Mission Mars Dr. John D. Johnson Adjunct Professor, St. Ambrose University & Staff Member, John Deere.

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Presentation transcript:

Mission Mars Dr. John D. Johnson Adjunct Professor, St. Ambrose University & Staff Member, John Deere

Agenda Man’s Fascination with Mars A Quick Tour of the Red Planet The Race to Mars: Losers & Winners The Early Years ( ) The Viking Landers (1976) The Forgetful Years ( ) Recent Missions, 1996-present The Mars Exploration Rovers (Spirit & Opportunity) Goals: What do we hope to learn? Challenges: Engineering & Political Results: Images and Preliminary Findings What’s Next? Have we got Mars Fever? The Bigger Context: Why Look to the Heavens?

Mythical Mars Mars was the son of Juno and a magical flower and initially was the Roman god of fertility and vegetation but later became associated with battle. As the god of spring, when his major festivals were held, he presided over agriculture in general. In his warlike aspect, Mars was offered sacrifices before combat and was said to appear on the battlefield accompanied by Bellona, a warrior goddess variously identified as his wife, sister or daughter. Mars unlike his Greek counterpart, Ares, was more widely worshipped than any of the other Roman gods, probably because his sons Romulus and Remus were said to have founded Rome. As the consort of Rhea Sylvia and father of Romulus and Remus, Mars was considered the father of the Roman people.

Canals? Faces? Gods? Little Green Men (or Cats)?? Percival Lowell pictured Mars covered in canals

A Quick Tour of Mars Mars is the only planet whose surface features can be seen through ground-based telescopes Probes to Mars have found craters, volcanoes and canyons Olympus Mons is the largest volcano in the Solar System, taller than Mount Everest, with a base larger than Colorado Valles Marineris is a huge canyon, that would stretch the length of the United States, deep enough to swallow the Grand Canyon Surface features indicate that water once flowed on Mars

Early Mars Missions (1960s) Mars 1960A - USSR Mars Probe - (October 10, 1960) Failed to reach Earth orbit. Mars 1960B - USSR Mars Probe - (October 14, 1960) Failed to reach Earth orbit. Mars 1962A - USSR Mars Flyby - (October 24, 1962) Spacecraft failed to leave Earth orbit after the final rocket stage exploded. Mars 1 - USSR Mars Flyby kg - (November 1, 1962) Communications failed en route. Mars 1962B - USSR Mars Lander - (November 4, 1962) Failed to leave Earth orbit. Mariner 3 - USA Mars Flyby kg - (November 5, 1964) Mars flyby attempt. Solar panels failed to open, preventing flyby. Mariner 3 is now in a solar orbit. Mariner 4 - USA Mars Flyby kg - (November 28, December 20, 1967) Mariner 4 arrived at Mars on July 14, 1965 and passed within 9,920 kilometers of the planet's surface. It returned 22 close-up photos showing a cratered surface. The thin atmosphere was confirmed to be composed of carbon dioxide in the range of 5-10 mbar. A small intrinsic magnetic field was detected. Mariner 4 is now in a solar orbit. Zond 2 - USSR Mars Flyby - (November 30, 1964) Contact was lost en route. Failed. At this point, all space missions were focused on the Moon for the remainder of the 60s.

Early Mars Missions (1970 – 1973) Mariner 8 - USA Mars Flyby - (May 8, 1971) Failed to reach Earth orbit. Kosmos USSR Mars Probe - (May 10, 1971) Failed to leave Earth orbit. Mars 2 - USSR Mars Orbiter/Soft Lander - 4,650 kg - (May 19, 1971) The Mars 2 lander was released from the orbiter on November 27, It crashed-landed because its breaking rockets failed - no data was returned and the first human artifact was created on Mars. The orbiter returned data until Mars 3 - USSR Mars Orbiter/Soft Lander - 4,643 kg - (May 28, 1971) Mars 3 arrived at Mars on December 2, The lander was released and became the first successful landing on Mars. It failed after relaying 20 seconds of video data to the orbiter. The Mars 3 orbiter returned data until August, It made measurements of surface temperature and atmospheric composition. Mariner 9Mariner 9 - USA Mars Orbiter kg - (May 30, ) Mariner 9 arrived at Mars on November 3, 1971 and was placed into orbit on November 24. This was the first US spacecraft to enter an orbit around a planet other than the Moon. At the time of its arrival a huge dust storm was in progress on the planet. Many of the scientific experiments were delayed until the storm had subsided. The first hi-resolution images of the moons Phobos and Deimos were taken. River and channel like features were discovered. Mariner 9 is still in Martian orbit.PhobosDeimos Mars 4 - USSR Mars Orbiter - 4,650 kg - (July 21, 1973) Mars 4 arrived at Mars on February, 1974, but failed to go into orbit due to a malfunction of its breaking engine. It flew past the planet with in 2,200 kilometers of the surface. It returned some images and data. Mars 5 - USSR Mars Orbiter - 4,650 kg - (July 25, 1973) Mars 5 entered into orbit around Mars on February 12, It acquired imaging data for the Mars 6 and 7 missions. Mars 6 - USSR Mars Orbiter/Soft Lander - 4,650 kg - (August 5, 1973) On March 12, 1974, Mars 6 entered into orbit and launched its lander. The lander returned atmospheric descent data, but failed on its way down. Mars 7 - USSR Mars Orbiter/Soft Lander - 4,650 kg - (August 9, 1973) On March 6, 1974, Mars 7 failed to go into orbit about Mars and the lander missed the planet. Carrier and lander are now in a solar orbit.

Early Mars Missions (1976) Viking 1 - USA Mars Orbiter/Lander - 3,399 kg - (August 20, August 7, 1980) Viking 1 and 2 were designed after the Mariner spacecraft. They consisted of an orbiter and lander. The orbiter weighed 900 kg and the lander 600 kg. Viking 1 went into orbit about Mars on June 19, The lander touched down on July 20, 1976 on the western slopes of Chryse Planitia. Both landers had experiments to search for Martian micro-organism. The results of these experiments are still being debated. The landers provided detailed color panoramic views of the Martian terrain. They also monitored the Martian weather. The orbiters mapped the planet's surface, acquiring over 52,000 images. Viking 1 orbiter was deactivate on August 7, 1980 when it ran out of altitude-control propellant. Viking 1 lander was accidentally shut down on November 13, 1982, and communication was never regained. Viking 2 - USA Mars Orbiter/Lander - 3,399 kg - (September 9, July 25, 1978) Viking 1 and 2 were designed after the Mariner spacecraft. They consisted of an orbiter and lander. The orbiter weighed 900 kg and the lander 600 kg. Viking 2 went into orbit about Mars on July 24, The lander touched down on August 7, 1976 at Utopia Planitia. Both landers had experiments to search for Martian micro-organism. The results of these experiments are still being debated. The landers provided detailed color panoramic views of the Martian terrain. They also monitored the Martian weather. The orbiters mapped the planet's surface, acquiring over 52,000 images. Viking 2 orbiter was deactivate on July 25, 1978 when it ran out of altitude-control propellant. Viking 2 lander used Viking 1 orbiter as a communications relay, and had to be shut down at the same time as the orbiter on August 7, &

The Lonely Years ( ) Phobos 1 - USSR Mars Orbiter/Lander - 5,000 kg - (July 7, 1988) Phobos 1 was sent to investigate the Martian moon Phobos. It was lost en route to Mars through a command error on September 2, Phobos 2 - USSR Phobos Flyby/Lander - 5,000 kg - (July 12, 1988) Phobos 2 arrived at Mars and was inserted into orbit on January 30, The orbiter moved within 800 kilometers of Phobos and then failed. The lander never made it to Phobos. Mars Observer - USA Mars Orbiter - (September 25, 1992) Communication was lost with Mars Observer on August 21, 1993, just before it was to be inserted into orbit.

Recent Missions (1996) Mars Global Surveyor - USA Mars Orbiter - (November 7, 1996) Mars Global Surveyor was inserted into an elliptical capture orbit on 12 September The spacecraft was initiated due to the loss of the Mars Observer and the basic design is after the Mars Observer. Mars Global Surveyor is designed to orbit Mars over a two year period and collect data on the surface morphology, topography, composition, gravity, atmospheric dynamics, and magnetic field. This data will be used to investigate the surface processes, geology, distribution of material, internal properties, evolution of the magnetic field, and the weather and climate of Mars. Mars 96 - Russia Orbiter & Lander - (November 16, 1996) Mars '96 consisted of an orbiter, two landers, and two soil penetrators that were to reach the planet in September The rocket carring Mars 96 lifted off successfully, but as it entered orbit the rocket's fourth stage ignited prematurely and sent the probe into a wild tumble. It crashed into the ocean somewhere between the Chilean coast and Easter Island. The spacecraft sank, carrying with it 270 grams of plutonium-238. Failure. Mars Pathfinder - USA Lander & Surface Rover kg (lander), 10.5 kg (rover) - (December 4, September 27, 1997) Mars Pathfinder arrived at Mars on July 4, 1997 and impacted the surface at 16:57 UT (12:57 PM EDT) at a velocity of about 18 m/s (40 mph). It bounced about 15 meters (50 feet) into the air, bouncing another 15 times and rolling before coming to rest approximately 2.5 minutes after impact and about 1 km from the initial impact site. The landing site was in the Ares Vallis region is at N, W and was named the Sagan Memorial Station. A six-wheel rover, named Sojourner, rolled onto the Martian surface on July 6 at about 05:40 UT. Mars Pathfinder returned 2.6 billion bits of information, including more than 16,000 images from the lander and 550 images from the rover, as well as more than 15 chemical analyses of rocks and extensive data on winds and other weather factors. The last successful data transmission was on September 27, 1997, the 83rd day of the mission since landing on the surface. This is the second mission in NASA's low-cost Discovery series. &

Recent Missions ( ) Nozomi (Planet B) - Japan Mars Orbiter - (3 July 1998) Japan's Institute of Space and Astronautical Science (ISAS) launched this probe to study the Martian environment. This probe lost power and the fuel froze. It was unable to regain control and missed a second rendezvous with Mars in December Failure. Mars Climate Orbiter - USA Mars Orbiter - (11 December 1998) The Mars Climate Orbiter, also known as the Mars Surveyor '98 Orbiter, was a companion to the Mars Polar Lander. Its the mission was to study the Martian weather, climate, and water and carbon dioxide budget. It was destroyed when a navigation error caused it to miss its target altitude at Mars by 80 to 90 kilometers, instead of entering the Martian atmosphere at an altitude of 57 kilometers during the orbit insertion maneuver. Mars Polar Lander - USA Mars Lander - (3 January 1999) The Mars Polar Lander, also known as the Mars Surveyor '98 Lander, was a companion to the Mars Climate Orbiter. It was to touch down on the southern polar layered terrain, between 73 S and 76 S, less than 1000 km from the south pole, near the edge of the carbon dioxide ice cap in Mars' late southern spring. The last telemetry from the spacecraft was sent just prior to atmospheric entry on 3 December No further signals have been received from the lander, the cause of this loss of communication is not known. Deep Space 2 (DS2) - USA Mars Penetrators - (3 January 1999) The Deep Space 2 (DS2) project is a New Millennium mission consisting of two probes which were to penetrate the surface of Mars near the south polar layered terrain and send back data on the sub-surface properties. On 3 December 1999 the probes were nearing Mars on a trajectory to enter the atmosphere and bring them to their intended landing site, but contact was never made with either probe and the mission was presumed lost.

Recent Missions ( ) 2001 Mars Odyssey - USA Mars Orbiter - (7 April 2001) The 2001 Mars Odyssey orbiter will nominally orbit Mars for three years, with the objective of conducting a detailed mineralogical analysis of the planet's surface from orbit and measuring the radiation environment. The mission has as its primary science goals to gather data to help determine whether the environment on Mars was ever conducive to life, to characterize the climate and geology of Mars, and to study potential radiation hazards to possible future astronaut missions. Mars Express - ESA Mars Orbiter and Lander - 1 June 2003 (Arrived 25 December 2003) While the British Beagle 2 lander was lost, the orbiter has been highly successful returning a wealth of information related to the composition of Mars. Mars Exploration Rovers - USA Two Mars Rovers - 22 May/4 June Arrived in January 2004 on schedule, with successful landings in both cases. Early technical problems delayed both rovers, but two months into the missions, both are productive and gathering a wealth of data, and the associated orbiters are operating as planned.

Mars Odyssey The Mars Odyssey has been a very successful mission to-date. Odyssey is part of a years-long program of Mars missions -- orbiters and landers -- that aims to learn enough about the still- mysterious planet to properly plan a crewed mission, one that many researchers figure will be needed to find any conclusive evidence for life. We still don't know if there is water anywhere close to the surface of Mars, except for the frozen variety at the poles. We don't know how harsh the radiation environment is, and thus what it would take to protect human explorers. If there is life on Mars, it needs water.

Mars Odyssey Odyssey has a set of eyes that can virtually drill into the surface, perhaps as far down as 100 meters. Recent studies have suggested there may be water at that depth. But the scientist responsible for the newest search is not expecting to spot a drop. The resolution of the visible-light camera in not as good as the camera aboard Mars Global Surveyor, which over the past few years has returned thousand of photos of Mars. A pixel in a THEMIS visible-light image will represent 18 meters on the ground, where MGS resolves 1.5 meters per pixel. The Thermal Imager is a sensitive infrared camera, which senses heat, will improve on the efforts of MGS, sharpening the resolution from 3 kilometers per pixel to a stunning 100 meters. If Mars has any heated football fields, Odyssey will see them. The thermal imager will be most effective at night, when the surface is uniformly cool. During the day, a sun-facing slope is warmer than a shaded area. The thermal imager, which measures heat by sensing infrared radiation, is so sensitive it can spot temperature differences of just 1 degree, even from its perch 250 miles above the surface. THEMIS also looks at infrared "spectral bands," described as the ranges of colors given off by various minerals. Studying this data will allow scientists to detect silicates, sulfates, oxides and other minerals on Mars' surface. Some of the minerals Odyssey will look for form only in the presence of water.

Mars Odyssey

Mars Odyssey

Mars Odyssey

Mars Express The ESA Mars Express Orbiter has been highly successful since it first entered orbit around Mars on Christmas, It has detected vast fields of perennial water ice, stretching out from the south pole of the Red Planet. Extremely detailed imagery has been sent back, such as the highlights we will show here.

Mars Express also seeks evidence of water on Mars.

Mars Exploration Rovers NASA's twin robot geologists, the Mars Exploration Rovers, launched toward Mars on June 10 and July 7, 2003, in search of answers about the history of water on Mars. They successfully landed on Mars January 3 and January 24, Primary among the mission's scientific goals is to search for and characterize a wide range of rocks and soils that hold clues to past water activity on Mars. The spacecraft targeted sites on opposite sides of Mars that appear to have been affected by liquid water in the past. The landing sites are at Gusev Crater, a possible former lake in a giant impact crater, and Meridiani Planum, where mineral deposits (hematite) suggest Mars had a wet past. There was a LOT of science and engineering involved in designing, launching, guiding, controlling, landing, and operating the rovers for this mission.

Mars Exploration Rovers

Spirit Landing Site

Gusev Crater may once have been a lake bed. Both sites may have shared a wet history at some time in the distant past.

The scientists at JPL have a reason to celebrate, as both landers will have a soft landing on Mars.

Mars Exploration Rovers Once they land, you still have to get the rovers communicating, test them out and after a week or so, they finally roll over the platform onto Martian soil.

Debugging a glitch when you are 90 Million Miles away isn’t trivial! But, it’s rewarding when you finally start to take data and pilot a vehicle on another planet!

SPIRIT

OPPORTUNITY

What’s Next?

Mars Reconnaissance Orbiter As Earth pulls away from Mars after last month's close approach, NASA is developing a spacecraft that will take advantage of the next close encounter in That spacecraft, Mars Reconnaissance Orbiter, will make a more comprehensive inspection of our planetary neighbor than any previous mission. For starters, it will examine landscape details as small as a coffee table with the most powerful telescopic camera ever sent to orbit a foreign planet. Some of its other tools will scan underground layers for water and ice, identify small patches of surface minerals to determine their composition and origins, track changes in atmospheric water and dust, and check global weather every day.

A Manned Mission to Mars?

Why Look Up At The Heavens? Man has always looked for how he fits into the grand design, and through scientific exploration we will learn amazing facts that we could not have guessed at. We will learn better how planets are formed, the conditions required for life and perhaps how common life is in our galaxy We will eventually outgrow our planet and resources and need to move out amongst the stars We always advance technology through scientific endeavors We learn more about ourselves as we seek to learn about the world around us We are a part of the Universe. It is humbling and inspiring to observe it and learn our role in a truly vast and amazing universe.