THE UNIVERSAL GRID SYSTEM



Similar documents
Earth Coordinates & Grid Coordinate Systems

UTM: Universal Transverse Mercator Coordinate System

EPSG. Coordinate Reference System Definition - Recommended Practice. Guidance Note Number 5

NGA GRID GUIDE HOW TO USE ArcGIS 8.x ANS 9.x TO GENERATE MGRS AND OTHER MAP GRIDS

Geomatics Guidance Note 3

An Introduction to Coordinate Systems in South Africa

The Map Grid of Australia 1994 A Simplified Computational Manual

量 說 Explanatory Notes on Geodetic Datums in Hong Kong

Measuring the Earth Using a GPS M. Scott Wilkerson & M. Beth Wilkerson, DePauw University, May 10, 2007

WHAT YOU NEED TO USE THE STATE PLANE COORDINATE SYSTEMS

Lecture 2. Map Projections and GIS Coordinate Systems. Tomislav Sapic GIS Technologist Faculty of Natural Resources Management Lakehead University

Coordinate Systems. Orbits and Rotation

Keywords: coordinate systems, latitude, longitude, georeferencing, global positioning system, GPS, geodetic datum, ellipsoid, geocoding, postal code

Lines on Maps and Globes. Cross Curricular Writing Activity Social Studies Grade 4

WGS AGD GDA: Selecting the correct datum, coordinate system and projection for north Australian applications

UTM Zones for the US UTM UTM. Uniform strips Scalable coordinates

4 The Rhumb Line and the Great Circle in Navigation

Finding location and velocity data for PBO GPS stations

The Chief Directorate: National

The Globe Latitudes and Longitudes

3D Visualization of Seismic Activity Associated with the Nazca and South American Plate Subduction Zone (Along Southwestern Chile) Using RockWorks

What are map projections?

Using Geocoded TIFF & JPEG Files in ER Mapper 6.3 with SP1. Eric Augenstein Earthstar Geographics Web:

Maintaining High Accuracy in Modern Geospatial Data

Navigation: Latitude and Longitude

Learning about GPS and GIS

CHAPTER 9 SURVEYING TERMS AND ABBREVIATIONS

Latitude, Longitude, and Time Zones

Lines of Latitude and Longitude

Basic Graphing Functions for the TI-83 and TI-84

2 GIS concepts. 2.1 General GIS principles

Celestial Observations

Chapter 19 Magnetic Forces and Fields

Sun Earth Relationships

MGL Avionics. MapMaker 2. User guide

Coordinate Conversions and Transformations including Formulas

MSLC Workshop Series Math Workshop: Polynomial & Rational Functions

3D MAGNETIC INVERSION OF A VTEM SURVEY. (Nicol Block) Submitted to: NORTHSTAR GOLD CORP. PRESENTED BY

TerraColor White Paper

Introduction to GIS (Basics, Data, Analysis) & Case Studies. 13 th May Content. What is GIS?

Getting Land Survey Vertical & Horizontal Control via the Internet

Lecture 8 : Coordinate Geometry. The coordinate plane The points on a line can be referenced if we choose an origin and a unit of 20

Exploring plate motion and deformation in California with GPS

WILD 3710 Lab 3: GIS Data Exploration Camp W.G. Williams

Topographic Maps Practice Questions and Answers Revised October 2007

Example 1. Rise 4. Run Our Solution

Newton s Law of Gravity

Gravitational potential

Metadata for Big River Watershed Geologic and Geomorphic Data

Programmer s Guide for MSP Geographic Translator (GEOTRANS) Version 3.4

6. The greatest atmospheric pressure occurs in the 1) troposphere 3) mesosphere 2) stratosphere 4) thermosphere

Release Notes / Version Description Document for MSP Geographic Translator (GEOTRANS) Version 3.4

11.1. Objectives. Component Form of a Vector. Component Form of a Vector. Component Form of a Vector. Vectors and the Geometry of Space

Reprojecting MODIS Images

1.2 GRAPHS OF EQUATIONS. Copyright Cengage Learning. All rights reserved.

2.5 Transformations of Functions

Trimble R8 Base and Rover Quick Setup Guide. Inland GPS Inc.

GIS IN ECOLOGY: SPATIAL REFERENCING

CHAPTER 4 LEGAL DESCRIPTION OF LAND DESCRIBING LAND METHODS OF DESCRIBING REAL ESTATE

Calculation of Azimuth, Elevation and Polarization for non-horizontal aligned Antennas

Thought Questions on the Geostrophic Wind and Real Winds Aloft at Midlatitudes

Linear Equations. Find the domain and the range of the following set. {(4,5), (7,8), (-1,3), (3,3), (2,-3)}

SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES

PLOTTING SURVEYING DATA IN GOOGLE EARTH

Solar Angles and Latitude

Motion & The Global Positioning System (GPS)

MODERN APPLICATIONS OF PYTHAGORAS S THEOREM

Section 1.5 Linear Models

Follow That Hurricane!

Algebra 2 Chapter 1 Vocabulary. identity - A statement that equates two equivalent expressions.

GPS accuracy: Hand-held versus RTK

The ecliptic - Earth s orbital plane

Inside Earth Chapter 3

GCalc 2.1. GDA94 Datum Transformation DLL Technical Specification

Beacon to Beacon Northern & Southern Maps


Math 215 Project (25 pts) : Using Linear Algebra to solve GPS problem

ELEMENTS OF SURVEYING FOR CADASTRAL MAPPING

OBJECTIVES. Identify the means by which latitude and longitude were created and the science upon which they are based.

Surveying on NAD83 State Plane Coordinate System

Digital Terrain Model Grid Width 10 m DGM10

GPS LOCATIONS FOR GIS: GETTING THEM RIGHT THE FIRST TIME

Basic Map & GPS Skills. How to read a topographic map, use a compass, and determine GPS locations on a map

Astromechanics. 1 solar day = sidereal days

SESSION 8: GEOGRAPHIC INFORMATION SYSTEMS AND MAP PROJECTIONS

A.2. Exponents and Radicals. Integer Exponents. What you should learn. Exponential Notation. Why you should learn it. Properties of Exponents

Graphing Linear Equations in Two Variables

Running on Renewables (Lesson Plan) (Utilizing HOMER: Modeling Software for Hybrid Electric Power Systems)

Utah State General Records Retention Schedule SCHEDULE 1 GEOSPATIAL DATA SETS

Creating Figure Ground Maps in ArcMap 10.x: Basic procedures to download, open, manipulate and print spatial data

MAPPING THE ST. FRANCIS DAM OUTBURST FLOOD WITH GEOGRAPHIC INFORMATION SYSTEMS

Graphing Quadratic Functions

Plot the following two points on a graph and draw the line that passes through those two points. Find the rise, run and slope of that line.

The Earth Really is Flat! The Globe and Coordinate Systems. Long History of Mapping. The Earth is Flat. Long History of Mapping

Noon Sun Angle = 90 Zenith Angle

An Analysis of the Rossby Wave Theory

Vocabulary Words and Definitions for Algebra

Transcription:

NGA Office of GEOINT Sciences Coordinate Systems Analysis (CSAT) Phone: 314-676-9124 Unclassified Email: coordsys@nga.mil March 2007 THE UNIVERSAL GRID SYSTEM Universal Transverse Mercator (UTM) Military Grid Reference System (MGRS) Universal Polar Stereographic (UPS) United States National Grid (USNG) A simplified definition and explanation of UTM and related systems THE UTM SYSTEM UTM coordinates are based on a family of 120 Transverse Mercator map projections (two for each UTM zone, with one for each N/S hemisphere). The earth is divided into 60 zones, each 6 wide in longitude (with the exception of a few non-standard-width zones for Svalbard and southwest Norway). See Figure 1. Figure 1.

Numbering of zones begins at 180 and proceeds eastward. o Zone 1 is from 180 W to 174 W, o Zone 2 is from 174 W to 168 W, and so on. Each zone has a central meridian. o Zone 1 central meridian is 177 W, o Zone 2 central meridian is 171 W, and so on. The X value, called the Easting, has a value of 500,000m at the central meridian of each zone (Figure 2). The Y value, called the Northing, has a value of 0m at the equator for the northern hemisphere (Figure 3), 10,000,000m at the equator for the southern hemisphere. Figure 2. Easting values. Figure 3. Northing values. UTM is limited to the area between 84 N and 80 S. Beyond that, Universal Polar Stereographic (UPS) coordinates are used. See section on UPS.

REFERENCING / EXPRESSING A POSITION IN UTM COORDINATES In the UTM system, positions are expressed as Easting / Northing, e.g. 580817mE, 4251205mN. In some cases, the letters are left off, e.g. 580817 4251205. If positions occur near UTM zone junctions, the UTM zone may also be specified, e.g. 580817mE, 4251205mN, Zone 15. Since the above expresses two possible positions on the earth, the hemisphere may also be specified, e.g. 580817mE, 4251205mN, Zone 15, Northern Hemisphere (Figure 4). Figure 4. Example of position expressed in both Lat/Long and UTM coordinates. Many systems abbreviate the above, representing the hemisphere as a single letter, N for northern hemisphere, and S for southern hemisphere, e.g. 15N 580817 4251205. CAUTION: IN MANY SYSTEMS, THE LETTER AFTER THE ZONE NUMBER DESIGNATES A LATITUDINAL BAND, NOT A HEMISPHERE. MORE ON THIS BELOW.

MGRS The Military Grid Reference System (MGRS) is an alpha-numeric system for expressing UTM / UPS coordinates. A single alpha-numeric value references a position that is unique for the entire earth. The components of MGRS values are as follows: (Example: 15SWC8081751205) The first two characters represent the 6 wide UTM zone. o Leading zeroes are included so that Zone 9 is 09. o For polar areas outside the UTM area, these characters are omitted. The third character is a letter designating a band of latitude. o Beginning at 80 S and preceding northward, the 20 bands are lettered C through X, omitting I and O. o The bands are all 8 high except band X, which is 12 high. o Outside the UTM area, A and B are used near the South Pole, Y and Z near the North Pole. The vertical UTM boundaries and horizontal latitudinal band boundaries form (generally) 6 X 8 Grid Zones. Hence, the first

three letters of the MGRS value, e.g. 15S, are referred to as the Grid Zone Designator (GZD). The fourth and fifth characters are a pair of letters identifying one of the 100,000-meter grid squares within the grid zone (or UPS area). See Figure 6. Figure 6. In this sample area, the Grid Zone Designators are shown in brown. The smaller gray letters are the100,000-meter grid square identifiers. The example point 15SWC8081751205 is located in square WC near the center of the figure. The remaining characters consist of the numeric Easting and Northing values within the 100,000-meter grid square (Figure 7). MGRS coordinates may be rounded to reflect lesser refinement. For example: 15SWC8081751205 is at one-meter refinement. 15SWC80825121 is at 10-meter refinement. 15SWC808512 is at 100-meter refinement. 15SWC8151 is at 1000-meter refinement.

There are two lettering schemes for the 100,000-meter grid square identifiers. Generally, one scheme is used for WGS-84, and the other is used for older ellipsoids associated with local datum s. Example: 15SWC8081751205 is on WGS-84. When converted to NAD-27 datum, Clarke 1866 ellipsoid, its value is: 15SWN8083350993 The 100,000-meter grid square WC for WGS-84 generally coincides with the grid square WN for Clarke 1866. See the section on USNG for further guidance. Figure 7. Magenta arrows show how MGRS easting and northing values are determined from within the 100,000-meter grid square. The MGRS value of this position is 15SWC8081751205.

THE LETTER AFTER THE UTM ZONE NUMBER: IS THAT A HEMISPHERE OR A LATITUDINAL BAND? Since the creation of UTM, developers have interpreted the rules for expressing an earth-wide unique UTM position in one of two ways: 1. By including an N or S after the zone number to specify a hemisphere. 2. By including the 8 latitudinal band designator (see the section on MGRS) after the zone number. Example: The position at 92 W, 38 N, expressed in UTM coordinates, is: 587798m E, 4206287m N, Zone 15. This reference is valid for two positions on the earth. In order to make it unique for only one position worldwide, i.e. 92 W, 38 N: Developer #1 includes an N to specify northern hemisphere: 15N 587798 4206287 Developer #2 includes the 8 latitudinal band designator: 15S 587798 4206287 This situation is causing confusion among users and developers. The two 8 latitudinal bands, from 0 to 8 N and from 32 N to 40 N, are assigned the designations N and S, respectively. These designations are often mistaken for hemisphere designations. Technical Manual 8358.1 contains the authoritative definition of UTM. NGA will soon publish an updated version of TM 8358.1, which will provide clarification on this issue.

THE UNIVERSAL POLAR STEREOGRAPHIC (UPS) SYSTEM UPS coordinates are based on a family of two Polar Stereographic map projections, one for each pole. The origin of the UPS coordinate system is the pole (north or south), where X=2,000,000m and Y=2,000,000m. The X-axis lies along the meridians 90 E and 90 W. o Moving from the pole (north or south), X-values (Easting s) increase along the 90 E meridian. The Y-axis lies along the meridians 0 and 180. o Moving from the North Pole, Y-values (Northing s) increase along the 180 meridian. o Moving from the South Pole, Y-values (Northing s) increase along the 0 meridian. THE UNITED STATES NATIONAL GRID (USNG) USNG is functionally equivalent to MGRS. The main difference between the two systems is in the method for specifying the datum. In MGRS, an alternate lettering scheme is used for the 100,000-meter grid square designator when the position is referenced to an older datum (see section on MGRS). The USNG does not use the alternate lettering scheme, but simply specifies the datum after the position reference. For example, a position on the NAD 27 datum is reported in the two systems as follows: MGRS: 15SWN8083350993 USNG: 15SWC8083350993 (NAD 27)