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- GPS coordinates are usually expressed as the combination of latitude and longitude. They are points of intersection in a grid system that pinpoint a specific location on Earth. Latitude refers to the distance north or south of the equator, which is measured in degrees.
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Mar 11, 2024 · GPS coordinates are usually expressed as the combination of latitude and longitude. They are points of intersection in a grid system that pinpoint a specific location on Earth. Latitude refers to the distance north or south of the equator, which is measured in degrees.
Oct 13, 2023 · Compared to longitude and latitude, GPS delivers more precision and accurate positioning information, while longitude and latitude serve as the foundation for understanding Earth's surface, establishing a reference point for navigation and exploration. Longitude and latitude are indispensable tools for pinpointing locations on Earth's surface.
- Overview
- A framework for describing locations
- Technical considerations
Latitude is a measurement on a globe or map of location north or south of the Equator. Technically, there are different kinds of latitude, which are geocentric, astronomical, and geographic (or geodetic), but there are only minor differences between them.
What is the length of a degree of latitude?
The length of a degree of arc of latitude is approximately 111 km (69 miles), varying, because of the nonuniformity of Earth’s curvature, from 110.567 km (68.706 miles) at the Equator to 111.699 km (69.41 miles) at the poles.
What is longitude?
Longitude is a measurement of location east or west of the prime meridian at Greenwich, London, England, the specially designated imaginary north-south line that passes through both geographic poles and Greenwich. Longitude is measured 180° both east and west of the prime meridian.
What is the distance per degree of longitude?
Lines of latitude (also called parallels) are imaginary lines that circle Earth’s surface, running east and west parallel to the Equator. Lines of longitude (also called meridians) run between the geographic North Pole and the geographic South Pole and are used to measure distances from the prime meridian. Both latitude and longitude are measured in degrees (°), which may be broken down into smaller units called minutes (′) and seconds (″). (Or they may be expressed in decimal degrees; negative values of decimal degrees represent latitudes in the Southern Hemisphere and longitudes in the Western Hemisphere.) The latitudes of the North Pole and South Pole are 90° north (N) and 90° south (S), respectively. Lines of latitude north of the Equator (the line that marks 0° latitude) are numbered from 1° to 89° N, and those south of the Equator are numbered from 1° to 89° S. Lines of longitude east of the prime meridian (the line that marks 0° longitude) are numbered from 1° to 179° east (E). Lines of longitude west of the prime meridian are numbered from 1° to 179° west (W). The 180th meridian, or 180°—which can be drawn north-south from pole to pole across the middle of the Pacific Ocean—is the line of longitude exactly opposite the prime meridian.
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The combination of meridians of longitude and parallels of latitude establishes a framework or grid that can be used to locate exact positions on a map or globe. For example, a point made up of the coordinates 40° N 30° W is located at latitude 40° north of the Equator and longitude 30° west of the Greenwich meridian (which is expressed in decimal degrees as latitude 40 and longitude –30). The location of Washington, D.C., which lies 39 degrees north of the Equator and 77 degrees west of the prime meridian, can be described using the coordinates 39° N 77° W. (In decimal degree formatting, the approximate location of Washington, D.C., is latitude 39 and longitude –77.)
Technically speaking, there are different kinds of latitude—geocentric, astronomical, and geographic (or geodetic)—but there are only minor differences between them. In most common references, geocentric latitude is implied. Given in degrees, minutes, and seconds, geocentric latitude is the arc (a curved line) that can be drawn along Earth’s surface, created by an imaginary plane that passes through Earth’s center, whose angle diverges from that of the equatorial plane (that is, the imaginary plane that cuts through Earth and includes all points along the Equator). Thus, a point at 30°15′20″ N is the arc that results from an angle of 30°15′20″ at the center of the globe. Astronomical latitude is the angle created by the equatorial plane and a line created by the direction of gravity (that is, the plumb line) occurring at a given point on Earth’s surface.
Geographic latitude, which is the kind used in mapping, is calculated using a slightly different process. Because Earth is not a perfect sphere—the planet’s curvature is flatter at the poles—geographic latitude is the arc resulting from an angle created by the equatorial plane and the normal line that can be drawn from a given point on Earth’s surface to Earth’s center. (The normal line is perpendicular to a tangent line touching Earth’s curvature at that point on the surface.) Different methods are used to determine geographic latitude, as by taking angle-sights on certain polar stars or by measuring with a sextant the angle of the noon Sun above the horizon. The length of a degree of arc of latitude is approximately 111 km (69 miles), varying, because of the nonuniformity of Earth’s curvature, from 110.567 km (68.703 miles) at the Equator to 111.699 km (69.41 miles) at the poles. Geographic latitude is also given in degrees, minutes, and seconds.
In contrast, longitude is the amount of arc created by drawing first a line from Earth’s center to the intersection of the Equator and the prime meridian and then another line drawn from Earth’s center to any point elsewhere along the Equator. Since lines of longitude are not parallel to one another, the distance between one degree of longitude and the next will vary significantly depending upon how close to the poles the measurement is taken. The distance per degree of longitude at the Equator is about 111.32 km (69.17 miles) and at the poles, 0.
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Mar 10, 2024 · Thanks to our geographic coordinate system, you can pinpoint any point on Earth such as GPS receivers. This includes the spot where you are reading this article right now. Latitude lines run east-west, are parallel and go from -90 to +90. Longitude lines run north-south, converge at the poles and are from -180 to +180.
Jan 21, 2020 · The latitude lines are the rungs and the longitude lines are the "long" lines that hold those rungs together. Latitude lines run east and west. Just like rungs on a ladder, they remain parallel as they run across the earth's surface. In this way, you can easily remember that latitude is just like "ladder"-tude.
- Matt Rosenberg
The World Geodetic System (WGS) is a standard used in cartography, geodesy, and satellite navigation including GPS. The current version, WGS 84 , defines an Earth-centered, Earth-fixed coordinate system and a geodetic datum , and also describes the associated Earth Gravitational Model (EGM) and World Magnetic Model (WMM).
The GPS coordinates contain only 2 pieces of information: latitude and longitude on the terrestrial globe. Altitude (or elevation, or z value) is the height of the point on Earth, relative to the sea level which is counted as the base altitude (0 meters). How to calculate the elevation of a GPS point?
