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SATNAV . . .
That’s right – satellite navigation signals, including those from the Global
Positioning System (GPS), can be picked up in space and used to determine
the receiver’s position. It’s a bit tricky since signals from these satellites
were only intended to be used within the Earth’s atmosphere. But with some
intelligent engineering and calculations, it can be done. There is even the
possibility that our Moon might get its own navigation satellites!
W
ith the likely forthcoming return to the Moon
(possibly as early as 2024), and ongoing space
exploration, it is vital to have reliable and accurate means to navigate in space.
Of particular interest for lunar exploration are ice deposits in craters near the south pole of the Moon, which
could be used for drinking water and also turned into hydrogen and oxygen for rocket fuel and breathing.
We have GPS and other satellite navigation systems here
on Earth, as described in detail in the November 2019 issue (siliconchip.com.au/Article/12083).
Those systems were designed for determining location
in the terrestrial, atmospheric and the near-Earth space environment. But could those same signals be used in space
or on the Moon?
GPS and other GNSS satellites orbit at an altitude of
around 20,000km so, in principle, any vehicle below that
altitude should be able to ‘see’ the satellites and make a
position fix. Since the antennas look down, one might
think it’s not possible to get a signal above the orbit of a
GPS satellite, but that is not the case.
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According to NASA, GPS signals can be received and
used in space in the same manner as on Earth, up to an
altitude of 3000km. NASA calls the space between the
surface of the Earth and an altitude of 3000km the “Terrestrial Service Volume” (see Fig.1). In this volume, GPS
works normally according to the GPS Standard Positioning Service (SPS) Performance Standard (www.gps.gov/
technical/ps/).
The volume at altitudes between 3000km and 36,000km
(geosynchronous satellite orbit) is defined by NASA as the
“Space Service Volume”. In this volume, which is subdivided into two parts, performance is not guaranteed to be
as good as in the Terrestial Service Volume.
As 36,000km is well above the 20,000km altitude of the
GPS satellite constellation, you might think that the signals could not be received because the GPS antennas are
pointing down toward Earth and not up. But there is another way the GPS signal can be received.
Instead of receiving a signal from a satellite above you,
you could receive a signal from a satellite on the opposite side of the Earth (see Fig.2). Its antenna is pointing
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. IN SPACE!
by Dr David Maddison
Fig.1: the “service volumes” for GPS, with the Terrestrial
Service Volume being everything below
3000km altitude. The GPS satellite and geosynchronous
orbit altitudes are also shown for comparison.
down toward Earth, but some of the signal would reach
your receiver.
A high Earth orbit (HEO) satellite and its trajectory,
which varies in altitude, is shown in Fig.2. Its path extends from the Terrestrial Service Volume, below 3000km,
to beyond the geosynchronous orbit altitude of 35,887km
(rounded to 36,000km) which is beyond even the Space
Service Volume.
The signal from one GPS satellite is shown, along with
the first side lobes (off-axis antenna radiation pattern) for
the L1 GPS frequency of 1575.42MHz. Fig.3 shows this radiation pattern in more detail. The receiving satellite can
obtain a GPS signal from the satellite shown from either
the main lobes or the first side lobes, or the signal may be
entirely blocked by the Earth.
Around 97% of radio energy is located in the main lobe
and just 3% in the side lobes, so a sensitive receiver is
needed. Only one GPS satellite is shown for simplicity;
in reality, other satellites will be visible and not blocked
by the Earth. As with terrestrial GPS, four satellites are
required for an accurate position fix.
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Fig.2: this shows how GPS signals are received in space,
even when the receiving spacecraft is above the orbit of the
GPS satellites. The dark green circle is the Earth, while the
lighter green shaded area is the umbra or shadow of the
Earth, where the satellite signals are blocked. The
receiving satellite is in an elliptical orbit encompassing
all possible volumes of space accessible with GPS.
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October 2020 11
Fig.3: a simplified generic diagram showing the radiation
pattern from GPS or similar antennas. The main lobe
of a GPS satellite is generally not available in space as
it is blocked by the Earth, but the first side lobe may be
available. The other side lobes and back lobe would be too
weak to be usable. Source: NASA.
Earlier versions of GPS satellites did not consider performance in the Space Service Volume and performance
was variable due to different side lobe radiation patterns
and power levels. This was addressed by NASA and the
US Department of Defense by writing specifications for
performance levels for the Space Service Volume during
2003-2005.
These specifications were implemented on Block III, SV
11+ (Space Vehicle 11) and subsequent GPS satellites.
It doesn’t matter where the receiver is located; if the signals from four GPS satellites can be received, then you can
identify your position in space. This should even work on
the surface of the Moon. However, additional calculations
would be needed to establish the relationship between the
Fig.4: GPSPAC was the first attempt to pick up GPS signals
in space. It was launched aboard LANDSAT 4 in 1982.
Source: USGS.
location of the Moon and the Earth to establish one’s position on the surface of the Moon.
Positional accuracy on the Moon will be less than on
Earth due to the much greater distances involved, resulting
in more significant timing and thus distance errors.
The distance from the centre of the Earth to the centre of the Moon averages 385,000km. But it varies by over
50,000km, and it can change as rapidly as 75m/s (270km/h).
These are important factors to keep in mind when using
GPS on the Moon, and they need to be incorporated in the
relevant calculations.
Based on an Earth radius of 6371km, a Moon radius of
1737km and a GPS satellite altitude of 20,183km, the closest a GPS receiver on the Moon could be to a GPS satellite
Figs.5&6: command and telemetry boards carried by TEAMSAT. This gives you an idea of the relatively basic electronics
used in the late 90s. Interestingly, both boards seem to be centred around FPGAs (field-programmable gate arrays).
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is 356,709km. That’s more than 17 times further than the
same receiver on Earth.
However, to receive a GPS signal on the Moon, that signal would have to come from a satellite on the far side of
the Earth, over 409,817km away. That’s 20 times further
away than the nearest a GPS receiver could be to a satellite on Earth.
Hence, timing and distance errors will be around 20 times
greater than on Earth (as rough figures), assuming the accuracy of the receiver clock is the same in both locations.
Note that GPS is already routinely used in the near-Earth
environment with vehicles such as low Earth orbit satellites and the International Space Station and its Crew Return Vehicle, as they are all well below the altitude of the
GPS satellites.
The limits of GPS
Currently, the formal altitude limit of GPS is that of the
outer limits of the Space Service Volume of 36,000km; but
the real practical limits are not yet known. Limits are imposed by the available signal strength, signal availability as
determined by geometric limitations imposed by satellite
antenna main and sidelobe patterns, and the occultation
(blocking) of GPS satellite signals by the Earth.
Uses for high orbital altitude GPS
The ability for satellites and other space vehicles to use
GPS at high orbital altitude confers many advantages due
to better knowledge of space vehicle location.
These include:
• better satellites station-keeping
• improved space vehicle rendezvous and docking
• geosynchronous satellite servicing possibilities
• better Earth science measurements including atmospheric, ionospheric, geodesy and geodynamics
• better navigation by uncrewed launch vehicles
• formation flying of constellations of satellites such as
MMS (magnetospheric multiscale mission; see below)
• improved weather satellites
• improved space weather observations
• improved astrophysical observations due to better navigation by orbiting telescopes
• better navigation en-route to the Moon and on the Moon
• closer spacing of satellites in geostationary orbit due to
better location fixes
• use of GNSS for time synchronisation of science experiments and space vehicle clock.
High orbital altitude GPS experiments
It had long been speculated that GPS could be used above
the maximum orbital altitude of the constellation. Many
GPS receivers were launched into space from 1982, and
especially from 1991 onwards, mainly in the Terrestrial
Service Volume (below 3000km).
For a complete list up to 2003 see http://gauss.gge.unb.
ca/grads/sunil/missions.htm
Note that GPS became available to civilians in 1983.
Significant early experiments with high altitude GPS use
were as follows:
• The first time GPS was installed on a satellite was LANDSAT 4 in 1982 (Fig.4). It carried a package known as GPSPAC. Three more GPSPAC units were also launched on
LANDSAT 5 in 1984 and US Department of Defense vesiliconchip.com.au
Fig.7: TEAMSAT, launched in 1997, carried YES (Young
Engineers’ Satellite). Its primary purpose was to study
GPS reception at altitudes above the GPS constellation
(20,183km). Source: ESA.
hicles in 1983 and 1984. The GPS constellation was not
fully operational at that time, and four satellites were in
view for just a few hours per day. The GPSPACs provided
essential data that was used in the development of the
rest of the Global Positioning System.
• Falcon Gold was an experiment of the US Air Force
Academy in 1997 to use a GPS receiver above the altitude of GPS satellites. The GPS signal was received up
to an altitude of 33,000km. The experiment confirmed
the possibility of using GPS in locations above the orbit
of the GPS satellite constellation, plus the ability to use
GPS sidelobe signals for navigation, previously a matter of debate.
• YES (Young Engineers’ Satellite) was launched in 1997
as a sub-satellite of TEAMSAT (Figs.5-7), which itself
was part of MaqSAT H. An orbit of 531 × 26,746 km was
achieved, with its primary purpose to study GPS reception at altitudes above the GPS constellation.
• Also in 1997, a GPS receiver was flown in the high Earth
orbit satellite Equator-S (Fig.8), above the altitude of the
GPS satellites. No navigation solution was possible because the required four satellites could not be simultaneously seen; however, useful signals were received at
an altitude up to 61,000km.
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October 2020 13
Fig.8: Equator-S was also launched in 1997 and carried
a GPS receiver. It was not able to get a location fix, but it
was determined that useful signals could be picked up at
altitudes of up to 61,000km.
Fig.9: the AMSAT (OSCAR-40) amateur satellite was
launched in 2000. In 2001, its onboard GPS receiver picked
up valid signals to the satellite’s maximum altitude of
60,000km, and mapped the main and sidelobe signals.
• In 2000, Kronman et al. were able to perform orbit determination of a geosynchronous satellite which received
GPS signals from the far side of the Earth and then retransmitted them to a ground-based receiver where all
data processing was performed, to determine the satellite’s orbit (see Fig.10).
The use of a satellite just to relay signals is known as
“bent pipe architecture”. No suitable receiver was available
off the shelf, so one had to be made. According to Kronman,
the following features were required but not commercially
available at the time in one unit:
The ability to navigate off the Earth (for acquisition), a
second-order tracking loop to accommodate anomalous Doppler, the ability to accept commands to track specific PRNs
(Pseudorandom Noise code), the availability of individual
PRN pseudorange data referenced to a precise local time
source, Selective Availability correction without P(Y)-code
capability (military encryption).
• In 2000, the AMSAT Phase 3-D (OSCAR-40) amateur satellite (Fig.9) was launched with NASA-sponsored GPS
experiments onboard, using existing receiver technology. The actual GPS experiment was done in 2001. It
received signals up to the satellite’s maximum altitude
of 60,000km, and mapped main and sidelobe signals.
As with the previous experiments, actual GPS locations
were computed on the ground rather than the satellite, and
not in real time. Based on the results, it was determined
that navigation considerably above 60,000km could be
performed with a suitable receiver and antenna.
• Also in 2000, two STRV-1 (Space Technology Research
Vehicle) missions were launched, the STRV-1c and STRV1d spacecraft (Fig.11). They had a 615 x 39,269km orbit.
They were equipped with GPS receivers which mapped
GPS signals to geosynchronous orbit, approximately
36,000km up.
• GIOVE-A (Galileo In-Orbit Validation Element-A) was a
European Space Agency (ESA) satellite launched in 2005
and retired in 2012 (Fig.12). Its purpose was to test aspects
of Europe’s GNSS navigation system, Galileo.
According to the ESA, its primary objective was to “secure vital frequency filings, generate the first Galileo navigation signals in space, characterise a prototype rubidium
atomic clock, and model the radiation environment of Medium Earth Orbit (MEO) for future Galileo spacecraft”. The
satellite was equipped with a GPS receiver.
In 2006, the receiver was activated for 90 minutes, and it
was confirmed that it could receive GPS data and it downloaded a full almanac. After its retirement, it was moved to
a “graveyard” orbit 100km above the Galileo constellation
altitude of 23,222km. That is beyond the 20,183km altitude
of the GPS constellation.
In the retirement phase, in 2013, new software was up-
600 nmi
(1.5 SCD
at GEO)
GPS
26
,5
60
km
Nominal
Visibility
Region
12.2°
GEO
42,200km
Fig.10: the relative geometry of a GPS
satellite, geosynchronous satellite (GEO) and Earth for the
Kronman et al. experiment in 2000. It is the sidelobes of the GPS satellite transmissions that
are being received. The GEO satellite receives signals in the shaded zone from 1.5 to 3.5 degrees above the limb of the Earth.
EARTH
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Fig.11: STRV-1c and STRV-1d (Space Technology Research
Vehicle), launched in the year 2000. They were equipped
with GPS receivers which mapped GPS signals to
geosynchronous orbit, approximately 36,000km up.
loaded to the GPS receiver on the satellite, and more extensive tests were made. Particular emphasis was made on
measuring properties of the GPS satellite sidelobe signals.
Current civilian missions using high-altitude GPS
In 2015, NASA launched the MMS (Magnetospheric Multiscale) mission (Phase 1) which is a four-satellite constellation which flies in a tetrahedral formation 7.2km apart, to
study aspects of the Earth’s magnetic field (Fig.13).
Each was equipped with a highly sensitive high-altituderated GPS receiver called Navigator for real-time position
x
Fig.12: GIOVE-A (Galileo In-Orbit Validation Element-A)
was launched in 2005, to test aspects of Europe’s GNSS
navigation system, Galileo.
measurements (see Fig.14). In 2016 and 2019, the highest
altitude GPS fixes to date were obtained at 70,006km and
187,167km respectively.
The Navigator GPS receiver is designed for fast and weak
GPS signal acquisition, and it is the highest operational
GPS receiver to date, at a distance of around halfway to the
Moon. It is designed to work in a variety of space regimes
such as low Earth orbit (LEO), geosynchronous orbit (GEO),
high Earth orbit (HEO), up to and beyond 12 Earth radii
(76,452km+), at launch and re-entry.
Pseudorange is the distance measured between the GPS
Other means of navigating the Moon
There is no significant magnetic field on the Moon, so a compass cannot be used. Also, the lack of atmosphere makes it hard for
astronauts to judge distances. The Apollo 14 crew missed a crater
they had intended to visit by only 30m because of these difficulties.
When Neil Armstrong landed the LEM on the Moon in 1969, he
used his eyes and maps to find the appropriate place to land (the
famous Apollo Guidance Computer was not intended to locate the
exact landing place). In space it is always good to have a backup
plan, so apart from NASA developing lunar GPS, they are also developing “terrain relative navigation” (see below).
This is similar to what Neil Armstrong did, but instead of using
eyes to compare lunar terrain to a map, a computer compares the
lunar terrain (imaged with a camera) to maps in the computer’s
memory.
Apart from terrain relative navigation, returning astronauts will
also use GPS, navigation Doppler lidar and hazard detection lidar.
Other methods that will be used to navigate on the Moon include:
• radiometric methods utilising the existing Deep Space Network to
measure range and speed (updated to allow for lunar tracking).
• lunar orbiting spacecraft such as the LRS (see separate panel).
and lunar surface stations such as the LCT (same panel).
• inertial navigation.
• optical techniques such as viewing stars relative to lunar surface features.
Images from a test of NASA’s terrain relative navigation in the Mojave Desert. The live image is on the left, and a
reconstructed image is on the right. It identifies and matches known features in the images to determine the current position.
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October 2020 15
The Lunar Relay Satellite (LRS) and Lunar Communications Terminal (LCT)
Apart from navigation on the Moon via GPS, for effective communications (especially if people are living on the Moon’s surface), it will be desirable or even necessary to have lunar relay
satellites along with a Lunar Communications Terminal (LCT).
NASA has proposed a system of two satellites to relay communications between the surface of the Moon and the Earth, as
well as crewed lunar vehicles, all part of the Artemis program.
These vehicles include Orion, to launch from Earth and orbit the
Moon, and the Altair lunar lander, to take the crew from Orion
to the surface of the Moon.
The orbit will be a “12 hour frozen elliptical lunar orbit”. This
is a special type of highly elliptical stable orbit. It is required
because above about 1200km altitude, Moon orbits are usually
unstable and short-lived (tens of days) due to the ‘tug-of-war’
with the Earth’s gravity.
Below 1200km, the inherent ‘lumpiness’ of the Moon and
thus variations in gravity cause orbits to be unstable and shortlived as well.
The proposed LRS satellites will have a service life of 7-10
years, a data bandwidth of 100Mbps from lunar habitats and the
LCT, and 50Mbps from elsewhere on the lunar surface.
The LCT will be a communications node for rovers, crew, habitats, science experiments etc. It will provide some navigational
support, 802.16 wireless LAN and line of sight communications
to 6km and have a 1m Ka-band antenna.
Navigation support will be in the form of one- and two-way
ranging to determine the range of a vehicle to the LCT, Doppler
satellite and the receiving satellite, and differs somewhat
from the true range due to several physical effects.
Its measurement precision depends on the signal strength
received (see Fig.15), but simulations show that the pseudorange with strong signals is better than ±1.5m. The pseudorange with weak signals is better than ±13m, and for measurements when a strong carrier phase signal is present, precision is better than ±1mm.
The receiver has been tested at velocities up to 10km/s.
An artist’s rendering of NASA’s proposed Lunar Relay
Satellite (LRS) along with the Moon based Lunar
Communications Terminal (LCT).
tracking for measurement of the range from space vehicles to
the LCT and beacon signals.
There are no official Internet top-level domains (TLDs) currently assigned to the Moon but, .ln, .le (lunar embassy) and
.lunar have been unofficially proposed.
However, they are not currently supported by the root servers.
It has also tracked as many as 12 GPS satellites simultaneously, many more than expected.
GOES-16 or Geostationary Operational Environmental
Satellite was launched in 2016; it is a weather satellite in
geostationary orbit. It is the first civilian geostationary satellite to use GPS for orbit determination. This will be used,
along with other equipment, to maintain an orbital position
within a 100m radius.
Extending GPS to the Moon
High-altitude GPS research has the ultimate objective of
extending GPS for use on the Moon, and NASA plans to use
existing GPS infrastructure to do this. The GPS receiver that
Fig.13: an artist’s concept of the MMS satellite constellation
examining so-called “magnetic reconnection” phenomena
in the Earth’s magnetic field (represented by blue lines). The
exact satellite locations must be known to create accurate
magnetic field maps, hence the use of GPS. Source: NASA.
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Fig.14: the Navigator GPS receiver, as used on MMS
mission satellites for high-altitude GPS fixes.
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Perigee
Apogee
Perigee
Hz
Strong
(main
lobe)
signals
Apogee: most
signals in
side lobes
Weak
(side lobe)
signals
Fig.15: measurements of signal strengths vs position in orbit for MMS mission
satellites. Strong main lobe signals are shown above the dotted line, while weaker side lobe signals (the majority) are
below. This shows the importance of sidelobe signals for satellites orbiting above the GPS constellation. Apogee is the
point of an orbit farthest from Earth and perigee is closest to Earth. Source: NASA.
will be used for this is based on the Navigator described
above, and the NavCube which we will soon discuss.
For use beyond its current orbit of almost halfway to the
Moon, the Navigator GPS will be enhanced with a higher-gain
antenna (up to 14dB of gain), antenna steering to keep the
antenna pointed towards Earth and the GPS constellation, a
more accurate clock and various other updated electronics.
While NASA is intending to leverage existing GPS infrastructure for Lunar use, it is not a perfect solution and will
also not work on the dark (far) side. It will be augmented by
other methods. The idea of building a mini GPS-like system
around the Moon called LunaNet is also still under consideration for the much longer term (see Fig.16). Apart from
Fig.16: an artist’s concept of LunaNet, providing
navigation, communications and other services on the
Moon.
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navigation, it would provide many other services, such as
communications.
NavCube
NavCube (Fig.17) is a combination of two NASA technologies. One is SpaceCube, which is a reconfigurable and fast
flight computing platform, and the other is the Navigator
GPS receiver used in the MMS mentioned above.
For high-altitude and near- or on-Moon real-time GPS fixes, a powerful computer is needed for data processing. The
NavCube combines both the GPS receiver and the com-
Fig.17: NASA’s NavCube. It uses a Navigator GPS receiver
and has substantial computing abilities for processing GPS
signals in lunar orbits and on the surface of the Moon. It
measures 25 x 20 x 15cm and weighs around 5kg.
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October 2020 17
puter. NavCube can also provide precise timing signals
for another experiment using X-rays for communications
(XCOM). A NavCube was recently placed on the International Space Station for testing.
Estimates of the accuracy of GPS on the Moon with NavCube vary. The worst accuracy is considered to be around
1km, which is useful enough but not ideal. With a highly
accurate atomic clock onboard, or accurate time signals
beamed from the proposed Lunar Gateway (see Figs.18 &
19), it could be improved to around 100m.
The Lunar Gateway is a mini space station proposed to
orbit the Moon in 2024 as a communications hub, labo-
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ratory, habitation module and a holding station for lunar
equipment.
Cheung, Lee et al. have estimated an accuracy figure of
200-300m based on modelling. Meanwhile, Winternitz,
Bamford et al. came up with several estimates depending on
whether the Lunar Gateway is crewed or uncrewed, as the
presence of crew causes perturbations which affect accuracy.
For GPS in conjunction with an onboard rubidium atomic
frequency and an uncrewed vessel, the lateral position accuracy is 31m, and the range accuracy is 9m; for a crewed
vessel, the figures are 77m lateral and 21m in range. With
ground tracking from the Earth using the Deep Space Net-
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work (no GPS), uncrewed accuracy is 468m lateral and
33m in range; crewed is 8144m lateral and 451m in range.
The first demonstration of lunar GPS could be in November 2021, with the launch of an uncrewed Orion capsule
on the Artemis 1 mission (to be launched with the Space
Launch System). Orion will record GPS signals throughout
the mission to determine the usefulness, and measure signal characteristics of GPS around the Moon.
Problems with using GPS in space
The speed of space vehicles requires fast signal acquisition. There is also the problem of much lower signal strength
due to having to rely on side lobe signals, and also the long
ranges from the GPS satellites.
Additional problems include large dynamic ranges between “weak” and “strong” satellites with wide signal gain
variability; high Doppler and Doppler rates of change of GPS
signals; fewer GPS satellite signals visible; mission antenna
placement causing visibility problems; multipath reflections
and radiation on very dynamic platforms.
Table 1 expands on these problems and their solutions.
How much accuracy does Lunar GPS require?
Terrestrial GPS can achieve accuracies of around one
Fig.18: the Lunar Gateway “lunar space station” concept, showing an Orion
spacecraft docking. The Orion will carry GPS and test it in the lunar environment as
early as November 2021. The Lunar Gateway, when placed into lunar orbit in 2024,
will also carry GPS with signals augmented by a very accurate onboard atomic clock.
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October 2020 19
Fig.19: an artist’s rendering of the Lunar Gateway. It
could help provide navigation services on the Moon by
transmitting a highly accurate timing signal to improve the
accuracy of lunar-based GPS.
Fig.20: an artist’s concept of a mining operation on the
Moon. Accurate navigation will be necessary for such
activities. Note the mirrors used to illuminate the area.
metre or better. Lunar GPS will be somewhat less accurate;
however, there are no roads to locate on the Moon, and any
target location such as a crater, mining site or base will be
visually apparent. So accuracies of even a few hundred
metres will be adequate.
For autonomous vehicles or other applications requiring greater navigational accuracy, this could be achieved by
augmentation with beacons and machine vision, plus artificial intelligence (AI) to avoid obstacles or locate targets in
outer space..
Regime
Altitude
Problems
Terrestrial Service
Under 3000km
High Doppler rates,
Volume
fast signal rise and set,
accurate ephemeris
upload required,
signal strength and
availability
comparable to
Earth use
Lower Space
3000-8000km
Service Volume
More GPS signals
available than for
terrestrial service
volume; very high
Doppler rates
Upper Space
8000-36,000km
Earth shadow
Service Volume
significantly reduces
main lobe signal;
significant periods
with fewer than four
satellites available;
weak signal strength
Beyond Space
36,000-360,000km
Very weak signals
Service Volume
(Moon)
and very poor signal
geometry
Mitigation
Development of
In widespread use
purpose-built space
receivers; fast
acquisition eliminates
the need for ephemeris
upload (data for
estimated position of
GPS receiver
relative to satellites)
Improved antennas;
receivers must be able
to process higher
Doppler rates
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In use by the USA
and others
Higher gain antennas,
In use by the USA
more sensitive receivers,
and others
use of GPS side lobe
transmissions, algorithms
such as in GEONS
software to navigate
with fewer than
four satellites
Higher gain antennas
and receivers; accept
degraded performance;
use other signals of
opportunity if possible,
eg, beacons, perhaps
from LCT or LRS
(see panel)
Table 1 – Problems and solutions for spaceborne GPS. Based on J.J.K. Parker, NASA.
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In use to 187,000km
by MMS (USA);
will be extended to
lunar orbit on
Artemis 1 mission
in 2021
SC
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