Cassini–Huygens
ESA / ASI | |
COSPAR ID | 1997-061A |
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SATCAT no. | 25008 |
Website | |
Mission duration |
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Spacecraft properties | |
Manufacturer | Cassini: Jet Propulsion Laboratory Huygens: Thales Alenia Space (then Aerospatiale)[1] |
Launch mass | 5,712 kg (12,593 lb)[2][3] |
Dry mass | 2,523 kg (5,562 lb)[2] |
Power | ~885 watts (BOL)[2] ~670 watts (2010)[4] ~663 watts (EOM/2017)[2] |
Start of mission | |
Launch date | October 15, 1997, 08:43:00 | UTC
Rocket | SLC-40 |
End of mission | |
Disposal | Controlled entry into Saturn[5][6] |
Last contact | September 15, 2017
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Orbital parameters | |
Reference system | Kronocentric |
Flyby of Venus (Gravity assist) | |
Closest approach | April 26, 1998 |
Distance | 283 km (176 mi) |
Flyby of Venus (Gravity assist) | |
Closest approach | June 24, 1999 |
Distance | 623 km (387 mi) |
Flyby of Earth-Moon system (Gravity assist) | |
Closest approach | August 18, 1999, 03:28 UTC |
Distance | 1,171 km (728 mi) |
Flyby of 2685 Masursky (Incidental) | |
Closest approach | January 23, 2000 |
Distance | 1,600,000 km (990,000 mi) |
Flyby of Jupiter (Gravity assist) | |
Closest approach | December 30, 2000 |
Distance | 9,852,924 km (6,122,323 mi) |
Saturn orbiter | |
Orbital insertion | July 1, 2004, 02:48 UTC |
Titan lander | |
Spacecraft component | Huygens |
Landing date | January 14, 2005 |
Large Strategic Science Missions → |
Cassini–Huygens (
Launched aboard a Titan IVB/Centaur on October 15, 1997, Cassini was active in space for nearly 20 years, with 13 years spent orbiting Saturn and studying the planet and its system after entering orbit on July 1, 2004.[9]
The voyage to Saturn included flybys of Venus (April 1998 and July 1999), Earth (August 1999), the asteroid 2685 Masursky, and Jupiter (December 2000). The mission ended on September 15, 2017, when Cassini's trajectory took it into Saturn's upper atmosphere and it burned up[10][11] in order to prevent any risk of contaminating Saturn's moons, which might have offered habitable environments to stowaway terrestrial microbes on the spacecraft.[12][13] The mission was successful beyond expectations – NASA's Planetary Science Division Director, Jim Green, described Cassini-Huygens as a "mission of firsts"[14] that has revolutionized human understanding of the Saturn system, including its moons and rings, and our understanding of where life might be found in the Solar System.[15]
Cassini's planners originally scheduled a mission of four years, from June 2004 to May 2008. The mission was extended for another two years until September 2010, branded the Cassini Equinox Mission. The mission was extended a second and final time with the Cassini Solstice Mission, lasting another seven years until September 15, 2017, on which date Cassini was de-orbited to burn up in Saturn's upper atmosphere.[16]
The Huygens module traveled with Cassini until its separation from the probe on December 25, 2004; Huygens landed by parachute on Titan on January 14, 2005. The separation was facilitated by the SED (Spin/Eject device), which provided a relative separation speed of 0.35 metres per second (1.1 ft/s) and a spin rate of 7.5 rpm.[17] It returned data to Earth for around 90 minutes, using the orbiter as a relay. This was the first landing ever accomplished in the outer Solar System and the first landing on a moon other than Earth's Moon.
At the end of its mission, the Cassini spacecraft executed its "Grand Finale": a number of risky passes through the gaps between Saturn and its inner rings.[5][6] This phase aimed to maximize Cassini's scientific outcome before the spacecraft was intentionally destroyed[18] to prevent potential contamination of Saturn's moons if Cassini were to unintentionally crash into them when maneuvering the probe was no longer possible due to power loss or other communication issues at the end of its operational lifespan. The atmospheric entry of Cassini ended the mission, but analysis of the returned data will continue for many years.[15]
Overview
Scientists and individuals from 27 countries made up the joint team responsible for designing, building, flying and collecting data from the Cassini orbiter and the Huygens probe.[19]
NASA's Jet Propulsion Laboratory in the United States, where the orbiter was assembled, managed the mission. The European Space Research and Technology Centre developed Huygens. The centre's prime contractor, Aérospatiale of France (part of Thales Alenia Space from 2005), assembled the probe with equipment and instruments supplied by many European countries (including Huygens' batteries and two scientific instruments from the United States). The Italian Space Agency (ASI) provided the Cassini orbiter's high-gain radio antenna, with the incorporation of a low-gain antenna (to ensure telecommunications with the Earth for the entire duration of the mission), a compact and lightweight radar, which also used the high-gain antenna and served as a synthetic-aperture radar, a radar altimeter, a radiometer, the radio science subsystem (RSS), and the visible-channel portion VIMS-V of VIMS spectrometer.[20]
NASA provided the VIMS infrared counterpart, as well as the Main Electronic Assembly, which included electronic sub-assemblies provided by CNES of France.[21][22]
On April 16, 2008, NASA announced a two-year extension of the funding for ground operations of this mission, at which point it was renamed the Cassini Equinox Mission.[23]
The round of funding was again extended[
Naming
The mission consisted of two main elements: the ASI/NASA Cassini orbiter, named for the Italian astronomer Giovanni Domenico Cassini, discoverer of Saturn's ring divisions and four of its satellites; and the ESA-developed Huygens probe, named for the Dutch astronomer, mathematician and physicist Christiaan Huygens, discoverer of Titan.
The mission was commonly called Saturn Orbiter Titan Probe (SOTP) during gestation, both as a Mariner Mark II mission and generically.[24]
Cassini-Huygens was a
Objectives
Cassini had several objectives, including:[25]
- Determining the three-dimensional structure and dynamic behavior of the rings of Saturn.
- Determining the composition of the satellite surfaces and the geological history of each object.
- Determining the nature and origin of the dark material on Iapetus's leading hemisphere.
- Measuring the three-dimensional structure and dynamic behavior of the magnetosphere.
- Studying the dynamic behavior of Saturn's atmosphere at cloud level.
- Studying the time variability of Titan's clouds and hazes.
- Characterizing Titan's surface on a regional scale.
Cassini–Huygens was launched on October 15, 1997, from
The total cost of this scientific exploration mission was about US$3.26
The primary mission for Cassini was completed on July 30, 2008. The mission was extended to June 2010 (Cassini Equinox Mission).[28] This studied the Saturn system in detail during the planet's equinox, which happened in August 2009.[23]
On February 3, 2010, NASA announced another extension for Cassini, lasting 61⁄2 years until 2017, ending at the time of summer solstice in Saturn's northern hemisphere (Cassini Solstice Mission). The extension enabled another 155 revolutions around the planet, 54 flybys of Titan and 11 flybys of Enceladus.[29] In 2017, an encounter with Titan changed its orbit in such a way that, at closest approach to Saturn, it was only 3,000 km (1,900 mi) above the planet's cloudtops, below the inner edge of the D ring. This sequence of "proximal orbits" ended when its final encounter with Titan sent the probe into Saturn's atmosphere to be destroyed.
Itinerary
Selected destinations (ordered largest to smallest but not to scale) | ||||||
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Titan | Earth's Moon | Rhea | Iapetus | Dione | Tethys | Enceladus |
Mimas | Hyperion | Phoebe | Janus | Epimetheus | Prometheus | Pandora |
Helene | Atlas | Pan | Telesto | Calypso | Methone |
History
Cassini–Huygens's origins date to 1982, when the European Science Foundation and the American National Academy of Sciences formed a working group to investigate future cooperative missions. Two European scientists suggested a paired Saturn Orbiter and Titan Probe as a possible joint mission. In 1983, NASA's Solar System Exploration Committee recommended the same Orbiter and Probe pair as a core NASA project. NASA and the European Space Agency (ESA) performed a joint study of the potential mission from 1984 to 1985. ESA continued with its own study in 1986, while the American astronaut Sally Ride, in her influential 1987 report NASA Leadership and America's Future in Space, also examined and approved of the Cassini mission.[30]
While Ride's report described the Saturn orbiter and probe as a NASA solo mission, in 1988 the Associate Administrator for Space Science and Applications of NASA, Len Fisk, returned to the idea of a joint NASA and ESA mission. He wrote to his counterpart at ESA, Roger Bonnet, strongly suggesting that ESA choose the Cassini mission from the three candidates at hand and promising that NASA would commit to the mission as soon as ESA did.[31]
At the time, NASA was becoming more sensitive to the strain that had developed between the American and European space programs as a result of European perceptions that NASA had not treated it like an equal during previous collaborations. NASA officials and advisers involved in promoting and planning Cassini–Huygens attempted to correct this trend by stressing their desire to evenly share any scientific and technology benefits resulting from the mission. In part, this newfound spirit of cooperation with Europe was driven by a sense of competition with the Soviet Union, which had begun to cooperate more closely with Europe as ESA drew further away from NASA. Late in 1988, ESA chose Cassini–Huygens as its next major mission and the following year the program received major funding in the US.[32][33]
The collaboration not only improved relations between the two space programs but also helped Cassini–Huygens survive congressional budget cuts in the United States. Cassini–Huygens came under fire politically in both 1992 and 1994, but NASA successfully persuaded the United States Congress that it would be unwise to halt the project after ESA had already poured funds into development because frustration on broken space exploration promises might spill over into other areas of foreign relations. The project proceeded politically smoothly after 1994, although citizens' groups concerned about the potential environmental impact a launch failure might have (because of its plutonium power source) attempted to derail it through protests and lawsuits until and past its 1997 launch.[34][35][36][37][38]
Spacecraft design
The spacecraft was planned to be the second three-axis stabilized, RTG-powered Mariner Mark II, a class of spacecraft developed for missions beyond the orbit of Mars, after the Comet Rendezvous Asteroid Flyby (CRAF) mission, but budget cuts and project rescopings forced NASA to terminate CRAF development to save Cassini. As a result, Cassini became more specialized. The Mariner Mark II series was cancelled.
The combined orbiter and probe is the third-largest uncrewed interplanetary spacecraft ever successfully launched, behind the Phobos 1 and 2 Mars probes, as well as being among the most complex.[39][40] The orbiter had a mass of 2,150 kg (4,740 lb), the probe 350 kg (770 lb) including 30 kg (66 lb) of probe support equipment left on the orbiter. With the launch vehicle adapter and 3,132 kg (6,905 lb) of propellants at launch, the spacecraft had a mass of 5,600 kg (12,300 lb).
The Cassini spacecraft was 6.8 meters (22 ft) high and 4 meters (13 ft) wide. Spacecraft complexity was increased by its
Cassini was powered by 32.7 kg (72 lb) of nuclear fuel, mainly
The heat from the material's radioactive decay was turned into electricity. Huygens was supported by Cassini during cruise, but used chemical batteries when independent.The probe contained a DVD with more than 616,400 signatures from citizens in 81 countries, collected in a public campaign.[44][45]
Until September 2017 the Cassini probe continued orbiting Saturn at a distance of between 8.2 and 10.2 astronomical units (1.23×109 and 1.53×109 km; 760,000,000 and 950,000,000 mi) from the Earth. It took 68 to 84 minutes for radio signals to travel from Earth to the spacecraft, and vice versa. Thus ground controllers could not give "real-time" instructions for daily operations or for unexpected events. Even if response were immediate, more than two hours would have passed between the occurrence of a problem and the reception of the engineers' response by the satellite.
Instruments
Summary
Instruments:[47]
- Optical Remote Sensing ("Located on the remote sensing pallet")[47]
- Composite Infrared Spectrometer (CIRS)
- Imaging Science Subsystem (ISS)
- Ultraviolet Imaging Spectrograph (UVIS)
- Visible and Infrared Mapping Spectrometer (VIMS)
- Fields, Particles and Waves (mostly in situ)
- Cassini Plasma Spectrometer (CAPS)
- Cosmic Dust Analyzer (CDA)
- Ion and Neutral Mass Spectrometer (INMS)
- Magnetometer (MAG)
- Magnetospheric Imaging Instrument (MIMI)
- Radio and Plasma Wave Science (RPWS)
- Microwave Remote Sensing
- Radar
- Radio Science (RSS)
Description
Cassini's instrumentation consisted of: a
- Cassini Plasma Spectrometer (CAPS)
- CAPS was an in situ instrument that measured the flux of charged particles at the location of the spacecraft, as a function of direction and energy. The ion composition was also measured using a time-of-flight mass spectrometer. CAPS measured particles produced by ionisation of molecules originating from Saturn's and Titan's ionosphere, as well as the plumes of Enceladus. CAPS also investigated plasma in these areas, along with the solar wind and its interaction with Saturn's magnetosphere.[48][49] CAPS was turned off in June 2011, as a precaution due to a "soft" electrical short circuit that occurred in the instrument. It was powered on again in March 2012, but after 78 days another short circuit forced the instrument to be shut down permanently.[50]
- Cosmic Dust Analyzer (CDA)
- The CDA was an in situ instrument that measured the size, speed, and direction of tiny dust grains near Saturn. It could also measure the grains' chemical elements.[51] Some of these particles orbited Saturn, while others came from other star systems. The CDA on the orbiter was designed to learn more about these particles, the materials in other celestial bodies and potentially about the origins of the universe.[48]
- Composite Infrared Spectrometer (CIRS)
- The CIRS was a remote sensing instrument that measured the aerosols and clouds. It also measured thermal characteristics and the composition of satellite surfaces and rings.[48]
- Ion and Neutral Mass Spectrometer (INMS)
- The INMS was an in situ instrument that measured the composition of charged particles (protons and heavier ions) and neutral particles (atoms and molecules) near Titan and Saturn to learn more about their atmospheres. The instrument used a
- Imaging Science Subsystem (ISS)
- The ISS was a remote sensing instrument that captured most images in
- Dual Technique Magnetometer (MAG)
- The MAG was an in situ instrument that measured the strength and direction of the magnetic field around Saturn. The magnetic fields are generated partly by the molten core at Saturn's center. Measuring the magnetic field is one of the ways to probe the core. MAG aimed to develop a three-dimensional model of Saturn's magnetosphere, and determine the magnetic state of Titan and its atmosphere, and the icy satellites and their role in the magnetosphere of Saturn.[48][55]
- Magnetospheric Imaging Instrument (MIMI)
- The MIMI was both an in situ and remote sensing instrument that produces images and other data about the particles trapped in Saturn's huge magnetic field, or magnetosphere. The in situ component measured energetic ions and electrons while the remote sensing component (the Ion And Neutral Camera, INCA) was an energetic neutral atom imager.[56] This information was used to study the overall configuration and dynamics of the magnetosphere and its interactions with the solar wind, Saturn's atmosphere, Titan, rings, and icy satellites.[48][57]
- Radar
- The on-board radar was an active and passive sensing instrument that produced maps of Titan's surface. Radar waves were powerful enough to penetrate the thick veil of haze surrounding Titan. By measuring the send and return time of the signals it is possible to determine the height of large surface features, such as mountains and canyons. The passive radar listened for radio waves that Saturn or its moons may emit.[48]
- Radio and Plasma Wave Science instrument (RPWS)
- The RPWS was an in situ instrument and remote sensing instrument that receives and measures radio signals coming from Saturn, including the radio waves given off by the interaction of the solar wind with Saturn and Titan. RPWS measured the electric and magnetic wave fields in the interplanetary medium and planetary magnetospheres. It also determined the electron density and temperature near Titan and in some regions of Saturn's magnetosphere using either plasma waves at characteristic frequencies (e.g. the upper hybrid line) or a Langmuir probe. RPWS studied the configuration of Saturn's magnetic field and its relationship to Saturn Kilometric Radiation (SKR), as well as monitoring and mapping Saturn's ionosphere, plasma, and lightning from Saturn's (and possibly Titan's) atmosphere.[48]
- Radio Science Subsystem(RSS)
- The RSS was a remote-sensing instrument that used radio antennas on Earth to observe the way radio signals from the spacecraft changed as they were sent through objects, such as Titan's atmosphere or Saturn's rings, or even behind the Sun. The RSS also studied the compositions, pressures and temperatures of atmospheres and ionospheres, radial structure and particle size distribution within rings, body and system masses and the gravitational field. The instrument used the spacecraft X-band communication link as well as S-band downlink and Ka-band uplink and downlink.[48]
- Ultraviolet Imaging Spectrograph (UVIS)
- The UVIS was a remote-sensing instrument that captured images of the ultraviolet light reflected off an object, such as the clouds of Saturn and/or its rings, to learn more about their structure and composition. Designed to measure ultraviolet light over wavelengths from 55.8 to 190 nm, this instrument was also a tool to help determine the composition, distribution, aerosol particle content and temperatures of their atmospheres. Unlike other types of spectrometer, this sensitive instrument could take both spectral and spatial readings. It was particularly adept at determining the composition of gases. Spatial observations took a wide-by-narrow view, only one pixel tall and 64 pixels across. The spectral dimension was 1,024 pixels per spatial pixel. It could also take many images that create movies of the ways in which this material is moved around by other forces.[48]
UVIS consisted of four separate detector channels, the Far Ultraviolet (FUV), Extreme Ultraviolet (EUV), High Speed Photometer (HSP) and the Hydrogen-Deuterium Absorption Cell (HDAC). UVIS collected hyperspectral imagery and discrete spectra of Saturn, its moons and its rings, as well as stellar occultation data.[58]
The HSP channel is designed to observe starlight that passes through Saturn's rings (known as stellar occultations) in order to understand the structure and optical depth of the rings.[59] Stellar occultation data from both the HSP and FUV channels confirmed the existence of water vapor plumes at the south pole of Enceladus, as well as characterized the composition of the plumes.[60]
- Visible and Infrared Mapping Spectrometer (VIMS)
- The VIMS was a remote sensing instrument that captured images using visible and infrared light to learn more about the composition of moon surfaces, the rings, and the atmospheres of Saturn and Titan. It consisted of two cameras - one used to measure visible light, the other infrared. VIMS measured reflected and emitted radiation from atmospheres, rings and surfaces over wavelengths from 350 to 5100 nm, to help determine their compositions, temperatures and structures. It also observed the sunlight and starlight that passes through the rings to learn more about their structure. Scientists used VIMS for long-term studies of cloud movement and morphology in the Saturn system, to determine Saturn's weather patterns.[48]
Plutonium power source
Because of Saturn's distance from the Sun,
To gain
NASA's risk analysis to use plutonium was publicly criticized by Michio Kaku on the grounds that casualties, property damage, and lawsuits resulting from a possible accident, as well as the potential use of other energy sources, such as solar and fuel cells, were underestimated.[67]
Telemetry
The Cassini spacecraft was capable of transmitting in several different telemetry formats. The telemetry subsystem is perhaps the most important subsystem, because without it there could be no data return.
The telemetry was developed from the ground up, due to the spacecraft using a more modern set of computers than previous missions.[68] Therefore, Cassini was the first spacecraft to adopt mini-packets to reduce the complexity of the Telemetry Dictionary, and the software development process led to the creation of a Telemetry Manager for the mission.
There were around 1088 channels (in 67 mini-packets) assembled in the Cassini Telemetry Dictionary. Out of these 67 lower complexity mini-packets, 6 mini-packets contained the subsystem covariance and Kalman gain elements (161 measurements), not used during normal mission operations. This left 947 measurements in 61 mini-packets.
A total of seven telemetry maps corresponding to 7 AACS telemetry modes were constructed. These modes are: (1) Record; (2) Nominal Cruise; (3) Medium Slow Cruise; (4) Slow Cruise; (5) Orbital Ops; (6) Av; (7) ATE (Attitude Estimator) Calibration. These 7 maps cover all spacecraft telemetry modes.
Huygens probe
The Huygens probe, supplied by the European Space Agency (ESA) and named after the 17th century Dutch astronomer who first discovered Titan, Christiaan Huygens, scrutinized the clouds, atmosphere, and surface of Saturn's moon Titan in its descent on January 15, 2005. It was designed to enter and brake in Titan's atmosphere and parachute a fully instrumented robotic laboratory down to the surface.[69]
The probe system consisted of the probe itself which descended to Titan, and the probe support equipment (PSE) which remained attached to the orbiting spacecraft. The PSE includes electronics that track the probe, recover the data gathered during its descent, and process and deliver the data to the orbiter that transmits it to Earth. The core control computer CPU was a redundant MIL-STD-1750A control system.
The data were transmitted by a radio link between Huygens and Cassini provided by Probe Data Relay Subsystem (PDRS). As the probe's mission could not be telecommanded from Earth because of the great distance, it was automatically managed by the Command Data Management Subsystem (CDMS). The PDRS and CDMS were provided by the Italian Space Agency (ASI).
After Cassini's launch, it was discovered that data sent from the Huygens probe to Cassini orbiter (and then re-transmitted to Earth) would be largely unreadable. The cause was that the
A work-around was found to recover the mission. The trajectory of Cassini was altered to reduce the line of sight velocity and therefore the doppler shift.[18][70] Cassini's subsequent trajectory was identical to the previously planned one, although the change replaced two orbits prior to the Huygens mission with three, shorter orbits.
Selected events and discoveries
Venus and Earth fly-bys and the cruise to Jupiter
The Cassini space probe performed two gravitational-assist flybys of Venus on April 26, 1998, and June 24, 1999. These flybys provided the space probe with enough momentum to travel all the way out to the asteroid belt, while the Sun's gravity pulled the space probe back into the inner Solar System.
On August 18, 1999, at 03:28 UTC, the craft made a gravitational-assist flyby of the Earth. One hour and 20 minutes before closest approach, Cassini made its closest approach to the Earth's Moon at 377,000 kilometers, and it took a series of calibration photos.
On January 23, 2000, Cassini performed a flyby of the asteroid 2685 Masursky at around 10:00 UTC. It took photos[71] in the period five to seven hours before the flyby at a distance of 1.6×10 6 km (0.99×10 6 mi) and a diameter of 15 to 20 km (9.3 to 12.4 mi) was estimated for the asteroid.
Jupiter flyby
This section needs additional citations for verification. (October 2018) |
Cassini made its closest approach to Jupiter on December 30, 2000, at 9.7 million kilometers, and made many scientific measurements. About 26,000 images of Jupiter, its
A major finding of the flyby, announced on March 6, 2003, was of Jupiter's atmospheric circulation. Dark "belts" alternate with light "zones" in the atmosphere, and scientists had long considered the zones, with their pale clouds, to be areas of upwelling air, partly because many clouds on Earth form where air is rising. But analysis of Cassini imagery showed that individual storm cells of upwelling bright-white clouds, too small to see from Earth, pop up almost without exception in the dark belts. According to Anthony Del Genio of NASA's Goddard Institute for Space Studies, "the belts must be the areas of net-rising atmospheric motion on Jupiter, [so] the net motion in the zones has to be sinking".
Other atmospheric observations included a swirling dark oval of high atmospheric haze, about the size of the Great Red Spot, near Jupiter's north pole. Infrared imagery revealed aspects of circulation near the poles, with bands of globe-encircling winds, with adjacent bands moving in opposite directions.
The same announcement also discussed the nature of Jupiter's
Tests of general relativity
On October 10, 2003, the mission's science team announced the results of tests of
Although some measurable deviations from the values calculated using the
New moons of Saturn
In total, the Cassini mission discovered seven new moons orbiting Saturn.[76] Using images taken by Cassini, researchers discovered Methone, Pallene and Polydeuces in 2004,[77] although later analysis revealed that Voyager 2 had photographed Pallene in its 1981 flyby of the ringed planet.[78]
On May 1, 2005, a new moon was discovered by Cassini in the
On April 14, 2014, NASA scientists reported the possible beginning of a new moon in Saturn's
Phoebe flyby
On June 11, 2004, Cassini flew by the moon Phoebe. This was the first opportunity for close-up studies of this moon (Voyager 2 performed a distant flyby in 1981 but returned no detailed images). It also was Cassini's only possible flyby for Phoebe due to the mechanics of the available orbits around Saturn.[82]
The first close-up images were received on June 12, 2004, and mission scientists immediately realized that the surface of Phoebe looks different from asteroids visited by spacecraft. Parts of the heavily cratered surface look very bright in those pictures, and it is currently believed that a large amount of water ice exists under its immediate surface.
Saturn rotation
In an announcement on June 28, 2004, Cassini program scientists described the measurement of the rotational period of Saturn.[83] Because there are no fixed features on the surface that can be used to obtain this period, the repetition of radio emissions was used. This new data agreed with the latest values measured from Earth, and constituted a puzzle to the scientists. It turns out that the radio rotational period had changed since it was first measured in 1980 by Voyager 1, and it was now 6 minutes longer. This, however, does not indicate a change in the overall spin of the planet. It is thought to be due to variations in the upper atmosphere and ionosphere at the latitudes which are magnetically connected to the radio source region.
In 2019 NASA announced Saturn's rotational period as 10 hours, 33 minutes, 38 seconds, calculated using Saturnian ring seismology. Vibrations from Saturn's interior cause oscillations in its gravitational field. This energy is absorbed by ring particles in specific locations, where it accumulates until it is released in a wave.[84] Scientists used data from more than 20 of these waves to construct a family of models of Saturn's interior, providing basis for calculating its rotational period.[85]
Orbiting Saturn
On July 1, 2004, the spacecraft flew through the gap between the F and G rings and achieved orbit, after a seven-year voyage.[86] It was the first spacecraft to ever orbit Saturn.
The Saturn Orbital Insertion (SOI) maneuver performed by Cassini was complex, requiring the craft to orient its High-Gain Antenna away from Earth and along its flight path, to shield its instruments from particles in Saturn's rings. Once the craft crossed the ring plane, it had to rotate again to point its engine along its flight path, and then the engine fired to decelerate the craft by 622 m/s to allow Saturn to capture it.
When Cassini was in Saturnian orbit, departure from the Saturn system was evaluated in 2008 during end of mission planning.[88][clarification needed]
Titan flybys
Cassini had its first flyby of
Huygens lands on Titan
External image | |
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Raw images from the Huygens probe descent on 14 January 2005 (37 pages) ESA/NASA/JPL/University of Arizona (ESA hosting) |
Cassini released the Huygens probe on December 25, 2004, by means of a spring and spiral rails intended to rotate the probe for greater stability. It entered the atmosphere of Titan on January 14, 2005, and after a two-and-a-half-hour descent landed on solid ground.[6] Although Cassini successfully relayed 350 of the pictures that it received from Huygens of its descent and landing site, a software error failed to turn on one of the Cassini receivers and caused the loss of another 350 pictures. While landing, for caution, NASA loaded Huygens with 3 parachutes.[89]
Enceladus flybys
During the first two close flybys of the moon Enceladus in 2005, Cassini discovered a deflection in the local magnetic field that is characteristic for the existence of a thin but significant atmosphere. Other measurements obtained at that time point to ionized water vapor as its main constituent. Cassini also observed water ice geysers erupting from the south pole of Enceladus, which gives more credibility to the idea that Enceladus is supplying the particles of Saturn's E ring. Mission scientists began to suspect that there may be pockets of liquid water near the surface of the moon that fuel the eruptions.[90]
On March 12, 2008, Cassini made a close fly-by of Enceladus, passing within 50 km of the moon's surface.[91] The spacecraft passed through the plumes extending from its southern geysers, detecting water, carbon dioxide and various hydrocarbons with its mass spectrometer, while also mapping surface features that are at much higher temperature than their surroundings with the infrared spectrometer.[92] Cassini was unable to collect data with its cosmic dust analyzer due to an unknown software malfunction.
On November 21, 2009, Cassini made its eighth flyby of Enceladus,[93] this time with a different geometry, approaching within 1,600 km (990 mi) of the surface. The Composite Infrared Spectrograph (CIRS) instrument produced a map of thermal emissions from the Baghdad Sulcus 'tiger stripe'. The data returned helped create a detailed and high resolution mosaic image of the southern part of the moon's Saturn-facing hemisphere.
On April 3, 2014, nearly ten years after Cassini entered Saturn's orbit, NASA reported evidence of a large salty internal ocean of liquid water in Enceladus. The presence of an internal salty ocean in contact with the moon's rocky core, places Enceladus "among the most likely places in the Solar System to host alien microbial life".[94][95][96] On June 30, 2014, NASA celebrated ten years of Cassini exploring Saturn and its moons, highlighting the discovery of water activity on Enceladus among other findings.[97]
In September 2015, NASA announced that gravitational and imaging data from Cassini were used to analyze the librations of Enceladus' orbit and determined that the moon's surface is not rigidly joined to its core, concluding that the underground ocean must therefore be global in extent.[98]
On October 28, 2015, Cassini performed a close flyby of Enceladus, coming within 49 km (30 mi) of the surface, and passing through the
On December 14, 2023, astronomers reported the first time discovery, in the
Radio occultations of Saturn's rings
In May 2005, Cassini began a series of
Spokes in rings verified
In images captured September 5, 2005, Cassini detected spokes in Saturn's rings,[102] previously seen only by the visual observer Stephen James O'Meara in 1977 and then confirmed by the Voyager space probes in the early 1980s.[103][104]
Lakes of Titan
Radar images obtained on July 21, 2006, appear to show lakes of
On March 13, 2007, the Jet Propulsion Laboratory announced that it had found strong evidence of seas of methane and ethane in the northern hemisphere of Titan. At least one of these is larger than any of the Great Lakes in North America.[106]
Saturn hurricane
In November 2006, scientists discovered a storm at the south pole of Saturn with a distinct
Iapetus flyby
On September 10, 2007, Cassini completed its flyby of the strange, two-toned, walnut-shaped moon,
Mission extension
On April 15, 2008, Cassini received funding for a 27-month extended mission. It consisted of 60 more orbits of Saturn, with 21 more close Titan flybys, seven of Enceladus, six of Mimas, eight of Tethys, and one targeted flyby each of Dione, Rhea, and Helene.[109] The extended mission began on July 1, 2008, and was renamed the Cassini Equinox Mission as the mission coincided with Saturn's equinox.[110]
Second mission extension
A proposal was submitted to NASA for a second mission extension (September 2010 – May 2017), provisionally named the extended-extended mission or XXM.[111] This ($60M pa) was approved in February 2010 and renamed the Cassini Solstice Mission.[112] It included Cassini orbiting Saturn 155 more times, conducting 54 additional flybys of Titan and 11 more of Enceladus.
Great Storm of 2010 and aftermath
On October 25, 2012, Cassini witnessed the aftermath of the massive Great White Spot storm that recurs roughly every 30 years on Saturn.[113] Data from the composite infrared spectrometer (CIRS) instrument indicated a powerful discharge from the storm that caused a temperature spike in the stratosphere of Saturn 83 K (83 °C; 149 °F) above normal. Simultaneously, a huge increase in ethylene gas was detected by NASA researchers at Goddard Research Center in Greenbelt, Maryland. Ethylene is a colorless gas that is highly uncommon on Saturn and is produced both naturally and through man-made sources on Earth. The storm that produced this discharge was first observed by the spacecraft on December 5, 2010, in Saturn's northern hemisphere. The storm is the first of its kind to be observed by a spacecraft in orbit around Saturn as well as the first to be observed at thermal infrared wavelengths, allowing scientists to observe the temperature of Saturn's atmosphere and track phenomena that are invisible to the naked eye. The spike of ethylene gas that was produced by the storm reached levels that were 100 times more than those thought possible for Saturn. Scientists have also determined that the storm witnessed was the largest, hottest stratospheric vortex ever detected in the Solar System, initially being larger than Jupiter's Great Red Spot.
Venus transit
On December 21, 2012, Cassini observed a transit of Venus across the Sun.[114] The VIMS instrument analyzed sunlight passing through the Venusian atmosphere.[114] VIMS previously observed the transit of exoplanet HD 189733 b.[114]
The Day the Earth Smiled
On July 19, 2013, the probe was pointed towards Earth to capture an image of the Earth and the Moon, as part of a natural light, multi-image portrait of the entire Saturn system. The event was unique as it was the first time NASA informed the public that a long-distance photo was being taken in advance.[115][116] The imaging team said they wanted people to smile and wave to the skies, with Cassini scientist Carolyn Porco describing the moment as a chance to "celebrate life on the Pale Blue Dot".[117]
Rhea flyby
On February 10, 2015, the Cassini spacecraft visited Rhea more closely, coming within 47,000 km (29,000 mi).[118] The spacecraft observed the moon with its cameras producing some of the highest resolution color images yet of Rhea.[119]
Hyperion flyby
Cassini performed its latest flyby of Saturn's moon Hyperion on May 31, 2015, at a distance of about 34,000 km (21,000 mi).[120]
Dione flyby
Cassini performed its last flyby of Saturn's moon Dione on August 17, 2015, at a distance of about 475 km (295 mi). A previous flyby was performed on June 16.[121]
Hexagon changes color
Between 2012 and 2016, the persistent hexagonal cloud pattern at Saturn's north pole changed from a mostly blue color to more of a golden color.[122] One theory for this is a seasonal change: extended exposure to sunlight may be creating haze as the pole swivels toward the Sun.[122] It was previously noted that there was less blue color overall on Saturn between 2004 and 2008.[123]
-
2012 and 2016: hexagon color changes
-
2013 and 2017: hexagon color changes
Grand Finale and destruction
Cassini's end involved a series of close Saturn passes, approaching within the rings, then an entry into Saturn's atmosphere on September 15, 2017, to destroy the spacecraft.[6][11][88] This method was chosen because it is imperative to ensure protection and prevent biological contamination to any of the moons of Saturn thought to offer potential habitability.[124]
In 2008 a number of options were evaluated to achieve this goal, each with varying funding, scientific, and technical challenges. A short period Saturn impact for an end of mission was rated "excellent" with the reasons "D-ring option satisfies unachieved AO goals;[definition needed] cheap and easily achievable" while collision with an icy moon was rated "good" for being "cheap and achievable anywhere/time".[citation needed]
There were problems in 2013–14 about NASA receiving U.S. government funding for the Grand Finale. The two phases of the Grand Finale ended up being the equivalent of having two separate Discovery Program-class missions in that the Grand Finale was completely different from the main Cassini regular mission. The U.S. government in late 2014 approved the Grand Finale at the cost of $200 million. This was far cheaper than building two new probes in separate Discovery-class missions.[125]
On November 29, 2016, the spacecraft performed a Titan flyby that took it to the gateway of F-ring orbits: This was the start of the Grand Finale phase culminating in its impact with the planet.[126][127] A final Titan flyby on April 22, 2017, changed the orbit again to fly through the gap between Saturn and its inner ring days later on April 26. Cassini passed about 3,100 km (1,900 mi) above Saturn's cloud layer and 320 km (200 mi) from the visible edge of the inner ring; it successfully took images of Saturn's atmosphere and began returning data the next day.[128] After a further 22 orbits through the gap, the mission was ended with a dive into Saturn's atmosphere on September 15; signal was lost at 11:55:46 UTC on September 15, 2017, just 30 seconds later than predicted. It is estimated that the spacecraft burned up about 45 seconds after the last transmission.
In September 2018, NASA won an
In December 2018, Netflix aired "NASA's Cassini Mission" on their series 7 Days Out documenting the final days of work on the Cassini mission before the spacecraft crashed into Saturn to complete its Grand Finale.
In January 2019, new research using data collected during Cassini's Grand Finale phase was published:
- The final close passes by the rings and planet enabled scientists to measure the length of a day on Saturn: 10 hours, 33 minutes and 38 seconds.
- Saturn's rings are relatively new, 10 to 100 million years old.[130]
Missions
The spacecraft operation was organized around a series of missions.[132] Each is structured according to a certain amount of funding, goals, etc.[132] At least 260 scientists from 17 countries have worked on the Cassini–Huygens mission; in addition thousands of people overall worked to design, manufacture, and launch the mission.[133]
- Prime Mission, July 2004 through June 2008.[134][135]
- Cassini Equinox Mission was a two-year mission extension which ran from July 2008 through September 2010.[132]
- Cassini Solstice Mission ran from October 2010 through April 2017.[132][136] (Also known as the XXM mission.)[123]
- Grand Finale (spacecraft directed into Saturn), April 2017 to September 15, 2017.[136]
-
Saturn by Cassini, 2016
-
Cassini-Huygens by the numbers
(September 2017) -
Farewell to Saturn and moons (Enceladus, Epimetheus, Janus, Mimas, Pandora and Prometheus)
(September 13, 2017)
Glossary
- AACS: Attitude and Articulation Control Subsystem
- ACS: Attitude Control Subsystem
- AFC: AACS Flight Computer
- ARWM: Articulated Reaction Wheel Mechanism
- ASI: Agenzia Spaziale Italiana, the Italian space agency
- BIU: Bus Interface Unit
- BOL: Beginning of Life
- CAM: Command Approval Meeting
- CDS: Command and Data Subsystem—Cassini computer that commands and collects data from the instruments
- CICLOPS: Cassini Imaging Central Laboratory for Operations Archived May 1, 2008, at the Wayback Machine
- CIMS: Cassini Information Management System
- CIRS: Composite Infrared Spectrometer
- DCSS: Descent Control Subsystem
- DSCC: Deep Space Communications Center
- DSN: Deep Space Network (large antennas around the Earth)
- DTSTART: Dead Time Start
- ELS: Electron Spectrometer (part of CAPS instrument)
- EOM: End of Mission
- ERT: Earth-received time, UTC of an event
- ESA: European Space Agency
- ESOC: European Space Operations Centre
- FSW: flight software
- HGA: High Gain Antenna
- HMCS: Huygens Monitoring and Control System
- HPOC: Huygens Probe Operations Center
- IBS: Ion Beam Spectrometer (part of CAPS instrument)
- IEB: Instrument Expanded Blocks (instrument command sequences)
- IMS: Ion Mass Spectrometer (part of CAPS instrument)
- ITL: Integrated Test Laboratory—spacecraft simulator
- IVP: Inertial Vector Propagator
- LGA: Low Gain Antenna
- NAC: Narrow Angle Camera
- NASA: National Aeronautics and Space Administration, the United States space agency
- OTM: Orbit Trim Maneuver
- PDRS: Probe Data Relay Subsystem
- PHSS: Probe Harness SubSystem
- POSW: Probe On-Board Software
- PPS: Power and Pyrotechnic Subsystem
- PRA: Probe Relay Antenna
- PSA: Probe Support Avionics
- PSIV: Preliminary Sequence Integration and Validation
- PSE: probe support equipment
- RCS: Reaction Control System
- RFS: Radio Frequency Subsystem
- RPX: ring plane crossing
- RWA: Reaction Wheel Assembly
- SCET: Spacecraft Event Time
- SCR: sequence change requests
- SKR: Saturn Kilometric Radiation
- SOI: Saturn Orbit Insertion (July 1, 2004)
- SOP: Science Operations Plan
- SSPS: Solid State Power Switch
- SSR: Solid State Recorder
- SSUP: Science and Sequence Update Process
- TLA: Thermal Louver Assemblies
- USO: UltraStable Oscillator
- VRHU: Variable Radioisotope Heater Units
- WAC: Wide Angle Camera
- XXM: Extended-Extended Mission
See also
- Europlanet, data network
- Galileo, Jupiter orbiter and entry probe (1989–2003)
- In Saturn's Rings
- List of missions to the outer planets
- Planetary Science Decadal Survey
- Timeline of Cassini–Huygens
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Further reading
- Ralph Lorenz (2017). NASA/ESA/ASI Cassini-Huygens: 1997 onwards (Cassini orbiter, Huygens probe and future exploration concepts) (Owners' Workshop Manual). Haynes Manuals, UK. ISBN 978-1785211119.
- ISBN 978-1-56751-125-3.
- David M. Harland (2002). Mission to Saturn: Cassini and the Huygens Probe. Springer-Verlag. ISBN 978-1-85233-656-1.
- Ralph Lorenz; ISBN 978-0-521-79348-3.
- Meltzer, Michael (2015). The Cassini-Huygens Visit to Saturn: A Historic Mission to the Ringed Planet. Cham: Springer International Publishing Switzerland. ISBN 978-3-319-07608-9.
- Irene Klotz (August 31, 2017). "Cassini's Ringside Seat At Saturn Coming To An End". Aviation Week & Space Technology. An epic journey of discovery at Saturn ends, leaving mysteries for future explorers.
External links
Official websites
- Cassini-Huygens website Archived January 26, 2018, at the Wayback Machine by the Jet Propulsion Laboratory
- Cassini-Huygens website by NASA
- Cassini-Huygens website by the European Space Agency
- Cassini-Huygens website Archived May 13, 2017, at the Wayback Machine by NASA's Solar System Exploration division
- Cassini Mission Archive Science-Data Repository at NASA's Planetary Data System
Media and telecommunications
- CICLOPS.org, Cassini imaging homepage
- Cassini Hall of Fame, image galleries by the Jet Propulsion Laboratory
- "Cassini at Saturn", a YouTube playlist by the Jet Propulsion Laboratory
- "Titan Touchdown", Depiction of Huygens descent and landing
- DESCANSO DSN Telecom information
- In Saturn's Rings, film animated from millions of still photographs
- Around Saturn, film animated from more than 200,000 images taken by Cassini from 2004 to 2012
- WebGL-based 3D rendering of Cassini
- Cassini image album by Kevin M. Gill
- NASA – Through the Eyes of Cassini