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The Planets .... brought to you by QuasArt Web Designs.
SPACECRAFT
AND MISSIONS
PAST
MISSIONS
ONGOING
MISSIONS
FUTURE MISSIONS 
- Luna
2
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impact on the surface of the Moon
1959 (USSR)
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first photos of the far side of the Moon
1959 (USSR)
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the
first successful probe to flyby Venus in December of 1962, and it returned information which
confirmed that Venus is a very hot (800 degrees Fahrenheit, now
revised to 900 degrees F.) world with a cloud-covered atmosphere
composed primarily of carbon dioxide.
(more
info from NASA Spacelink)
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launched on November 5, 1964, was lost when its
protective shroud failed to eject as the craft was placed into
interplanetary space. Unable to collect the Sun's energy for power
from its solar panels, the probe soon died when its batteries
ran out and is now in solar orbit. It was intended for a Mars
flyby with Mariner 4.
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the
sister probe to Mariner 3, did reach Mars in 1965 and took the first close-up images of the Martian
surface (22 in all) as it flew by the planet. The probe found
a cratered world with an atmosphere much thinner than previously
thought. Many scientists concluded from this preliminary scan
that Mars was a "dead" world in both the geological and biological
sense.
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Mariner 9, the sister probe to Mariner 8 which
failed on launch, became the first craft to orbit Mars
in 1971. It returned information on the Red Planet that no other
probe had done before, revealing huge volcanoes on the Martian
surface, as well as giant canyon systems, and evidence that water
once flowed across the planet. The probe also took the first detailed
closeup images of Mars' two small moons, Phobos
and Deimos.
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6 manned landings on the Moon
and sample returns 1969-72. (The seventh landing, Apollo 18, was
canceled for political reasons)
(Apollo
"home page"; Apollo
Missions)
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automated sample return from the Moon
1970 (USSR)
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Pioneer 10 was the first spacecraft to flyby Jupiter
in 1973. Pioneer 11 followed it in 1974,
and then went on to become the first probe to study Saturn
in 1979. The Pioneers were designed to test the ability of spacecraft
to survive passage thru the asteroid belt and Jupiter's magnetosphere.
The asteroid belt was easy, but they were nearly fried by ions
trapped in Jupiter's magnetic field. This information was crucial
to the success of the Voyager missions.
Pioneer 11's RTG power supply is dead. Its last
communication with Earth was in November 1995. Pioneer 10 is still
functioning (barely) but is no longer being tracked regularly
due to budget cutbacks. The last data was received from it on
1997 March 31. They are heading off into interstellar space, the
first craft ever to do so.
As the first two spacecraft to leave our solar system, Pioneer
10 & 11 carry a graphic message in the form of a 6- by 9-inch
gold anodized plaque bolted to the
spacecraft's main frame.
(Pioneer
Project Home Page and more about Pioneer
10 and Pioneer
11 from NASA Spacelink; current status from
NASA Ames)
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used Venus as a gravity
assist to Mercury in 1974. The probe
did return the first close-up images of the Venusian atmosphere
in ultraviolet, revealing previously unseen details in the cloud
cover, plus the fact that the entire cloud system circles the
planet in four Earth days. Mariner 10 eventually made three flybys
of Mercury from 1974 to 1975 before running out of attitude control
gas. The probe revealed Mercury as a heavily cratered world with
a mass much greater than thought. This would seem to indicate
that Mercury has an iron core which makes up 75 percent of the
entire planet.
(more from JPL and JPL)
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First probe to return data from the surface of
another planet (Venus) in 1970.
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soft landing on Venus,
pictures of the surface 1975. (USSR) This was the first spacecraft
to land on the surface of another planet.
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1978; orbiter and four atmospheric probes; made
the first high-quality map of the surface of Venus.
(more
info from NASA Spacelink; and NSSDC
a tutorial
from UCLA)
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Viking 1 was launched from Cape Canaveral, Florida
on August 20, 1975 on a TITAN 3E-CENTAUR D1 rocket. The probe
went into Martian orbit on June 19, 1976, and the lander set down on
the western slopes of Chryse Planitia on July 20, 1976. It soon
began its programmed search for Martian micro-organisms (there
is still debate as to whether the probes found life there or not),
and sent back incredible color panoramas of its surroundings.
One thing scientists learned was that Mars' sky was pinkish in
color, not dark blue as they originally thought (the sky is pink
due to sunlight reflecting off the reddish dust particles in the
thin atmosphere). The lander set down among a field of red sand
and boulders stretching out as far as its cameras could image.
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Viking 2 was launched on September 9, 1975, and
arrived in Martian orbit on August 7,
1976. The lander touched down on September 3, 1976 in Utopia Planitia.
It accomplished essentially the same tasks as its sister lander,
with the exception that its seismometer worked, recording one
marsquake.
The last data from Viking (Lander 1) made its final transmission
to Earth Nov. 11, 1982. Controllers at JPL tried unsuccessfully
for another six and one-half months to regain contact with Viking
Lander 1. The overall mission came to an end May 21, 1983.
An interesting side note: Viking 1's lander has been designated
the Thomas A. Mutch Memorial Station in honor of the late leader
of the lander imaging team. The National Air and Space Museum
in Washington, DC is entrusted with the safekeeping of the Mutch
Station Plaque until it can be attached to the lander by a manned
expedition.
(more info (pdf) and an web page from JPL)
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Voyager 1 (image at top) was launched September
5, 1977, and flew past Jupiter on March
5, 1979 and by Saturn on November 13,
1980. Voyager 2 was launched August 20, 1977 (before Voyager 1),
and flew by Jupiter on August 7, 1979, by Saturn on August 26,
1981, by Uranus on January 24, 1986, and by Neptune
on August 8, 1989. Voyager 2 took advantage of a rare once-every-189-years
alignment to slingshot its way from outer planet to outer planet.
Voyager 1 could, in principle, have headed towards Pluto,
but JPL opted for the sure thing of a Titan close up.
Between the two probes, our knowledge of the 4 giant planets,
their satellites, and their rings has become immense. Voyager
1&2 discovered that Jupiter has complicated atmospheric dynamics,
lightning and aurorae. Three new
satellites were discovered. Two of the major surprises were that
Jupiter has rings and that Io has active
sulfurous volcanoes, with major effects on the Jovian magnetosphere.
When the two probes reached Saturn, they discovered over 1000
ringlets and 7 satellites, including the predicted shepherd satellites
that keep the rings stable. The weather was tame compared with
Jupiter: massive jet streams with minimal variance (a 33-year
great white spot/band cycle is known). Titan's
atmosphere was smoggy. Mimas's appearance
was startling: one massive impact crater gave it the Death Star
appearance. The big surprise here was the stranger aspects of
the rings. Braids, kinks, and spokes were both unexpected and
difficult to explain.
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Voyager 2, thanks to heroic engineering and programming
efforts, continued the mission to Uranus
and Neptune. Uranus itself was highly
monochromatic in appearance. One oddity was that its magnetic
axis was found to be highly skewed from the already completely
skewed rotational axis, giving Uranus a peculiar magnetosphere.
Icy channels were found on Ariel, and
Miranda was a bizarre patchwork of
different terrains. 10 satellites and one more ring were discovered.
In contrast to Uranus, Neptune was found to have rather active
weather, including numerous cloud features. The ring arcs turned
out to be bright patches on one ring. Two other rings, and 6 other
satellites, were discovered. Neptune's magnetic axis was also
skewed. Triton had a canteloupe appearance
and geysers. (What's liquid at 38K?)
If no unforeseen failures occur, we will be able to maintain communications
with both spacecraft until at least the year 2030. Both Voyagers
have plenty of hydrazine fuel -- Voyager 1 is expected to have
enough propellant until 2040 and Voyager 2 until 2034. The limiting
factor is the RTGs (radio-isotope thermal generators). The power
output from the RTGs is slowly dropping each year. By 2000, there
won't be enough power for the UVS (ultraviolet spectrometer) instrument.
By 2010, the power will have dropped low enough such that not
all of the fields and particles instruments can be powered on
at the same time. A power sharing plan will go into effect then,
where some of the F&P instruments are powered on, and others off.
The spacecraft can last in this mode for about another 10 years,
and after that the power will probably be too low to maintain
the spacecraft.
(the Voyager Project Home Page
from JPL; another nice "home page" at NSSDC;
fact sheets and a web page from
JPL; General
Info from NASA/ARC)
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International
project VENUS-HALLEY, launched in 1984, carried a Venus orbiter
and lander and did a fly-by of Comet Halley.
(Vega Mission Home
page )
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Two spacecraft were launched by the USSR in 1988.
One failed with out a trace. A few images were returned before
the second one failed, too.
(Phobos Mission
Home page
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Giotto was launched by an Ariane-1 by ESA on July
2 1985, and approached within 540 km +/- 40 km of the nucleus
of Comet Halley on March 13, 1986. The
spacecraft carried 10 instruments including a multicolor camera,
and returned data until shortly before closest approach, when
the downlink was temporarily lost. Giotto was severely damaged
by high-speed dust encounters during the flyby and was placed
into hibernation shortly afterwards.
In April, 1990, Giotto was reactivated. 3 of the instruments proved
fully operational, 4 partially damaged but usable, and the remainder,
including the camera, were unusable. On July 2, 1990, Giotto made
a close encounter with Earth and was retargeted to a successful
flyby of comet Grigg-Skjellerup on July 10, 1992.
(more
info from NSSDC)
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a joint mission of the Ballistic Missile Defense
Organization (formerly SDIO) and NASA to flight test sensors developed
by Lawrence Livermore for BMDO. The spacecraft, built by the Naval
Research Lab, was launched on January 25 1994 to a 425 km by 2950
km orbit of the Moon for a 2 month mapping
mission. Instruments onboard include UV to mid-IR imagers, including
an imaging lidar that may be able
to also obtain altimetric data for the middle latitudes of the
Moon. In early May the spacecraft was
to have been sent out of lunar orbit toward a flyby of the asteroid
1620 Geographos but a failure prevented the attempt.
Ground controllers have regained control of the spacecraft, however.
Its potential future mission is being considered.
(for more information see the Clementine
Mission Home page from USGS and the Clementine
page from NASA PDS or The Clementine
Mission from LPI.)
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Mars orbiter including 1.5 m/pixel resolution camera.
Launched 9/25/92 on a Titan III/TOS booster. Contact was lost
with MO on 8/21/93 while it was preparing for entry into Mars
orbit. The spacecraft has been written off (postmortem
analysis). Mars Global Surveyor,
a replacement mission to achieve most of MO's science goals, is
scheduled to launch in November 1996.
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Launched in May 1989, Magellan has mapped 98% of
the surface of Venus at better than 300
meter resolution and obtained a comprehensive gravity field map
for 95 percent of the planet. Magellan recently executed an 80-day
aerobraking program to lower and circularize its orbit. Magellan
has completed its radar mapping and gravity data collection. In
the fall of 1994, just before it would have failed due to deterioration
in its solar panels, Magellan was deliberately sent into Venus'
atmosphere to further study aerobraking techniques which can make
major savings in fuel for future missions.
(more info (pdf), a web
page and another web
page from JPL; fact sheet from
NSSDC)
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a large orbiter with several landers originally
known as Mars 94. Launch failed 1996 November 17. (The original
Mars 96 was known for a while as Mars 98 and then cancelled.)
(more info from MSSS and from
IKI (Russia))
- Voyagers
1 and 2
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still operational after more than 15 years in space
and are traveling out of the Solar System. The two Voyagers are
expected to last until at least the year 2015 when their radioisotope
thermoelectric generators (RTG) power supplies are expected for
fail. Their trajectories give negative evidence about possible
planets beyond Pluto. Their next major scientific discovery should
be the location of the heliopause.
Low-frequency radio emissions believed to originate at the heliopause
have been detected by both Voyagers.
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Both Voyagers are using their ultraviolet spectrometers to map
the heliosphere and study the incoming interstellar wind. The
cosmic ray detectors are seeing the energy spectra of interstellar
cosmic rays in the outer heliosphere
Voyager 1 has passed the Pioneer 10 spacecraft and is now the
most distant human-made object in space.
(more info from
JPL)
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Jupiter
orbiter and atmosphere probe, now in Jupiter orbit. It will make
extensive surveys of the Jovian moons and the probe has descended
into Jupiter's atmosphere to provide our first direct evidence
of the interior of a gas giant.
Galileo has already returned the first resolved images of two
asteroids, 951 Gaspra and 243
Ida, while in transit to Jupiter. It has also returned pictures
of the impact of Comet SL9 onto Jupiter
from its unique vantage point.
Efforts to unfurl the stuck High Gain Antenna (HGA) have essentially
been abandoned. With its Low Gain Antenna Galileo transmits data
at about 10 bits per second. JPL has developed a backup plan using
enhancements of the receiving antennas in the Deep Space Network
and data compression (JPEG-like for images, lossless compression
for data from the other instruments) on the spacecraft. This should
allow Galileo to achieve approximately 70% of its original science
objectives with the much lower speed Low Gain Antenna. Long term
Jovian weather monitoring, which is imagery intensive, will suffer
the most.
Galileo Schedule (times UTC) ---------------- 10/18/89 - Launch from Space Shuttle
02/09/90 - Venus Flyby 10/**/90 - Venus Data Playback 12/08/90 - 1st Earth Flyby
05/01/91 - High Gain Antenna (was to have) Unfurled 07/91 - 06/92 - 1st Asteroid
Belt Passage 10/29/91 - Asteroid Gaspra Flyby 12/08/92 - 2nd Earth Flyby 05/93
- 11/93 - 2nd Asteroid Belt Passage 08/28/93 - Asteroid Ida Flyby 07/13/95 - Probe
Separation 07/20/95 - Orbiter Deflection Maneuver 12/07/95 - Jupiter Encounter
06/27/96 06:30 - Ganymede-1 09/06/96 19:01 - Ganymede-2 11/04/96 13:30 - Callisto-3
11/06/96 18:42 - Europa-3A ("non-targeted" flyby @32,000 km on the same orbit
as Callisto-3) 12/19/96 06:56 - Europa-4 01/20/97 01:13 - Europa-5A (flyby @27,400
km during solar conjunction - counts for gravity - not science) 02/20/97 17:03
- Europa-6 04/04/97 06:00 - Europa-7A ("non-targeted" @23,200 km on the Ganymede-7
orbit) 04/05/97 07:11 - Ganymede-7 05/06/97 12:12 - Callisto-8A ("non-targeted"
@33,500 km on the Ganymede-8 orbit) 05/07/97 15:57 - Ganymede-8 06/25/97 13:48
- Callisto-9 06/26/97 17:20 - Ganymede-9A ("non-targeted" @80,000 km on the Callisto-9
orbit) 09/17/97 00:21 - Callisto-10 11/06/97 21:47 - Europa-11 (more details)
Galileo's extended mission has been approved. If
all goes well, it will spend another two years focusing primarily
on Europa.
(Education and Public Outreach
(images!); Galileo Home Page; Galileo Probe Home Page and
more info from JPL;
newsletter; web
page; NSSDC page; preliminary
Galileo Probe Results from JPL and ARC and
LANL)
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launched April 1990; fixed December 1993. HST can
provide pictures and spectra over a long period of time. This
provides an important extra dimension to the higher resolution
data from the planetary probes. For example, recent HST data show
that Mars is colder and drier than during
the Viking missions; and HST images of Neptune
indicate that its atmospheric features change rapidly.
Named for the American astronomer Edwin Hubble.
Much, much more information about HST and HST pictures are available
at the Space Telescope
Science Institute. HST's latest
images are posted regularly. (Here is a brief history
of the HST project. There's also some more
HST info at JPL.)
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now investigating the Sun's
polar regions (European Space Agency/NASA). Ulysses was launched
by the Space Shuttle Discovery in October 1990. In February 1992,
it got a gravity boost from Jupiter and to take it out of the plane of the ecliptic.
It has now completed its main mission of surveying both of the
Sun's poles. Its mission has been extended for another orbit so
that it can survey the Sun's poles near the maximum of the sunspot
cycle, too. Its aphelion is 5.2
AU, and, surprisingly, its perihelion is about 1.5 AU-- that's
right, a solar-studies spacecraft that's always further from the
Sun than the Earth is! It expected to provide a much better understanding
of the Sun's magnetic field and the solar
wind.
(Ulysses Home Pages from JPL
and ESA; yet
more info
from JPL)
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After its November 1, 1994, launch, NASA's Wind
satellite will take up a vantage point between the Sun and the
Earth, giving scientists a unique opportunity to study the enormous
flow of energy and momentum known as the solar wind.
The main scientific goal of the mission is to measure the mass,
momentum and energy of the solar wind that somehow is transferred
into the space environment around the Earth. Although much has
been learned from previous space missions about the general nature
of this huge transfer, it is necessary to gather a great deal
of detailed information from several strategic regions of space
around the Earth before scientists understand the ways in which
the planet's atmosphere responds to changes in the solar wind.
The launch also marks the first time a Russian instrument will
fly on an American spacecraft. The Konus Gamma-Ray Spectrometer
instrument, provided by the Ioffe Institute, Russia, is one of
two instruments on Wind which will study cosmic gamma-ray bursts,
rather than the solar wind. A French instruments is also aboard.
At first, the satellite will have a figure-eight orbit around
the Earth with the assistance of the Moon's gravitational field.
Its furthest point from the Earth will be up to 990,000 miles
(1,600,000 kilometers), and its closest point will be at least
18,000 miles (29,000 kilometers).
Later in the mission, the Wind spacecraft will be inserted into
a special halo orbit in the solar wind upstream from the Earth,
at the unique distance which allows Wind to always remain between
the Earth and the Sun (about 930,000 to 1,050,000 miles, or 1,500,000
to 1,690,000 kilometers, from the Earth).
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The Near Earth Asteroid Rendezvous (NEAR) mission
promises to answer fundamental questions about the nature of near-Earth
objects such as asteroids and comets.
Launched on 1996 February 17 aboard a Delta 2 rocket, the NEAR
spacecraft should arrive in orbit around asteroid 433 Eros in
early January 1999. It will then survey the rocky body for a minimum
of one year, at altitudes as close as 15 miles (24 kilometers).
Eros is one of the largest and best-observed asteroids whose orbits
cross Earth's path. These asteroids are closely related to the
more numerous "Main Belt" asteroids that orbit the Sun in a vast
doughnut-shaped ring between Mars and Jupiter.
(NEAR Home Page; more info from NSSDC;
more from John Hopkins
Univ.; Curriculum
materials; more from JPL)
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Mars
Global Surveyor is the first mission
of a new, decade-long program of robotic exploration of Mars,
called the Mars Exploration Program. This will be an aggressive
series of orbiters and landers to be launched every 26 months,
as Mars moves into alignment with Earth. The program will be affordable,
costing about $100 million per year; engaging to the public, providing
fresh new global and close-up images of Mars; and have high scientific
value obtained with the development of leading-edge space technologies.
Mars Global Surveyor will be a polar-orbiting spacecraft at Mars
designed to provide global maps of surface topography, distribution
of minerals and monitoring of global weather.
Launched with a Delta II expendable vehicle from Cape Canaveral,
Fla., on November 7 1996, the spacecraft in an elliptical orbit
around Mars. During the year, thruster firings and aerobraking
techniques will be used to reach the nearly circular mapping orbit
over the Martian polar caps. Aerobraking, a technique pioneered
by the Magellan mission, which uses the
forces of atmospheric drag to slow the spacecraft into its final
mapping orbit, will provide a means of minimizing the amount of
fuel required to reach the low Mars orbit. Mapping operations
are expected to begin in March 1999.
The spacecraft will circle Mars once every two hours, maintaining
a "sun synchronous" orbit that will put the sun at a standard
angle above the horizon in each image and allow the mid-afternoon
lighting to cast shadows in such a way that surface features will
stand out. The spacecraft will carry a portion of the Mars
Observer instrument payload and will use these instruments
to acquire data of Mars for a full Martian year, the equivalent
of about two Earth years. The spacecraft will then be used as
a data relay station for signals from U.S. and international landers
and low-altitude probes for an additional three years.
International participation, collaboration and coordination will
enhance all missions of the program. Landers in future years --
1998, 2001, 2003 and 2005 -- will capitalize on the experience
of the Mars Pathfinder lander mission launched in 1996. Small
orbiters launched in the 1998 and 2003 opportunities will carry
other instruments from the Mars Observer payload and will serve
as data relay stations for international missions of the future.
The Mars Global Surveyor spacecraft will be acquired from industry
through a competitive procurement. The science payload will be
provided as government-furnished equipment that was built to duplicate
the instruments flown on Mars Observer. The payload includes the
Mars orbital camera, thermal emission spectrometer, ultra-stable
oscillator, laser altimeter, magnetometer/electron reflectometer
and Mars relay system.
The Jet Propulsion Laboratory will manage the project for NASA's
Solar System Exploration Division and will provide the mission
design, navigation, and conduct mission operations. Tracking and
data acquisition will be provided by a 34-meter subnetwork of
the worldwide Deep Space Network.
Project costs for the Mars Global Surveyor through 30 days after
launch will be approximately $155 million.
(MGS Home
Page from JPL; Planned Missions
from 1996 to 2003)
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The Mars Pathfinder (formerly known as the Mars
Environmental Survey, or MESUR, Pathfinder) is the second of NASA's
low-cost planetary Discovery missions. The mission consists of
a stationary lander and a surface rover known as Sojourner. The
mission has the primary objective of demonstrating the feasibility
of low-cost landings on and exploration of the Martian surface.
This objective will be met by tests of communications between
the rover and lander, and the lander and Earth, and tests of the
imaging devices and sensors.
The scientific objectives include atmospheric entry science, long-range
and close-up surface imaging, with the general objective being
to characterize the Martian environment for further exploration.
The spacecraft will enter the Martian atmosphere without going
into orbit around the planet and land on Mars with the aid of
parachutes, rockets and airbags, taking atmospheric measurements
on the way down. Prior to landing, the spacecraft will be enclosed
by three triangular solar panels (petals), which will unfold onto
the ground after touchdown.
Mars Pathfinder was launched 1996 December 4 and landed successfully
on Mars on 1997 July 4.
(info and MPF
Home Page from JPL; more
info from NSSDC; images
and press releases from MSFC; Mars
Watch, Linking Amateur and Professional Mars Observing Communities
for Observational Support of the Mars Pathfinder Mission)
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Saturn
orbiter and Titan atmosphere probe. Cassini
is a joint NASA/ESA project designed to accomplish an exploration
of the Saturnian system with its Cassini Saturn Orbiter and Huygens
Titan Probe. Cassini was launched aboard a Titan IV/Centaur 1997
Oct 15. En route to Saturn, Cassini will first execute two gravity
assist flybys of Venus, then one of Earth, and then one of Jupiter
(a "VVEJGA" trajectory). It will arrive at Saturn on 2004 July
1. Upon arrival, the Cassini spacecraft performs several maneuvers
to achieve an orbit around Saturn. Near the end of this initial
orbit, the Huygens Probe separates from the Orbiter and descends
through the atmosphere of Titan. The Orbiter relays the Probe
data to Earth for about 3 hours while the Probe enters and traverses
the cloudy atmosphere to the surface. After the completion of
the Probe mission, the Orbiter continues touring the Saturnian
system for three and a half years. Titan synchronous orbit trajectories
will allow about 35 flybys of Titan and targeted flybys of Iapetus,
Dione and Enceladus.
The objectives of the mission are threefold: conduct detailed
studies of Saturn's atmosphere, rings and magnetosphere; conduct
close-up studies of Saturn's satellites, and characterize Titan's
atmosphere and surface.
An earlier plan for an asteroid fly-by on the way out similar
to the highly successful Galileo fly-bys
of Ida and Gaspra
was scrapped in order to reduce costs.
One of the most intriguing aspects of Titan
is the possibility that its surface may be covered in part with
lakes of liquid hydrocarbons that result from photochemical processes
in its upper atmosphere. These hydrocarbons condense to form a
global smog layer and eventually rain down onto the surface. The
Cassini orbiter will use onboard radar to peer through Titan's
clouds and determine if there is liquid on the surface. Experiments
aboard both the orbiter and the entry probe will investigate the
chemical processes that produce this unique atmosphere.
Key Scheduled Dates for the Cassini Mission (VVEJGA Trajectory) -- 10/15/97 --
Titan IV/Centaur Launch 04/26/98 - Venus 1 Gravity Assist 06/24/99 - Venus 2 Gravity
Assist 08/18/99 - Earth Gravity Assist 12/30/00 - Jupiter Gravity Assist 07/01/04
- Saturn Arrival 11/06/04 - Probe Separation 11/27/04 - Titan Probe Entry 06/25/08
- End of Primary Mission
(Cassini Home Page
from JPL; Huygens
Home Page; another Cassini
page from JPL; more
info from JPL;
from NASA Spacelink; info on the Doppler
Wind Experiment on Huygens)
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Lunar
Prospector, the first NASA mission to the Moon in almost 30 years,
was launched Jan 6th, 1998. Within a month it will begin returning
answers to long-standing questions about the Moon, its resources,
its structure and its origins. (Welcome
to the Moon, Lunar Prospector home page); more
from NSSDC
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The Mars Surveyor '98 program is the next generation
of spacecraft to be sent to Mars. Consisting of an orbiter--to
be launched Dec. 10, 1998, and lander, set for launch on Jan.
3, 1999--the Mars '98 mission will add to the knowledge gained
by the Global Surveyor and Pathfinder missions. The general science
theme for the 1998 Surveyor missions is "Volatiles and Climate
History."
The Mars '98 orbiter will arrive at Mars Sept. 23, 1999, while
the lander will touch down Dec. 3, 1999.
The lander will land near the southern polar cap and is equipped
with cameras, a robotics arm and instruments to measure the composition
of the Martian soil. Two small microprobes are also piggybacking
on the lander, which will penetrate into the Martian subsurface
to detect water ice.
The science package for the lander includes the Mars Volatile
and Climate Surveyor (MVACS) integrated lander payload, the Mars
Descent Imager (MARDI) and an atmospheric lidar experiment provided
by the Russian Space Agency Institute for Space Science. The integrated
lander payload includes a surface stereo imager with Mars Pathfinder
heritage; a meteorology package; an instrumented robotic arm for
sample acquisition, soil manipulation and closeup imaging of the
surface and subsurface; and the thermal and evolved gas analysis
experiment for determining the nature and abundance of volatile
material in the Martian soil.
The images obtained while the lander descends to the surface will
establish the geological and physical context of the landing site.
The atmospheric lidar experiment will determine the dust content
of the Martian atmosphere above the landing site.
(home page)
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Scheduled for launch in February 1999, Stardust
will fly close to a comet and, for the first time ever, bring
material from the comets coma back to Earth for analysis by scientists
worldwide. Scheduled to fly-by Comet Wild-2 in 2004, return to
Earth in 2006.
(home page)
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As part of NASA's Ice and Fire Preprojects, planning
has begun on a mission to send a spacecraft to Europa to measure
the thickness of the surface ice and to detect an underlying liquid
ocean if it exists. Using an instrument called a radar sounder
to bounce radio waves through the ice, the Europa Orbiter sciencecraft
would be able to detect an ice-water interface, perhaps as little
as 1 km below the surface. Other instruments would reveal details
of the surface and interior processes. This mission would be a
precursor mission to sending "hydrobots" or remote controlled
submarines that could melt through the ice and explore the undersea
realm.
(home page;
see also Europa Ocean Explorer)
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Pluto-Kuiper
Express
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(was Pluto Express and before that Pluto Fast Fly-by) a small,
fast, relatively cheap initial look at the as yet unvisited Pluto.
Possible launch in 2001 (if a 1998 new start is authorized). Calls
for launch of two spacecraft weighing less than 100 kg using Titan
IV/Centaur or Proton (possibly with additional solid kick stages)
in 2001 and encounters with Pluto and Charon
around 2006-8 (depending on trajectory choice). Flybys would be
at 12-18 km/second; data would be recorded onboard the probes
during the short encounters and returned to Earth slowly (due
to low power, small antenna sizes, and large distances) over the
next year or so. Russian "Drop Zond" probes to sample the atmosphere
may be included as well.
Science objectives include characterizing global
geology and geomorphology of Pluto and Charon, mapping both sides
of each body, and characterizing Pluto's atmosphere (the atmosphere
is freezing out as Pluto moves away from the Sun, so launching
early and minimizing flight time is critical for this objective).
The 7 kilogram instrument package might include a CCD imaging
camera, IR mapping spectrometer, UV spectrometer, and radio science
occultation experiments.
The PFF spacecraft would be highly a miniaturized descendant of
the present class of outer solar system platforms, breaking the
trend of increasingly complex and expensive probes such as Galileo
and Cassini.
There's an article about PFF by its designers in the Sep/Oct 1994
issue of The Planetary Report, the bimonthly newsletter from The
Planetary Society.
Funding for this project is very much in doubt.
(more
info from NASA; Pluto
Express home page; Pluto
Express Science)
-
Muses-C
The Japanese-managed Muses-C mission will collect and return to
Earth a sample from an asteroid.
This innovative mission will use new flight technology, including
solar electric propulsion, to send a spacecraft to asteroid 4660
Nereus and deliver a JPL-developed rover, which measures about
the size of a shoebox, to the asteroid's surface. The Muses-C
spacecraft will also fire explosive charges into the asteroid,
collect the samples that are ejected from the impacts, and return
the samples to Earth in a capsule for laboratory analysis. The
mission is scheduled for launch in 2002.
(All missions not otherwise labeled
are NASA)
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