There are three major components of the Navstar Global Positioning System ( GPS ) :-
The Space Segment is a constellation of 27 Earth-orbiting satellites ( 24 in operation and three spare ). The U.S. military developed and implemented this satellite network as a navigation system, but soon opened it up to commercial use. It provides both commercial and recreational users 24 hour, worldwide navigation coverage with a possible accuracy to 15 metres. Each of these 1360 to 1820 kg. solar-powered satellites circles the globe at about 19,300 km., every 12 hours, and each has a service life of approx. ten years. The orbits are arranged so that at any time, anywhere on Earth, there are at least four satellites "visible".
![]() Artist's concept of the GPS satellite constellation |
The Control Segment. Controls the satellites by providing them with continuous corrected orbital and clock data. There are five stations around the world, four unmanned and one master control station. The unmanned stations constantly receive data from the satellites, and send that to the master control for correction and retransmission.
The User Segment. Is the GPS receiver in its various forms. A GPS receiver's job is to locate four or more of these satellites, calculate the distance to each, and use this information to deduce its own location.
This operation is based on a mathematical principle called
trilateration. Visualising trilateration in three-dimensional space can be difficult, and it is convenient to initially demonstrate the simpler two-dimensional trilateration.
2-D Trilateration This is a nice, hard fact, but it is not particularly useful by itself. You
could be anywhere on a circle around Mt. Isa that has a radius of 625 km,
like this:
Imagine you are
somewhere in Queensland and you are totally lost -- for whatever reason, you
have absolutely no clue where you are. You find a friendly local and ask, "Where
am I?" He says, "You are 625 km from Mt. Isa."
You ask somebody else where you are, and she says, "You are 690 km from Emerald." Now you're getting somewhere. If you combine this information with the Mt. Isa information, you have two circles that intersect. You now know that you must be at one of these two intersection points, if you are 625 km from Mt. Isa and 690 km from Emerald.
If a third person tells you that you are 615 km from Dirranbandi, you can
eliminate one of the possibilities, because the third circle will only intersect
with one of these points. You now know exactly where you are -- near Windorah, Qld. ( if you have a map.)
This same concept works in three-dimensional space, as well, but we are
dealing with spheres instead of circles.
3-D Trilateration.
Imagine each satellite to be the centre of an imaginary sphere. If we know our exact distance from a satellite in space, we know we are somewhere on the surface of an imaginary sphere with a radius equal to the distance to the satellite. If we know our exact distance from a second satellite, the same fact will apply.The intersecting plane of the spheres forms a perfect circle, and the observer will be at some point on the circumference of that circle. If we take a third and a fourth measurement from two more satellites, similar circular intercepts will give a precise point of observation on the Earth surface. Receivers generally look to four or more satellites, to
improve accuracy and provide precise altitude information.
In order to make this calculation, the GPS receiver has to know two things:
The GPS receiver figures both of these things out by analyzing high-frequency, low-power radio signals from the GPS satellites. They transmit on several low power ( 20 - 25 watts ) radio frequencies in the UHF range. The civilain frequency is designated L1, 1575.42 mhz. Better units have multiple receivers, so they can pick up signals from several satellites simultaneously.
Radio waves are electromagnetic energy, which means they travel at the speed of light ( about 300,000 km per second in a vacuum). The receiver can
figure out how far the signal has traveled by timing how long it took the signal
to arrive.
Measuring Distance.
We have seen that a GPS receiver
calculates the distance to GPS satellites by timing a signal's journey from
satellite to receiver. As it turns out, this is a fairly elaborate process.
At a particular time (let's say midnight), the satellite begins transmitting a long, digital pattern called a pseudo-random code. The receiver begins running the same digital pattern also exactly at midnight. When the satellite's signal reaches the receiver, its transmission of the pattern will lag a bit behind the receiver's playing of the pattern.
The length of the delay is equal to the signal's travel time. The receiver multiplies this time by the speed of light to determine how far the signal traveled. Assuming the signal traveled in a straight line, this is the distance from receiver to satellite.
In order to make this measurement, the receiver and satellite both need clocks that can be synchronized down to the nanosecond. To make a satellite positioning system using only synchronized clocks, you would need to have atomic clocks not only on all the satellites, but also in the receiver itself. But atomic clocks cost somewhere between $50,000 and $100,000, which makes them a just a bit too expensive for everyday consumer use.
The Global Positioning System has a clever, effective solution to this
problem. Every satellite contains an expensive atomic clock, but the receiver
itself uses an ordinary quartz clock,
which it constantly resets. In a nutshell, the receiver looks at incoming
signals from four or more satellites and gauges its own inaccuracy.
Differential GPS
When you measure the distance to four located satellites, you can draw four spheres that all
intersect at one point. Three spheres will intersect even if your numbers are
way off, but four spheres will not intersect at one point if you've
measured incorrectly. Since the receiver makes all its distance measurements
using its own built-in clock, the distances will all be proportionally
incorrect.
The receiver can easily calculate the necessary adjustment that will cause the four spheres to intersect at one point. Based on this, it resets its clock to be in sync with the satellite's atomic clock. The receiver does this constantly whenever it's on, which means it is nearly as accurate as the expensive atomic clocks in the satellites.
In order for the distance information to be of any use, the receiver also has to know where the satellites actually are. This isn't particularly difficult because the satellites travel in very high and predictable orbits. The GPS receiver simply stores an almanac that tells it where every satellite should be at any given time. Things like the pull of the moon and the sun do change the satellites' orbits very slightly, but the master control station constantly monitors their exact positions and transmits any adjustments to all GPS receivers as part of the satellites' signals.
This system works pretty well, but inaccuracies do pop up. For one thing, this method assumes the radio signals will make their way through the atmosphere at a consistent speed (the speed of light). In fact, the Earth's atmosphere slows the electromagnetic energy down somewhat, particularly as it goes through the ionosphere and troposphere. The delay varies depending on where you are on Earth, which means it's difficult to accurately factor this into the distance calculations. Problems can also occur when radio signals bounce off large objects, such as skyscrapers, giving a receiver the impression that a satellite is farther away than it actually is. On top of all that, satellites sometimes just send out bad almanac data, misreporting their own position.
Differential GPS (DGPS) helps correct these errors. The basic idea is
to gauge GPS inaccuracy at a stationary receiver station with a known location.
Since the DGPS hardware at the station already knows its own position, it can
easily calculate its receiver's inaccuracy. The station then broadcasts a radio
signal to all DGPS-equipped receivers in the area, providing signal correction
information for that area. In general, access to this correction information
makes DGPS receivers much more accurate than ordinary receivers.
Using the Data
We have seen that the most
essential function of a GPS receiver is to pick up the transmissions of at least
four satellites and combine the information in those transmissions with
information in an electronic almanac, all in order to figure out the receiver's
position on Earth.
Once the receiver makes this calculation, it can tell you the latitude, longitude and altitude (or some similar measurement) of its current position. To make the navigation more user-friendly, most receivers plug this raw data into map files stored in memory. You can use maps stored in the receiver's memory, connect the receiver to a computer that can hold more detailed maps in its memory, or simply buy a detailed map of your area and find your way using the receiver's latitude and longitude readouts. Some receivers let you download detailed maps into memory or supply detailed maps with plug-in map cartridges.
For the mariner, a standard GPS receiver will not only place you on a chart at any particular
location, but will also trace your path across the chart as you move. If you leave
your receiver on, it can stay in constant communication with GPS satellites to
see how your location is changing. With this information and its built-in clock,
the receiver can give you several pieces of valuable information:
You should never rely on only one method of navigation, especially if you will be out of sight of land. You should not rely solely on your GPS. You should use every method of navigation available and compare the results to make sure that you are where you think you are.
Note that the Global Positioning System operates on the Geodetic Datum WGS84. Your receiver must be set to this datum. See the note on all marine charts.
For more info on Geodetic Datums, see | Chart Datums | and | Datums and Coordinates. |