 ellipsoid was used. For the remaining areas of the Earth, including Hawaii, the International Ellipsoid was used. Currently, the WGS84 ellipsoid is used as the underlying model of the Earth in the UTM coordinate system.
Prior to the development of the Universal Transverse Mercator coordinate system, several European nations demonstrated the utility of grid-based conformal maps by mapping their territory during the interwar period. Calculating the distance between two points on these maps could be performed more easily in the field (using the Pythagorean theorem) than was otherwise possible using the trigonometric formulas required under the graticule-based system of latitude and longitude. In the post-war years, these concepts were extended into the Universal Transverse Mercator / Universal Polar Stereographic (UTM/UPS) coordinate system, which is a global (or Universal) system of grid-based maps.
[edit] Definitions
[edit] UTM longitude zone
The UTM system divides the surface of the Earth between 80° S latitude and 84° N latitude into 60 zones, each 6° of longitude in width and centered over a meridian of longitude. Zones are numbered from 1 to 60. Zone 1 is bounded by longitude 180° to 174° W and is centered on the 177th West meridian. Zone numbering increases in an easterly direction.
Each of the 60 longitude zones in the UTM system is based on a Transverse Mercator projection, which is capable of mapping a region of large north-south extent with a low amount of distortion. By using narrow zones of 6° in width, and reducing the scale factor along the central meridian to 0.9996, (a reduction of 1:2500) the amount of distortion is held below 1 part in 1,000 inside each zone. Distortion of scale increases to 1.0010 at the outer zone boundaries along the equator.
The reduction in the scale factor along the central meridian creates two lines of true scale located approximately 180 km on either side of, and approximately parallel to, the central meridian. The scale factor is too small inside these lines and too large outside of these lines, but the overall distortion scale inside the entire zone is minimized.
[edit] UTM latitude zone
The UTM system segments each longitude zone into 20 latitude zones. Each latitude zone is 8 degrees high, and is lettered starting from "C" at 80° S, increasing up the English alphabet until "X", omitting the letters "I" and "O" (because of their similarity to the digits one and zero). The last latitude zone, "X", is extended an extra 4 degrees, so it ends at 84° N latitude, thus covering the northern most land on Earth. Latitude zones "A" and "B" do exist, as do zones "Y" and Z". They cover the western and eastern sides of the antarctic and arctic regions respectively. A convenient trick to remember is that the letter "N" is the first letter in the northern hemisphere, so any letter coming before "N" in the alphabet is in the southern hemisphere, and any letter "N" or after is in the northern hemisphere.
[edit] Notation
Each grid square is referred to by the longitude zone number and the latitude zone character. The longitude zone is always written first, followed by the latitude zone. For example (see image, top right), a position in Toronto, Canada, would find itself in longitude zone 17 and latitude zone "T", thus the full reference is "17T".
[edit] Exceptions
These longitude and latitude zones are uniform over the globe, except in two areas. On the southwest coast of Norway, the UTM zone 32V is extended further west, and the zone 31V is correspondingly shrunk to cover only open water. Also, in the region around Svalbard, the longitude zones are given double their normal width.
 Europe |
 Africa |
 South America |
 Bering Sea with Alaska |
Picture gallery: UTM zones in various parts of the world
[edit] Locating a position using UTM coordinates
A position on the Earth is referenced in the UTM system by the UTM longitude zone, the projected distance of the position from the central meridian -- called the easting -- and the projected distance of the point from the equator -- called the northing. The point of origin of each UTM zone is the intersection of the equator and the zone's central meridian. In order to avoid dealing with negative numbers, the central meridian of each zone is given a "false easting" value of 500,000 meters. Thus, anything west of the central meridian will have an easting less than 500,000 meters. For example, UTM eastings range from 167,000 meters to 833,000 meters at the equator (these ranges narrow towards the poles). In the northern hemisphere, positions are measured northward from the equator, which has an initial "northing" value of 0 meters and a maximum "northing" value of approximately 9,328,000 meters at the 84th parallel -- the maximum northern extent of the UTM zones. In the southern hemisphere, northings decrease as you go southward from the equator, which is given a "false northing" of 10,000,000 meters so that no point within the zone has a negative northing value.
As an example, the CN Tower is located at the geographic position . This is in longitude zone 17, and the grid position is 630084m east, 4833438m north.
The latitude zone is unnecessary if the full distance from the equator is given (as above) and the hemisphere is known. It does, however, become important when further sub-division of the UTM grid is undertaken, such as in the military grid reference system.
[edit] Overlapping Grids
Distortion of scale increases in each UTM zone as the boundaries between the longitude zones are approached. However, it is often convenient or necessary to measure a series of locations on a single grid when some are located in two adjacent zones. Around the boundaries of large scale maps (1:100,000 or larger) coordinates for both adjoining UTM zones are usually printed within a minimum distance of 40 km on either side of a zone boundary. Ideally, the coordinates of each position should be measured on the grid for the zone in which they are located, but because the scale factor is still relatively small near zone boundaries, it is possible to overlap measurements into an adjoining zone for some distance when necessary.
[edit] See also
Military grid reference system
MTM (Modified Transverse Mercator)
[edit] External links
- U.S. Geological Survey UTM Grid Fact Sheet
- National Geodetic Survey (U.S.) UTM Utilities
- [1] TM8358.1: Datums, Ellipsoids, Grids and Grid Referece Systems
- [2] TM8358.2: Defense Mapping Agency Technical Manual 8358.2 The Universal Grids: Universal Transverse Mercator (UTM) and Universal Polar Stereographic (UPS)
- Converting Latitude/Longitude to Universal Transverse Mercator (UTM)
- UTM Zones
- UTM conversion library written in Perl
- UTM conversion library written in Python
- GIS MGRS Grid Data layers and UTM zones in GIS Format
- Converting UTM to Latitude and Longitude (Or Vice Versa)
- GEOTRANS Geographic Translator software and source code from the US National Geospatial-Intelligence Agency
- Geographic/UTM Coordinate Converter
[edit] References
Snyder, John P. (1987). Map Projections - A Working Manual. U.S. Geological Survey Professional Paper 1395. United States Government Printing Office, Washington, D.C..
