Showing posts sorted by relevance for query voyager. Sort by date Show all posts
Showing posts sorted by relevance for query voyager. Sort by date Show all posts

Wednesday, June 12, 2024

Ed Stone: Former JPL Director & Voyager Project Scientist (1936-2024) | NASA

Ed Stone: Former JPL Director & Voyager Project Scientist (1936-2024) | NASA

Ed Stone, former director of the Jet Propulsion Laboratory (JPL) and project scientist for the Voyager mission, died on June 9, 2024. A friend, mentor, and colleague to many, he was known for his straightforward leadership and commitment to communicating with the public. 

Known for his steady leadership, consensus building, and enthusiasm for engaging the public in science, Stone left a deep impact on the space community.

Edward C. Stone was preceded in death by his wife, Alice Stone, whom he met at the University of Chicago. They are survived by their two daughters, Susan and Janet Stone, and two grandsons.

Stone also served as the David Morrisroe professor of physics and vice provost for special projects at Caltech in Pasadena, California, which last year established a new faculty position, the Edward C. Stone Professorship.

Ed Stone, former director of NASA’s Jet Propulsion Laboratory and longtime project scientist of the Voyager mission, passed away on June 9, 2024. He was 88 years old.

“Ed Stone was a trailblazer who dared mighty things in space. He was a dear friend to all who knew him, and a cherished mentor to me personally,” said Nicola Fox, associate administrator for the Science Mission Directorate at NASA Headquarters in Washington. “Ed took humanity on a planetary tour of our solar system and beyond, sending NASA where no spacecraft had gone before. His legacy has left a tremendous and profound impact on NASA, the scientific community, and the world. My condolences to his family and everyone who loved him. Thank you, Ed, for everything.”

Stone served on nine NASA missions as either principal investigator or a science instrument lead, and on five others as a co-investigator (a key science instrument team member). These roles primarily involved studying energetic ions from the Sun and cosmic rays from the galaxy. He had the distinction of being one of the few scientists involved with both the mission that has come closest to the Sun (NASA’s Parker Solar Probe) and the one that has traveled farthest from it (Voyager).

“Ed will be remembered as an energetic leader and scientist who expanded our knowledge about the universe—from the Sun to the planets to distant stars—and sparked our collective imaginations about the mysteries and wonders of deep space,” said Laurie Leshin, JPL director and Caltech vice president. “Ed’s discoveries have fueled exploration of previously unseen corners of our solar system and will inspire future generations to reach new frontiers. He will be greatly missed and always remembered by the NASA, JPL, and Caltech communities and beyond.”

At the Helm of Voyager

Stone is best known for his work on NASA’s longest-running mission, Voyager, whose twin spacecraft launched in 1977 and are still exploring deep space today. He served as Voyager’s sole project scientist from 1972 until his retirement in 2022. Under Stone’s leadership, the mission took advantage of a celestial alignment that occurs just once every 176 years to visit Jupiter, Saturn, Uranus, and Neptune. During their journeys, the spacecraft revealed the first active volcanoes beyond Earth, on Jupiter’s moon Io, and an atmosphere rich with organic molecules on Saturn’s moon Titan. Voyager 2 remains the only spacecraft to fly by Uranus and Neptune, revealing Uranus’ unusual tipped magnetic poles, and the icy geysers erupting from Neptune’s moon Triton.

Now more than 15 billion miles (24 million kilometers) from Earth, Voyager 1 is the most distant human-made object. Voyager 2, traveling slightly slower and in a different direction, is more than 12 billion miles (20 billion km) from Earth. Both probes are exploring interstellar space—the region outside the heliosphere, which is a protective bubble created by the Sun’s magnetic field and the outward flow of charged particles.

“Becoming Voyager project scientist was the best decision I made in my life,” Stone said in 2018. “It opened a wonderful door of exploration.”

He was particularly proud of the way Voyager quickened the pace of scientific analysis and took advantage of opportunities to engage the public. When Voyager 1 and 2 made their close flybys of the giant planets between 1979 and 1989, Stone was overseeing 11 teams of scientists, all accustomed to releasing their results at a slower pace through peer-reviewed journals.

Stone took the lead in tailoring the peer-review process to the faster pace of the mission’s planetary encounters: In the early afternoon, after data had come down, teams of scientists would decide what they thought their best results were for the day and hold up their conclusions for feedback in front of the whole science steering group.

Based on that discussion, Stone would choose the most interesting results to present to the media and the public the next morning. The scientists would then hone their presentations that evening and even overnight — with Stone often pressing them to come up with analogies that would make the material more approachable for a lay audience—while a graphics team worked on putting together supporting images. After the news conference the following morning, the process would begin anew. This cycle could continue daily through the duration of each planetary encounter.

“It was a very exciting time, and everyone was making discoveries,” said Stamatios “Tom” Krimigis of the Johns Hopkins Applied Physics Laboratory, who has served as the principal investigator of Voyager’s low-energy charged particles instrument since the mission’s launch. “Ed’s approach showed us how much public interest there really was in what Voyager was doing, but it also resulted in better science. You need more than one piece of information to make a picture, and hearing about other scientists’ data helped us interpret our own.”

It was a process that continued to serve the Voyager team well in 2012 and 2013 as they debated whether or not Voyager 1 had exited the heliosphere and entered interstellar space. Some signs pointed to a new environment, but one key marker — the direction of the magnetic field lines around Voyager — hadn’t changed as significantly as scientists expected.

The team remained puzzled for months until Voyager 1’s plasma wave instrument detected a significantly denser plasma environment around the spacecraft — the result of a chance outburst of material from the Sun that set the plasma around Voyager 1 ringing like a bell. Stone gathered the team.

“Nobody could wait to get to interstellar space, but we wanted to get it right,” said Suzanne Dodd, who has served as Voyager project manager, overseeing the engineering team, at JPL since 2010. “We knew there would be people who disagreed. So Ed wanted to understand the full story and the assumptions people were making. He did a good job listening to everybody and letting them participate in the dialogue without anyone monopolizing. Then he made a decision.”

Stone realized that the scientists didn’t need to fixate on the direction of the magnetic field lines. They were a proxy for the plasma environment. The team concluded that the plasma wave science instrument’s detection provided a better analysis of the current plasma environment and was evidence of humankind’s arrival into interstellar space.

Leading JPL

Voyager’s high profile lifted Stone’s profile as well. In 1991, roughly two years after the mission completed its planetary flybys, Stone became director of JPL, serving until 2001. Under his leadership, JPL was responsible for more than two dozen missions and instruments. Highlights for Stone’s tenure included landing NASA’s Pathfinder mission with the first Mars rover, Sojourner, in 1996 and launching the NASA-ESA (European Space Agency) Cassini/Huygens mission in 1997. The first Saturn orbiter, Cassini was a direct outgrowth of the scientific questions that arose from Voyager’s two flybys, and it carried the only probe that has ever landed in the outer solar system (at Titan).

The 1990s were an era of shifting national priorities after the Cold War, with significant cuts in spending in the NASA and defense budgets. Stone restructured several missions so that they could fly under these more stringent cost constraints, including overseeing a redesign of the Spitzer Space Telescope cooling system so that it was more cost effective and could still deliver high-impact science and stunning infrared images of the universe.

Journey to Space

Edward Carroll Stone Jr. was born on Jan. 23, 1936, in Knoxville, Iowa. The eldest of two sons of Edward Carroll Stone Sr. and Ferne Elizabeth Stone, he grew up in the nearby commercial center of Burlington.

Edward Stone Sr. was a construction superintendent who delighted in showing his son how to take things apart and put them back together again — cars, radios, hi-fi stereos. When the younger Stone was in junior high, the principal asked him to learn how to operate the school’s 16 mm movie projector and soon followed up with a request to run the school’s reel-to-reel tape recorder.

“I was always interested in learning about why something is this way and not that way,” Stone said in an interview about this career in 2018. “I wanted to understand and measure and observe.”

His first job was at a J.C. Penney department store, where he worked his way up from stockroom to clerk on the store floor. He also earned money playing French horn in the Burlington Municipal Band.

After high school, Stone enrolled in Burlington Junior College to study physics, and went on to the University of Chicago for graduate school. Shortly after he was accepted, the Soviet Union launched Sputnik and the Space Age began.

“Space was a brand-new field waiting for discovery,” Stone recalled in 2018.

He joined a team at the university that was building science instruments to launch into space. The first he designed rode aboard Discoverer 36, a since-declassified spy satellite that launched in 1961 and took photographs of Earth from space as part of the Corona program. Stone’s instrument, which measured the Sun’s energetic particles, helped scientists figure out why solar radiation was fogging the film and ultimately improved their understanding of the Van Allen belts, energetic particles trapped in Earth’s magnetic field.

In 1964, Stone joined Caltech as a postdoctoral fellow, running the university’s Space Radiation Lab together with Robbie Vogt, who had been a colleague at Chicago. They worked closely on a number of NASA satellite missions, studying galactic cosmic rays and solar energetic particles. In 1972, Vogt recommended Stone to JPL leadership for the position of Voyager project scientist, which he held for 50 years.

Among Stone’s many awards, the National Medal of Science from President George H.W. Bush stands out as the most prominent. In 2019 he won the Shaw Prize in Astronomy, with an award of $1.2 million, for his leadership in the Voyager project, which, as the citation noted, “has over the past four decades, transformed our understanding of the four giant planets and the outer solar system, and has now begun to explore interstellar space.” He was also proud to have a middle school named after him in Burlington, Iowa, as an inspiration to young learners.


Credit: NASA/Jet Propulsion Laboratory-Caltech

Release Date: June 11, 2024


#NASA #Astronomy #Space #Science #VoyagerSpacecraft #Voyager1 #Voyager2 #Planets #Mars #Jupiter #Saturn #SolarSystem #InterstellarSpace #MilkyWayGalaxy #SpaceExploration #EdStone #EdwardStone #Scientist #Explorer #Leader #JPL #Caltech #History #UnitedStates #STEM #Education

Monday, May 13, 2024

Madrid Deep Space Network Reaches NASA's Voyager 1 across 24 billion kilometers

Madrid Deep Space Network Reaches NASA's Voyager 1 across 24 billion kilometers

"By Their Powers Combined": This April 20, 2024, image shows a first—all six radio frequency antennas at the Madrid Deep Space Communication Complex in Spain, part of NASA’s Deep Space Network (DSN), carried out a test to receive data from the agency’s Voyager 1 spacecraft (1977-2024) at the same time.

Combining the antennas’ receiving power, or arraying, lets the DSN collect the very faint signals from faraway spacecraft. Voyager 1 is over 15 billion miles (24 billion kilometers) away, so its signal on Earth is far fainter than any other spacecraft that the DSN communicates with. It currently takes Voyager 1’s signal over 22 ½ hours to travel from the spacecraft to Earth. To better receive Voyager 1’s radio communications, a large antenna—or an array of multiple smaller antennas—can be used. A five-antenna array is currently needed to downlink science data from the spacecraft’s Plasma Wave System (PWS) instrument. As Voyager gets further way, six antennas will be needed.

The twin Voyager 1 and 2 spacecraft are still operating and traveling where no spacecraft—or anything touched by humanity—has gone before. As we celebrate the 47th anniversary of the Voyager 1 launch later this year, we will again reflect on the vision that inspired the mission, its greatest achievements, and its enduring legacy.

Image Description: In a nighttime landscape of rolling grasses and trees, six large off-white satellites face to the right. Each satellite has bright spotlights near it, but the surrounding area remains mostly dark.


Image Credit: MDSCC/INTA, Francisco “Paco” Moreno

Release Date: May 1, 2024


#NASA #Astronomy #Science #Space #VoyagerSpacecraft #Voyager1 #Planets #Jupiter #Saturn  #SolarSystem #Interstellar #MilkyWayGalaxy #SpaceExploration #RadioTelescopes #DSN #Madrid #Spain #EspaƱa #JPL #Caltech #California #History #UnitedStates #STEM #Education

Wednesday, June 12, 2024

A Tribute to Scientist & Explorer Edward C. Stone (1936-2024) | NASA/JPL

A Tribute to Scientist & Explorer Edward C. Stone (1936-2024) | NASA/JPL

Edward C. Stone, former director of NASA’s Jet Propulsion Laboratory (JPL) and longtime project scientist of the Voyager mission, passed away on June 9, 2024. He was 88 years old. In this 2018 video, Stone talks about the Voyager 2 spacecraft reaching interstellar space, six years after Voyager 1 reached the same milestone. The twin Voyager spacecraft were launched in 1977 on a five-year mission that is still operating today. Stone served as the mission’s project scientist for 50 years, from 1972 to 2022.

In addition to his work on Voyager, Stone was the director of JPL from 1991 to 2001. Under his leadership, JPL was responsible for 21 missions and instruments and developed six new missions. Highlights during Stone’s tenure included landing NASA’s Pathfinder mission with the first Mars rover, Sojourner, in 1996 and launching the NASA-European Space Agency (ESA) Cassini/Huygens mission in 1997. The first Saturn orbiter, Cassini was a direct outgrowth of the scientific questions that arose from Voyager’s two flybys, and it carried the only probe that has ever landed in the outer solar system (at Titan).

The twin Voyager 1 and 2 spacecraft are traveling where no spacecraft—or anything touched by humanity—has gone before. As we prepare to celebrate the 47th anniversary of the Voyager 1 launch later this year, we reflect on the vision and work of people like Ed Stone that supported its achievements and enduring legacy.


Video Credit: NASA's Jet Propulsion Laboratory (JPL)

Duration: 2 minutes

Release Date: June 11, 2024


#NASA #Astronomy #Space #Science #VoyagerSpacecraft #Voyager1 #Voyager2 #Planets #Mars #Jupiter #Saturn #SolarSystem #InterstellarSpace #MilkyWayGalaxy #SpaceExploration #EdStone #EdwardStone #Scientist #Explorer #JPL #Caltech #History #UnitedStates #STEM #Education #HD #Video

Friday, September 08, 2017

NASA's Voyager 1 Launches Aboard Titan III/Centaur in 1977


The Voyager 1 aboard the Titan III/Centaur lifted off on September 5, 1977, joining its sister spacecraft, the Voyager 2. NASA's Voyager 1 spacecraft launched atop its Titan/Centaur-6 launch vehicle from the Kennedy Space Center Launch Complex in Florida on September 5, 1977, at 8:56 a.m. local time.

The twin Voyager 1 and 2 spacecraft are still operating and traveling where no spacecraft—or anything touched by humanity—has gone before. As we celebrate the 40th anniversary of the Voyager 1 launch, we reflect on the vision that inspired the mission, its greatest achievements, and its enduring legacy.

Image Credit: NASA
Release Date: September 5, 2017

#NASA #Astronomy #Science #Space #Voyager #Voyager1 #Launch #Jupiter #Saturn #Voyager2 #Spacecraft #SolarSystem #Interstellar #MilkyWay #Exploration #History #JPL #Pasadena #California #Kennedy #KSC #Florida #UnitedStates #STEM #Education

Saturday, May 27, 2023

Crescent Planet Neptune and Moon Triton | NASA Voyager 2

Crescent Planet Neptune and Moon Triton | NASA Voyager 2

Gliding through the outer Solar System in 1989, the Voyager 2 spacecraft looked toward the Sun to find this view of most distant planet Neptune and its moon Triton together in a crescent phase. This elegant image of the ice-giant planet and its largest moon was taken from behind just after Voyager's closest approach. It could not have been taken from Earth because the most distant planet never shows a crescent phase to sunward eyes. Heading for the heliopause and beyond, Voyager 2's parting vantage point lacks Neptune's familiar blue hue. 

The nuclear-powered Voyager 2 spacecraft remains in contact with Earth through NASA's Deep Space Network. The Voyager 2 probe was launched on August 20, 1977.

Learn more about Planet Neptune:

https://solarsystem.nasa.gov/planets/neptune/overview/


Image Credit: NASA's Jet Propulsion Laboratory (JPL)

Image Date: August 1989


#NASA #Astronomy #Space #Science #Planet #Neptune #Moon #Triton #SolarSystem #Voyager2Spacecraft #SpaceExploration #JPL #Caltech #UnitedStates #STEM #Education

Sunday, September 03, 2017

Voyager 40th Anniversary Grand Tour Poster | NASA JPL


Launched in 1977 on a tour of the outer planets of the Solar System, Voyager 1 and 2 have become the longest operating and most distant spacecraft from Earth. Nearly 16 light-hours from the Sun, Voyager 2 has reached the edge of the heliosphere, the realm defined by the influence of the solar wind and the Sun's magnetic field. Now humanity's first ambassador to the Milky Way, Voyager 1 is over 19 light-hours away, beyond the heliosphere in interstellar space. Celebrate the Voyagers' 40 year journey toward the stars with NASA on September 5.

Poster Illustration Credit: NASA, JPL-Caltech, Voyager
Release Date: September 2, 2017


#NASA #Astronomy #Science #Space #Voyager #Voyager1 #Jupiter #Saturn #Voyager2 #Spacecraft #SolarSystem #Interstellar #MilkyWay #Exploration #History #JPL #Pasadena #California #UnitedStates #STEM #Education #Poster #Art

Milky Way Voyager 40th Anniversary Poster | NASA JPL


Launched in 1977 on a tour of the outer planets of the Solar System, Voyager 1 and 2 have become the longest operating and most distant spacecraft from Earth. Nearly 16 light-hours from the Sun, Voyager 2 has reached the edge of the heliosphere, the realm defined by the influence of the solar wind and the Sun's magnetic field. Now humanity's first ambassador to the Milky Way, Voyager 1 is over 19 light-hours away, beyond the heliosphere in interstellar space. Celebrate the Voyagers' 40 year journey toward the stars with NASA on September 5.

Poster Illustration Credit: NASA, JPL-Caltech, Voyager
Release Date: September 2, 2017


#NASA #Astronomy #Science #Space #Voyager #Voyager1 #Jupiter #Saturn #Voyager2 #Spacecraft #SolarSystem #Interstellar #MilkyWay #Exploration #History #JPL #Pasadena #California #UnitedStates #STEM #Education #Poster #Art #APoD

Voyager 40th Anniversary Grand Tour Poster | NASA JPL


Launched in 1977 on a tour of the outer planets of the Solar System, Voyager 1 and 2 have become the longest operating and most distant spacecraft from Earth. Nearly 16 light-hours from the Sun, Voyager 2 has reached the edge of the heliosphere, the realm defined by the influence of the solar wind and the Sun's magnetic field. Now humanity's first ambassador to the Milky Way, Voyager 1 is over 19 light-hours away, beyond the heliosphere in interstellar space. Celebrate the Voyagers' 40 year journey toward the stars with NASA on September 5.

Poster Illustration Credit: NASA, JPL-Caltech, Voyager
Release Date: September 2, 2017


#NASA #Astronomy #Science #Space #Voyager #Voyager1 #Jupiter #Saturn #Voyager2 #Spacecraft #SolarSystem #Interstellar #MilkyWay #Exploration #History #JPL #Pasadena #California #UnitedStates #STEM #Education #Poster #Art

Voyager 40th Anniversary "Disco" Poster | NASA JPL


Launched in 1977 on a tour of the outer planets of the Solar System, Voyager 1 and 2 have become the longest operating and most distant spacecraft from Earth. Nearly 16 light-hours from the Sun, Voyager 2 has reached the edge of the heliosphere, the realm defined by the influence of the solar wind and the Sun's magnetic field. Now humanity's first ambassador to the Milky Way, Voyager 1 is over 19 light-hours away, beyond the heliosphere in interstellar space. Celebrate the Voyagers' 40 year journey toward the stars with NASA on September 5.

Poster Illustration Credit: NASA, JPL-Caltech, Voyager
Release Date: September 2, 2017


#NASA #Astronomy #Science #Space #Voyager #Voyager1 #Jupiter #Saturn #Voyager2 #Spacecraft #SolarSystem #Interstellar #MilkyWay #Exploration #History #JPL #Pasadena #California #UnitedStates #STEM #Education #Poster #Art

Thursday, February 09, 2023

New Spokes Spotted on Saturn's Rings | Hubble

New Spokes Spotted on Saturn's Rings | Hubble


Mysterious Features First Seen Decades Ago by NASA's Voyager Spacecraft

Since their discovery by NASA's Voyager mission in the 1980s, temporary "spoke" features across Saturn's rings have fascinated scientists, yet eluded explanation. They have been observed in the years preceding and following the planet's equinox, becoming more prominent as the date approaches.

Image Description: Planet Saturn with bright white rings and multi-colored main sphere. Spoke features on the left side of the rings appear like faint gray smudges against the rings' bright backdrop, about midway from the planet to the rings' outer edge. Above the rings plane, the planet's bands are shades of red and orange, with brighter yellow nearer the equator.

Saturn's upcoming autumnal equinox of the northern hemisphere on May 6, 2025, means that spoke season has come again. NASA's Hubble Space Telescope will be on the job studying the spokes, thanks to time dedicated to Saturn in the mission’s ongoing Outer Planet Atmospheres Legacy (OPAL) program. Are the smudgy features related to Saturn's magnetic field and its interaction with the solar wind, as prevailing theory suggests? Confirmation could come in this spoke season, as scientists combine archival data from NASA's Cassini mission with new Hubble observations.

Planet Saturn with bright white rings and multi-colored main sphere. Spoke features appear like faint gray smudges against the rings' bright backdrop, about midway from the planet to the rings' outer edge. Above the rings plane, the planet's bands are shades of red and orange, with brighter yellow nearer the equator.

New images of Saturn from NASA's Hubble Space Telescope herald the start of the planet's "spoke season" surrounding its equinox, when enigmatic features appear across its rings. The cause of the spokes, as well as their seasonal variability, has yet to be fully explained by planetary scientists.

Like Earth, Saturn is tilted on its axis and therefore has four seasons, though because of Saturn's much larger orbit, each season lasts approximately seven Earth years. Equinox occurs when the rings are tilted edge-on to the Sun. The spokes disappear when it is near summer or winter solstice on Saturn. (When the Sun appears to reach either its highest or lowest latitude in the northern or southern hemisphere of a planet.) As the autumnal equinox of Saturn's northern hemisphere on May 6, 2025, draws near, the spokes are expected to become increasingly prominent and observable.

The suspected culprit for the spokes is the planet's variable magnetic field. Planetary magnetic fields interact with the solar wind, creating an electrically charged environment (on Earth, when those charged particles hit the atmosphere this is visible in the northern hemisphere as the aurora borealis, or northern lights). Scientists think that the smallest, dust-sized icy ring particles can become charged as well, which temporarily levitates those particles above the rest of the larger icy particles and boulders in the rings.

The ring spokes were first observed by NASA's Voyager mission in the early 1980s. The transient, mysterious features can appear dark or light depending on the illumination and viewing angles.

"Thanks to Hubble's OPAL program, which is building an archive of data on the outer solar system planets, we will have longer dedicated time to study Saturn’s spokes this season than ever before," said NASA senior planetary scientist Amy Simon, head of the Hubble Outer Planet Atmospheres Legacy (OPAL) program.

Saturn's last equinox occurred in 2009, while NASA's Cassini spacecraft was orbiting the gas giant planet for close-up reconnaissance. With Cassini's mission completed in 2017, and the Voyager spacecrafts long gone, Hubble is continuing the work of long-term monitoring of changes on Saturn and the other outer planets.

"Despite years of excellent observations by the Cassini mission, the precise beginning and duration of the spoke season is still unpredictable, rather like predicting the first storm during hurricane season," Simon said.

While our solar system's other three gas giant planets also have ring systems, nothing compares to Saturn's prominent rings, making them a laboratory for studying spoke phenomena. Whether spokes could or do occur at other ringed planets is currently unknown. "It's a fascinating magic trick of nature we only see on Saturn—for now at least," Simon said.

Hubble's OPAL program will add both visual and spectroscopic data, in wavelengths of light from ultraviolet to near-infrared, to the archive of Cassini observations. Scientists are anticipating putting these pieces together to get a more complete picture of the spoke phenomenon, and what it reveals about ring physics in general.

The Hubble Space Telescope is a project of international cooperation between NASA and the European Space Agency (ESA). NASA's Goddard Space Flight Center in Greenbelt, Maryland, manages the telescope. The Space Telescope Science Institute (STScI) in Baltimore conducts Hubble science operations. STScI is operated for NASA by the Association of Universities for Research in Astronomy, in Washington, D.C.


Image & Caption Credit: NASA, European Space Agency (ESA), Space Telescope Science Institute (STScI)

Processing: Alyssa Pagan (STScI)

Image Date: Sept. 22, 2022

Release Date: Feb. 9, 2023


#NASA #Hubble #Astronomy #Space #Science #Planet #Saturn #Rings #Spokes #SolarSystem #Exploration #Voyager #Spacecraft #Cosmos #Universe #HST #SpaceTelescope #ESA #Europe #GSFC #STScI #UnitedStates #Infographic #STEM #Education

Thursday, August 02, 2018

Planet Uranus | NASA Voyager 2

The dark side of Uranus imaged by a departing Voyager 2 spacecraft on Feb. 2, 1986 from a distance of 1.189 million kilometers.

Uranus is the seventh planet from the Sun. It has the third-largest planetary radius and fourth-largest planetary mass in the Solar System. Uranus is similar in composition to Neptune, and both have different bulk chemical composition from that of the larger gas giants Jupiter and Saturn. For this reason, scientists often classify Uranus and Neptune as "ice giants" to distinguish them from the gas giants. Uranus's atmosphere is similar to Jupiter's and Saturn's in its primary composition of hydrogen and helium, but it contains more "ices" such as water, ammonia, and methane, along with traces of other hydrocarbons. It is the coldest planetary atmosphere in the Solar System, with a minimum temperature of 49 K (−224 °C; −371 °F), and has a complex, layered cloud structure with water thought to make up the lowest clouds and methane the uppermost layer of clouds. The interior of Uranus is mainly composed of ices and rock.

Like the other giant planets, Uranus has a ring system, a magnetosphere, and numerous moons. The Uranian system has a unique configuration among those of the planets because its axis of rotation is tilted sideways, nearly into the plane of its solar orbit. Its north and south poles, therefore, lie where most other planets have their equators. In 1986, images from Voyager 2 showed Uranus as an almost featureless planet in visible light, without the cloud bands or storms associated with the other giant planets. Observations from Earth have shown seasonal change and increased weather activity as Uranus approached its equinox in 2007. Wind speeds can reach 250 meters per second (900 km/h; 560 mph).
(Source: Wikipedia)

Credit: NASA/JPL
Processing: Jason Major
Image Date: Feb. 2, 1986
Release Date: July 31, 2018

#NASA #Astronomy #Space #Science #Uranus #Planet #Atmosphere #SolarSystem #Voyager2 #Voyager #Spacecraft #JPL #Caltech #STEM #Education

Tuesday, May 15, 2018

Earth & Moon | NASA's Mars Cube One


A Pale Blue Dot via CubeSat | NASA JPL
First image captured by one of NASA's Mars Cube One (MarCO) CubeSats
The image, which shows both the CubeSat's unfolded high-gain antenna at right and the Earth and its moon in the center, was acquired by MarCO-B on May 9. Distance: Over 1 million kilometers from Earth
May 15, 2018: NASA's Voyager 1 took a classic portrait of Earth from several billion miles away in 1990. Now a class of tiny, boxy spacecraft, known as CubeSats, have just taken their own version of a "pale blue dot" image, capturing Earth and its moon in one shot.

NASA set a new distance record for CubeSats on May 8 when a pair of CubeSats called Mars Cube One (MarCO) reached 621,371 miles (1 million kilometers) from Earth. One of the CubeSats, called MarCO-B (and affectionately known as "Wall-E" to the MarCO team) used a fisheye camera to snap its first photo on May 9. That photo is part of the process used by the engineering team to confirm the spacecraft's high-gain antenna has properly unfolded.

As a bonus, it captured Earth and its moon as tiny specks floating in space.

"Consider it our homage to Voyager," said Andy Klesh, MarCO's chief engineer at NASA's Jet Propulsion Laboratory, Pasadena, California. JPL built the CubeSats and leads the MarCO mission. "CubeSats have never gone this far into space before, so it's a big milestone. Both our CubeSats are healthy and functioning properly. We're looking forward to seeing them travel even farther."

The MarCO spacecraft are the first CubeSats ever launched to deep space. Most never go beyond Earth orbit; they generally stay below 497 miles (800 kilometers) above the planet. Though they were originally developed to teach university students about satellites, CubeSats are now a major commercial technology, providing data on everything from shipping routes to environmental changes.

The MarCO CubeSats were launched on May 5 along with NASA's InSight lander, a spacecraft that will touch down on Mars and study the planet's deep interior for the first time. InSight, short for Interior Exploration using Seismic Investigations, Geodesy and Heat Transport, will attempt to land on Mars on Nov. 26. JPL also leads the InSight mission.

Mars landings are notoriously challenging due to the Red Planet's thin atmosphere. The MarCO CubeSats will follow along behind InSight during its cruise to Mars. Should they make it all the way to Mars, they will radio back data about InSight while it enters the atmosphere and descends to the planet's surface. The high-gain antennas are key to that effort; the MarCO team have early confirmation that the antennas have successfully deployed, but will continue to test them in the weeks ahead.

InSight won't rely on the MarCO mission for data relay. That job will fall to NASA's Mars Reconnaissance Orbiter. But the MarCOs could be a pathfinder so that future missions can "bring their own relay" to Mars. They could also demonstrate a number of experimental technologies, including their antennas, radios and propulsion systems, which will allow CubeSats to collect science in the future.

Later this month, the MarCOs will attempt the first trajectory correction maneuvers ever performed by CubeSats. This maneuver lets them steer towards Mars, blazing a trail for CubeSats to come.

For more information about MarCO, visit:
www.jpl.nasa.gov/cubesat/missions/marco.php
https://www.jpl.nasa.gov/news/press_kits/insight/appendix/mars-cube-one/

Credit: NASA/JPL-Caltech
Release Date: May 15, 2018


#NASA #Space #Mars #Earth #PaleBlueDot #Moon #MarCOs #MarsCubeOne #CubeSats #Nanosats #Insight #Voyager #Voyager1 #JPL #Caltech #Pasadena #California #UnitedStates #STEM #Education

Wednesday, September 21, 2022

Neptune’s Rings: Clearest View in Decades | James Webb Space Telescope

Neptune’s Rings: Clearest View in Decades | James Webb Space Telescope

Infrared Observations Tease Out Never Seen Atmospheric and Ring Details

The NASA/European Space Agency/Canadian Space Agency James Webb Space Telescope is showing off its capabilities closer to home with its first image of Neptune. Not only has Webb captured the clearest view of this peculiar planet’s rings in more than 30 years, but its cameras are also revealing the ice giant in a whole new light.

Image Description: Webb’s Near-Infrared Camera (NIRCam) image of Neptune, taken on July 12, 2022. The most prominent features of Neptune’s atmosphere in this image are a series of bright patches in the planet’s southern hemisphere that represent high-altitude methane-ice clouds. More subtly, a thin line of brightness circling the planet’s equator could be a visual signature of global atmospheric circulation that powers Neptune’s winds and storms. Additionally, for the first time, Webb has teased out a continuous band of high-latitude clouds surrounding a previously-known vortex at Neptune’s southern pole.

Neptune lurks in one of the dimmest parts of our solar system. With its complex rings, bizarre moon, Triton, and roaring winds faster than the speed of sound here on Earth, Neptune has long perplexed astronomers. Just one spacecraft, Voyager 2, has ever visited this far-flung planet, and observations from both space- and ground-based telescopes over the years have tracked the many turbulent storms.

Most striking in Webb’s new image is the crisp view of the planet’s rings—some of which have not been detected since NASA’s Voyager 2 became the first spacecraft to observe Neptune during its flyby in 1989. In addition to several bright, narrow rings, the Webb image clearly shows Neptune’s fainter dust bands. 

“It has been three decades since we last saw those faint, dusty bands, and this is the first time we’ve seen them in the infrared,” notes Heidi Hammel, a Neptune system expert and interdisciplinary scientist for Webb. Webb’s extremely stable and precise image quality permits these very faint rings to be detected so close to Neptune.

Neptune has fascinated researchers since its discovery in 1846. Located 30 times farther from the Sun than Earth, Neptune orbits in the remote, dark region of the outer solar system. At that extreme distance, the Sun is so small and faint that high noon on Neptune is similar to a dim twilight on Earth. 

This planet is characterized as an ice giant due to the chemical make-up of its interior. Compared to the gas giants, Jupiter and Saturn, Neptune is much richer in elements heavier than hydrogen and helium. This is readily apparent in Neptune’s signature blue appearance in Hubble Space Telescope images at visible wavelengths, caused by small amounts of gaseous methane. 

Webb’s Near-Infrared Camera (NIRCam) images objects in the near-infrared range from 0.6 to 5 microns, so Neptune does not appear blue to Webb. In fact, the methane gas so strongly absorbs red and infrared light that the planet is quite dark at these near-infrared wavelengths, except where high-altitude clouds are present. Such methane-ice clouds are prominent as bright streaks and spots, which reflect sunlight before it is absorbed by methane gas. Images from other observatories, including the Hubble Space Telescope and the W.M. Keck Observatory, have recorded these rapidly evolving cloud features over the years. 

More subtly, a thin line of brightness circling the planet’s equator could be a visual signature of global atmospheric circulation that powers Neptune’s winds and storms. The atmosphere descends and warms at the equator, and thus glows at infrared wavelengths more than the surrounding, cooler gases. 

Neptune’s 164-year orbit means its northern pole, at the top of this image, is just out of view for astronomers, but the Webb images hint at an intriguing brightness in that area. A previously-known vortex at the southern pole is evident in Webb’s view, but for the first time Webb has revealed a continuous band of high-latitude clouds surrounding it.

Webb also captured seven of Neptune’s 14 known moons. 

The James Webb Space Telescope is the world's premier space science observatory. Webb will solve mysteries in our solar system, look beyond to distant worlds around other stars, and probe the mysterious structures and origins of our universe and our place in it. Webb is an international program led by NASA with its partners, the European Space Agency (ESA) and the Canadian Space Agency (CSA).


Credits: NASA, ESA, CSA, Space Telescope Science Institute (STScI)

Image Date: July 12, 2022

Release Date: September 21, 2022


#NASA #ESA #Astronomy #Space #Science #Neptune #Planet #Rings #Atmosphere #Moons #NIRCam #Infrared #JamesWebb #WebbTelescope #JWST #SpaceTelescope #SolarSystem #Cosmos #Universe #UnfoldTheUniverse #Europe #CSA #Canada #GSFC #STScI #STEM #Education

Monday, July 01, 2024

Saturn Moons Titan & Tethys | NASA Cassini Mission

Saturn Moons Titan & Tethys | NASA Cassini Mission

NASA's Cassini spacecraft arrived in the Saturn system in 2004 and ended its mission in 2017 by deliberately plunging into Saturn's atmosphere. This method was chosen because it is necessary to ensure protection and prevent biological contamination to any of the moons of Saturn thought to offer potential habitability. The Cassini Mission mapped more than 620,000 square miles (1.6 million square kilometers) of liquid lakes and seas on the surface of Saturn's largest moon Titan (visible in foreground). This work was performed with its radar instrument that sent out radio waves and collected a return signal (or echo) that provided information about the terrain and the liquid bodies' depth and composition, along with two imaging systems that could penetrate the moon's thick atmospheric haze.

Titan is larger than the planet Mercury and is the second largest moon in our solar system. Titan is the only moon known to have a dense atmosphere, and the only object in space, other than Earth, where clear evidence of stable bodies of surface liquid has been found. Titan’s subsurface water could be a place to harbor life as we know it, while its surface lakes and seas of liquid hydrocarbons could conceivably harbor life that uses different chemistry than we are used to—that is, life as we do not yet know it. 

Tethys (visible in background) is Saturn's fifth largest moon. This cold, airless and heavily scarred body is very similar to sister moons Dione and Rhea except that Tethys is not as heavily cratered as the other two. This may be because its proximity to Saturn causes more tidal warming, and that warming kept Tethys partially molten longer, erasing or dulling more of the early terrain.

Tethys' density is 0.97 times that of liquid water. This suggests that Tethys is composed almost entirely of water ice plus a small amount of rock.

Tethys has a high reflectivity (or visual albedo) of 1.229 in the visual range, again suggesting a composition largely of water ice. However, this would behave like rock in the Tethyan average temperature of -305 degrees Fahrenheit (-187 degrees Celsius). Many of the crater floors on Tethys are bright, suggesting an abundance of water ice. Also contributing to the high reflectivity is that Tethys is bombarded by Saturn E-ring water-ice particles generated by geysers on Enceladus.

Tethys appeared as a tiny dot to astronomers until the Voyager (1 and 2) encounters in 1980 and 1981. The Voyager images showed a major impact crater and a great chasm. The Cassini spacecraft has added details including a great variety of colors at small scales suggesting a variety of materials not seen elsewhere.

The Cassini-Huygens mission was a cooperative project of NASA, European Space Agency (ESA) and the Italian Space Agency. NASA's Jet Propulsion Laboratory, a division of Caltech in Pasadena, California, manages the mission for NASA's Science Mission Directorate, Washington. JPL designed, developed and assembled the Cassini orbiter. The Cassini radar instrument was built by JPL and the Italian Space Agency, working with team members from the U.S. and several European countries.

Cassini Mission information:

https://solarsystem.nasa.gov/cassini


Image Credit: NASA / JPL-Caltech / SSI / CICLOPS

Processing: Kevin M. Gill

Image Date: Nov. 26 2009

Image Date: July 1, 2024


#NASA #Astronomy #Space #Science #Planet #Saturn #Moons #Titan #Tethys #Astrobiology #SolarSystem #CassiniMission #CassiniSpacecraft #JPL #Caltech #UnitedStates #ESA #Italy #Italia #ASI #Europe #STEM #Education

Friday, January 28, 2022

Saturn and Tethys | NASA Cassini Mission

Saturn and Tethys | NASA Cassini Mission

Italian mathematician, astronomer and engineer, Giovanni Cassini, discovered Tethys on March 21, 1684.

Overview

Tethys is Saturn's fifth largest moon. Its irregular shape is 331 miles (533 kilometers) in mean radius, with dimensions 669 x 657 x 654 miles (1076.8 x 1057.4 x 1052.6 kilometers). This cold, airless and heavily scarred body is very similar to sister moons Dione and Rhea except that Tethys is not as heavily cratered as the other two. This may be because its proximity to Saturn causes more tidal warming, and that warming kept Tethys partially molten longer, erasing or dulling more of the early terrain.

Tethys' density is 0.97 times that of liquid water, which suggests that Tethys is composed almost entirely of water ice plus a small amount of rock.

Tethys has a high reflectivity (or visual albedo) of 1.229 in the visual range, again suggesting a composition largely of water ice, which would behave like rock in the Tethyan average temperature of -305 degrees Fahrenheit (-187 degrees Celsius). Many of the crater floors on Tethys are bright, which also suggests an abundance of water ice. Also contributing to the high reflectivity is that Tethys is bombarded by Saturn E-ring water-ice particles generated by geysers on Enceladus.

Tethys appeared as a tiny dot to astronomers until the Voyager (1 and 2) encounters in 1980 and 1981. The Voyager images showed a major impact crater and a great chasm. The Cassini spacecraft has added details including a great variety of colors at small scales suggesting a variety of materials not seen elsewhere.

For more than a decade, NASA’s Cassini spacecraft shared the wonders of Saturn and its family of icy moons—taking us to astounding worlds where methane rivers run to a methane sea and where jets of ice and gas are blasting material into space from a liquid water ocean that might harbor the ingredients for life.

Cassini revealed in great detail the true wonders of Saturn, a giant world ruled by raging storms and delicate harmonies of gravity.

Cassini carried a passenger to the Saturn system, the European Huygens probe—the first human-made object to land on a world in the distant outer solar system.

After 20 years in space — 13 of those years exploring Saturn — Cassini exhausted its fuel supply. And so, to protect moons of Saturn that could have conditions suitable for life, Cassini was sent on a daring final mission that would seal its fate. After a series of nearly two dozen nail-biting dives between the planet and its icy rings, Cassini plunged into Saturn’s atmosphere on Sept. 15, 2017, returning science data to the very end.

Credit: NASA/JPL-Caltech/Space Science Institute (SSI)/CICLOPS/Kevin M. Gill

Image Date: August 19, 2012

Release Date: January 3, 2022

#NASA #Astronomy #Science #Space #Saturn #Planet #Rings #Shadows #Moon #Tethys #SolarSystem #Exploration #Cassini #Spacecraft #JPL #California #SSI #UnitedStates #ESA #History #STEM #Education

Wednesday, May 10, 2023

Planet Uranus’ Large Moons: Four May Hold Water | NASA/JPL

Planet Uranus’ Large Moons: Four May Hold Water | NASA/JPL

New modeling shows that there likely is an ocean layer in four of Uranus' major moons: Ariel, Umbriel, Titania, and Oberon. Miranda is too small to retain enough heat for an ocean layer.

Re-analysis of data from NASA’s Voyager spacecraft, along with new computer modeling, has led NASA scientists to conclude that four of Uranus’ largest moons likely contain an ocean layer between their cores and icy crusts. Their study is the first to detail the evolution of the interior makeup and structure of all five large moons: Ariel, Umbriel, Titania, Oberon, and Miranda. The work suggests four of the moons hold oceans that could be dozens of miles deep.

In all, at least 27 moons circle Uranus, with the four largest ranging from Ariel, at 720 miles (1,160 kilometers) across, to Titania, which is 980 miles (1,580 kilometers) across. Scientists have long thought that Titania, given its size, would be most likely to retain internal heat, caused by radioactive decay. The other moons had previously been widely considered too small to retain the heat necessary to keep an internal ocean from freezing, especially because heating created by the gravitational pull of Uranus is only a minor source of heat.

The National Academies’ 2023 Planetary Science and Astrobiology Decadal Survey prioritized exploring Uranus. In preparation for such a mission, planetary scientists are focusing on the ice giant to bolster their knowledge about the mysterious Uranus system. Published in the Journal of Geophysical Research, the new work could inform how a future mission might investigate the moons, but the paper also has implications that go beyond Uranus, said lead author Julie Castillo-Rogez of NASA’s Jet Propulsion Laboratory in Southern California.

Journal of Geophysical Research article:

https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2022JE007432

“When it comes to small bodies—dwarf planets and moons—planetary scientists previously have found evidence of oceans in several unlikely places, including the dwarf planets Ceres and Pluto, and Saturn’s moon Mimas,” she said. “So there are mechanisms at play that we don’t fully understand. This paper investigates what those could be and how they are relevant to the many bodies in the solar system that could be rich in water but have limited internal heat.”

The study revisited findings from NASA’s Voyager 2 flybys of Uranus in the 1980s and from ground-based observations. The authors built computer models infused with additional findings from NASA’s Galileo, Cassini, Dawn, and New Horizons (each of which discovered ocean worlds), including insights into the chemistry and the geology of Saturn’s moon Enceladus, Pluto and its moon Charon, and Ceres—all icy bodies around the same size as the Uranian moons.

What Lies Above and Beneath

The researchers used that modeling to gauge how porous the Uranian moons’ surfaces are, finding that they’re likely insulated enough to retain the internal heat that would be needed to host an ocean. In addition, they found what could be a potential heat source in the moons’ rocky mantles, which release hot liquid, and would help an ocean maintain a warm environment—a scenario that is especially likely for Titania and Oberon, where the oceans may even be warm enough to potentially support habitability.

By investigating the composition of the oceans, scientists can learn about materials that might be found on the moons’ icy surfaces as well, depending on whether substances underneath were pushed up from below by geological activity. There is evidence from telescopes that at least one of the moons, Ariel, has material that flowed onto its surface, perhaps from icy volcanoes, relatively recently.

In fact, Miranda, the innermost and fifth largest moon, also hosts surface features that appear to be of recent origin, suggesting it may have held enough heat to maintain an ocean at some point. The recent thermal modeling found that Miranda is unlikely to have hosted water for long: It loses heat too quickly and is probably frozen now.

However, internal heat would not be the only factor contributing to a moon’s subsurface ocean. A key finding in the study suggests that chlorides, as well as ammonia, are likely abundant in the oceans of the icy giant’s largest moons. Ammonia has been long known to act as antifreeze. In addition, the modeling suggests that salts likely present in the water would be another source of antifreeze, maintaining the bodies’ internal oceans.

Of course, there still are a lot of questions about the large moons of Uranus, Castillo-Rogez said, adding that there is plenty more work to be done: “We need to develop new models for different assumptions on the origin of the moons in order to guide planning for future observations.”

Digging into what lies beneath and on the surfaces of these moons will help scientists and engineers choose the best science instruments to survey them. For instance, determining that ammonia and chlorides may be present means that spectrometers, which detect compounds by their reflected light, would need to use a wavelength range that covers both kinds of compounds.

Likewise, they can use that knowledge to design instruments that can probe the deep interior for liquid. Searching for electrical currents that contribute to a moon’s magnetic field is generally the best way to find a deep ocean, as Galileo mission scientists did at Jupiter’s moon Europa. However, the cold water in the interior oceans of moons such as Ariel and Umbriel could make the oceans less able to carry these electrical currents and would present a new kind of challenge for scientists working to figure out what lies beneath.


Credit: NASA's Jet Propulsion Laboratory (JPL)

Release Date: May 4, 2023


#NASA #Space #Astronomy #Science #SolarSystem #Planet #Uranus #UranianSystem #Moons #Ariel #Umbriel #Titania #Oberon #OceanWorlds #Astrobiology #VoyagerSpacecraft #JPL #Caltech #UnitedStates #SpaceExploration #Illustration #Infographic #STEM #Education

Thursday, August 17, 2023

Planet Neptune's Cloud Cover over Three Decades: Linked to Solar Cycle | Hubble

Planet Neptune's Cloud Cover over Three Decades: Linked to Solar Cycle | Hubble


This sequence of Hubble Space Telescope images chronicles the waxing and waning of the amount of cloud cover on Neptune. This long set of observations shows that the number of clouds grows increasingly following a peak in the solar cycle—where the Sun's level of activity rhythmically rises and falls over an 11-year period. The chemical changes are caused by photochemistry, which happens high in Neptune's upper atmosphere and takes time to form clouds.

The images reveal an intriguing pattern between seasonal changes in Neptune’s cloud cover and the solar cycle—the period when the Sun's magnetic field flips every 11 years as it becomes more tangled like a ball of yarn. This is evident in the increasing number of sunspots and increasing solar flare activity. As the cycle progresses, the Sun’s tempestuous behavior builds to a maximum, until the magnetic field beaks down and reverses polarity. Then the Sun settles back down to a minimum, only to start another cycle.

When it is stormy weather on the Sun, more intense ultraviolet (UV) radiation floods the solar system. The team found that two years after the solar cycle's peak, an increasing number of clouds appear on Neptune. The team further found a positive correlation between the number of clouds and the ice giant's brightness from the sunlight reflecting off it.

The link between Neptune and solar activity is surprising to planetary scientists because Neptune is our solar system's farthest major planet and receives sunlight with about 0.1% of the intensity Earth receives. Yet Neptune's global cloudy weather seems to be driven by solar activity, and not the planet's four seasons, which each last approximately 40 years.

In 1989, NASA's Voyager 2 spacecraft provided the first close-up images of linear, bright clouds, reminiscent of cirrus clouds on Earth, seen high in Neptune's atmosphere. They form above most of the methane in Neptune's atmosphere and reflect all colors of sunlight, which makes them white. Hubble picks up where the brief Voyager flyby left off by continually keeping an eye on the planet yearly.

The Hubble Space Telescope is a project of international cooperation between NASA and the European Space Agency (ESA). NASA's Goddard Space Flight Center in Greenbelt, Maryland, manages the telescope. The Space Telescope Science Institute (STScI) in Baltimore conducts Hubble science operations. STScI is operated for NASA by the Association of Universities for Research in Astronomy, in Washington, D.C.


Credits: NASA, European Space Agency, Erandi Chavez (UC Berkeley), Imke de Pater (UC Berkeley)

Release Date: Aug. 17, 2023


#NASA #Hubble #Astronomy #Space #Science #Sun #SolarCycle #UltravioletRadiation #Planet #Neptune #Atmosphere #Photochemistry #Clouds #SolarSystem #SpaceExploration #VoyagerSpacecraft #Cosmos #Universe #HST #HubbleSpaceTelescope #ESA #Europe #GSFC #STScI #UnitedStates #Infographic #STEM #Education

Thursday, September 29, 2022

NASA’s Juno Shares First Image From Flyby of Jupiter’s Moon Europa | JPL

NASA’s Juno Shares First Image From Flyby of Jupiter’s Moon Europa | JPL


Closest view of Europa in over Twenty Years!

Sept. 29, 2022: Observations from the Juno spacecraft’s pass of Juputer's moon Europa provided the first close-up in over two decades of this ocean world, resulting in remarkable imagery and unique science.

The first picture NASA’s Juno spacecraft took as it flew by Jupiter’s ice-encrusted moon Europa has arrived on Earth. Revealing surface features in a region near the moon’s equator called Annwn Regio, the image was captured during the solar-powered spacecraft’s closest approach, on Thursday, Sept. 29, at 2:36 a.m. PDT (5:36 a.m. EDT), at a distance of about 219 miles (352 kilometers).

This is only the third close pass in history below 310 miles (500 kilometers) altitude and the closest look any spacecraft has provided at Europa since Jan. 3, 2000, when NASA’s Galileo came within 218 miles (351 kilometers) of the surface.

Europa is the sixth-largest moon in the solar system, slightly smaller than Earth’s moon. Scientists think a salty ocean lies below a miles-thick ice shell, sparking questions about potential conditions capable of supporting life underneath Europa’s surface.

This segment of the first image of Europa taken during this flyby by the spacecraft’s JunoCam (a public-engagement camera) zooms in on a swath of Europa’s surface north of the equator. Due to the enhanced contrast between light and shadow seen along the terminator (the nightside boundary), rugged terrain features are easily seen, including tall shadow-casting blocks, while bright and dark ridges and troughs curve across the surface. The oblong pit near the terminator might be a degraded impact crater.

With this additional data about Europa’s geology, Juno’s observations will benefit future missions to the Jovian moon, including the agency’s Europa Clipper. Set to launch in 2024, Europa Clipper will study the moon’s atmosphere, surface, and interior, with its main science goal being to determine whether there are places below Europa’s surface that could support life.

As exciting as Juno’s data will be, the spacecraft had only a two-hour window to collect it, racing past the moon with a relative velocity of about 14.7 miles per second (23.6 kilometers per second).

“It’s very early in the process, but by all indications Juno’s flyby of Europa was a great success,” said Scott Bolton, Juno principal investigator from Southwest Research Institute in San Antonio. “This first picture is just a glimpse of the remarkable new science to come from Juno’s entire suite of instruments and sensors that acquired data as we skimmed over the moon’s icy crust.”

During the flyby, the mission collected what will be some of the highest-resolution images of the moon (0.6 miles, or 1 kilometer, per pixel) and obtained valuable data on Europa’s ice shell structure, interior, surface composition, and ionosphere, in addition to the moon’s interaction with Jupiter’s magnetosphere.

“The science team will be comparing the full set of images obtained by Juno with images from previous missions, looking to see if Europa’s surface features have changed over the past two decades,” said Candy Hansen, a Juno co-investigator who leads planning for the camera at the Planetary Science Institute in Tucson, Arizona. “The JunoCam images will fill in the current geologic map, replacing existing low-resolution coverage of the area.”

Juno’s close-up views and data from its Microwave Radiometer (MWR) instrument will provide new details on how the structure of Europa’s ice varies beneath its crust. Scientists can use all this information to generate new insights into the moon, including data in the search for regions where liquid water may exist in shallow subsurface pockets.

Building on Juno’s observations and previous missions such as Voyager 2 and Galileo, NASA’s Europa Clipper mission, slated to arrive at Europa in 2030, will study the moon’s atmosphere, surface, and interior—with a goal to investigate habitability and better understand its global subsurface ocean, the thickness of its ice crust, and search for possible plumes that may be venting subsurface water into space.

The close flyby modified Juno’s trajectory, reducing the time it takes to orbit Jupiter from 43 to 38 days. The flyby also marks the second encounter with a Galilean moon during Juno’s extended mission. The mission explored Ganymede in June 2021 and is scheduled to make close flybys of Io, the most volcanic body in the solar system, in 2023 and 2024.

NASA’s Jet Propulsion Laboratory, a division of Caltech in Pasadena, California, manages the Juno mission for the principal investigator, Scott J. Bolton, of the Southwest Research Institute in San Antonio. Juno is part of NASA’s New Frontiers Program, which is managed at NASA’s Marshall Space Flight Center in Huntsville, Alabama, for the agency’s Science Mission Directorate in Washington. Lockheed Martin Space in Denver built and operates the spacecraft.


More information about Juno is available at:

https://www.nasa.gov/juno

and

https://www.missionjuno.swri.edu


Credit: NASA's Jet Propulsion Laboratory (JPL)

Release Date: September 29, 2022


#NASA #Astronomy #Space #Science #Jupiter #Planet #Europa #Moon #Ocean #Astrobiology #Biosignatures #Habitability #Radiation #Juno #Spacecraft #SolarSystem #Exploration #JPL #California #UnitedStates #STEM #Education

Wednesday, July 12, 2017

NASA's Juno Spacecraft Spots Jupiter's Great Red Spot


This enhanced-color image of Jupiter's Great Red Spot was created by citizen scientist Gerald EichstƤdt using data from the JunoCam imager on NASA's Juno spacecraft. | July 12, 2017: Images of Jupiter's Great Red Spot reveal a tangle of dark, veinous clouds weaving their way through a massive crimson oval. The JunoCam imager aboard NASA's Juno mission snapped pics of the most iconic feature of the solar system's largest planetary inhabitant during its Monday (July 10) flyby. The images of the Great Red Spot were downlinked from the spacecraft's memory on Tuesday and placed on the mission's JunoCam website Wednesday morning.

"For hundreds of years scientists have been observing, wondering and theorizing about Jupiter's Great Red Spot," said Scott Bolton, Juno principal investigator from the Southwest Research Institute in San Antonio. "Now we have the best pictures ever of this iconic storm. It will take us some time to analyze all the data from not only JunoCam, but Juno's eight science instruments, to shed some new light on the past, present and future of the Great Red Spot."

As planned by the Juno team, citizen scientists took the raw images of the flyby from the JunoCam site and processed them, providing a higher level of detail than available in their raw form. The citizen-scientist images, as well as the raw images they used for image processing, can be found at:

https://www.missionjuno.swri.edu/junocam/processing

"I have been following the Juno mission since it launched," said Jason Major, a JunoCam citizen scientist and a graphic designer from Warwick, Rhode Island. "It is always exciting to see these new raw images of Jupiter as they arrive. But it is even more thrilling to take the raw images and turn them into something that people can appreciate. That is what I live for."

Measuring in at 10,159 miles (16,350 kilometers) in width (as of April 3, 2017) Jupiter's Great Red Spot is 1.3 times as wide as Earth. The storm has been monitored since 1830 and has possibly existed for more than 350 years. In modern times, the Great Red Spot has appeared to be shrinking.

All of Juno's science instruments and the spacecraft's JunoCam were operating during the flyby, collecting data that are now being returned to Earth. Juno's next close flyby of Jupiter will occur on Sept. 1.

Juno reached perijove (the point at which an orbit comes closest to Jupiter's center) on July 10 at 6:55 p.m. PDT (9:55 p.m. EDT). At the time of perijove, Juno was about 2,200 miles (3,500 kilometers) above the planet's cloud tops. Eleven minutes and 33 seconds later, Juno had covered another 24,713 miles (39,771 kilometers), and was passing directly above the coiling, crimson cloud tops of the Great Red Spot. The spacecraft passed about 5,600 miles (9,000 kilometers) above the clouds of this iconic feature.

Juno launched on Aug. 5, 2011, from Cape Canaveral, Florida. During its mission of exploration, Juno soars low over the planet's cloud tops -- as close as about 2,100 miles (3,400 kilometers). During these flybys, Juno is probing beneath the obscuring cloud cover of Jupiter and studying its auroras to learn more about the planet's origins, structure, atmosphere and magnetosphere.

Early science results from NASA's Juno mission portray the largest planet in our solar system as a turbulent world, with an intriguingly complex interior structure, energetic polar aurora, and huge polar cyclones.

"These highly-anticipated images of Jupiter's Great Red Spot are the 'perfect storm' of art and science. With data from Voyager, Galileo, New Horizons, Hubble and now Juno, we have a better understanding of the composition and evolution of this iconic feature," said Jim Green, NASA's director of planetary science. "We are pleased to share the beauty and excitement of space science with everyone."

JPL manages the Juno mission for the principal investigator, Scott Bolton, of Southwest Research Institute in San Antonio. The Juno mission is part of the New Frontiers Program managed by NASA's Marshall Space Flight Center in Huntsville, Alabama, for the Science Mission Directorate. Lockheed Martin Space Systems, Denver, built the spacecraft. JPL is a division of Caltech in Pasadena.

More information on the Juno mission is available at:
https://www.nasa.gov/juno
http://missionjuno.org

More information on the Great Red Spot can be found at:
https://www.nasa.gov/feature/goddard/jupiter-s-great-red-spot-a-swirling-mystery
https://www.nasa.gov/feature/jupiter-s-great-red-spot-likely-a-massive-heat-source

More information on Jupiter can be found at:
https://www.nasa.gov/jupiter

Credit: NASA/JPL-Caltech/SwRI/MSSS/Gerald Eichstadt
Release Date: July 12, 2017


#NASA #Astronomy #Space #Science #Jupiter #Planet #Atmosphere #GreatRedSpot #GRS #Juno #Spacecraft #SwRI #JPL #Pasadena #California #UnitedStates #STEM #Education #CitizenScience