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

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

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

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

Monday, June 10, 2024

Planet Mars Auroras during Epic May 2024 Solar Storm | NASA MAVEN Mission

Planet Mars Auroras during Epic May 2024 Solar Storm | NASA MAVEN Mission

The purple color in this video shows auroras on Mars’ nightside as detected by the ultraviolet instrument aboard NASA’s MAVEN orbiter between May 14 and 20, 2024. The brighter the purple, the more auroras that were present. 

Auroras Over Mars: High above NASA's Mars Curiosity rover, NASA’s MAVEN (Mars Atmosphere and Volatile EvolutioN) orbiter captured another effect of the recent solar activity—glowing auroras over the planet. The way these auroras occur is different than those seen on Earth.

Our home planet is shielded from charged particles by a robust magnetic field. It normally limits auroras to regions near the poles. (Solar maximum is the reason behind the recent auroras seen as far south as Alabama.) Mars lost its internally generated magnetic field in the ancient past, so there is no protection from the barrage of energetic particles. When charged particles hit the Martian atmosphere, it results in auroras that engulf the entire planet.

During solar events, the Sun releases a wide range of energetic particles. Only the most energetic can reach the surface to be measured by RAD. Slightly less energetic particles, those that cause auroras, are sensed by MAVEN’s Solar Energetic Particle instrument.

Scientists can use that instrument’s data to rebuild a timeline of each minute as the solar particles screamed past, meticulously teasing apart how the event evolved.

“This was the largest solar energetic particle event that MAVEN has ever seen,” said MAVEN Space Weather Lead, Christina Lee of the University of California, Berkeley’s Space Sciences Laboratory. “There have been several solar events in past weeks, so we were seeing wave after wave of particles hitting Mars.”

The data coming in from NASA’s spacecraft won’t only help future planetary missions to the Red Planet. It is contributing to a wealth of information being gathered by the agency’s other heliophysics missions, including Voyager, Parker Solar Probe, and the forthcoming ESCAPADE (Escape and Plasma Acceleration and Dynamics Explorers) mission.

Targeting a late-2024 launch, ESCAPADE’s twin small satellites will orbit Mars and observe space weather from a unique dual perspective that is more detailed than what MAVEN can currently measure alone.

More About the Missions
MAVEN’s principal investigator is based at the Laboratory for Atmospheric and Space Physics (LASP) at the University of Colorado Boulder. LASP is also responsible for managing science operations and public outreach and communications. NASA’s Goddard Space Flight Center in Greenbelt, Maryland, manages the MAVEN mission. Lockheed Martin Space built the spacecraft and is responsible for mission operations. NASA’s Jet Propulsion Laboratory in Southern California provides navigation and Deep Space Network support. The MAVEN team is preparing to celebrate the spacecraft’s 10th year at Mars in September 2024.

Similarly, the star camera NASA’s 2001 Mars Odyssey orbiter uses for orientation was inundated with energy from solar particles, momentarily going out. (Odyssey has other ways to orient itself, and recovered the camera within an hour.) Even with the brief lapse in its star camera, the orbiter collected vital data on X-rays, gamma rays, and charged particles using its High-Energy Neutron Detector.

This was not Odyssey’s first brush with a solar flare. In 2003, solar particles from a solar flare that was ultimately estimated to be an X45 fried Odyssey’s radiation detector. Ironically, it was designed to measure such events.

NASA’s Goddard Space Flight Center in Greenbelt, Maryland, manages the MAVEN mission.

For more information on MAVEN, go to: https://science.nasa.gov/mission/maven/

Video Credit: NASA/University of Colorado/LASP
Duration: 17 seconds
Release Date: June 10, 2024

#NASA #Space #Astronomy #Science #Star #Sun #SolarMax #Planet #Mars #Atmosphere #Ultraviolet #Auroras #UV #Radiation #Astronauts #MAVENMission #MAVENSpacecraft #SolarSystem #SpaceExploration #GSFC #LASP #CUBoulder #UnitedStates #STEM #Education #HD #Video

Monday, May 13, 2024

Exploring Planet Uranus | NASA Goddard

Exploring Planet Uranus | NASA Goddard

In one of the least explored regions of our solar system, there is an ice giant that scientists believe can help us unlock some of the remaining mysteries of our universe. This video takes us on a journey there to explore planet Uranus, as well as its rings and moons, highlighting many fascinating features.

We also look back on what was discovered by NASA's Voyager 2 spacecraft, as well as subsequent findings by ground-based telescopes and the Hubble Space Telescope. The ongoing search for ocean worlds and life beyond Earth makes Uranus an exciting target for the James Webb Space Telescope and for future up-close exploration.


Video Credit: NASA’s Goddard Space Flight Center (GSFC)
Video Produced, Edited and Narrated by: David Ladd (Abacus Technology Corp)
Animations by NASA’s CI Labs:
Animators – Krystofer Kim (Rothe); Jenny McElligott (Rothe)
Art Director – Michael Lentz (ARES)
Manager – Walt Feimer (Rothe)
Duration: 3 minutes, 16 seconds
Release Date: May 13, 2024 


#NASA #ESA #Astronomy #Space #Science #SolarSystem #Planet #Uranus #IceGiant #Rings #Atmosphere #Moons #UranianSystem #Voyager2Spacecraft #HST #JWST #GSFC #STScI #UnitedStates #Europe #CSA #Canada #STEM #Education #Animation #HD #Video

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 #España #JPL #Caltech #California #History #UnitedStates #STEM #Education

Wednesday, January 17, 2024

Pan: Ring Spoke Season on Planet Saturn | Hubble Space Telescope

Pan: Ring Spoke Season on Planet Saturn | Hubble Space Telescope

This photo of Saturn was taken by the NASA/European Space Agency Hubble Space Telescope on Oct. 22, 2023, when the ringed planet was approximately 1,365 million kilometers from Earth. Hubble's ultra-sharp vision reveals a phenomenon called ring spokes.

Saturn's spokes are transient features that rotate along with the rings. Their ghostly appearance only persists for two or three rotations around Saturn. During active periods, freshly-formed spokes continuously add to the pattern.

In 1981, NASA's Voyager 2 first photographed the ring spokes. Hubble continues observing Saturn annually as the spokes come and go. This cycle has been captured by Hubble's Outer Planets Atmospheres Legacy (OPAL) program that began nearly a decade ago to annually monitor weather changes on all four gas-giant outer planets.

Hubble's crisp images show that the frequency of spoke apparitions is seasonally driven, first appearing in OPAL data in 2021 but only on the morning (left) side of the rings. Long-term monitoring shows that both the number and contrast of the spokes vary with Saturn's seasons. Saturn is tilted on its axis like Earth and has seasons lasting approximately seven years.

This year, these ephemeral structures appear on both sides of the planet simultaneously as they spin around the giant world. Although they look small compared with Saturn, their length and width can stretch longer than Earth's diameter!

The OPAL team notes that the leading theory is that spokes are tied to interactions between Saturn's powerful magnetic field and the sun. Planetary scientists think that electrostatic forces generated from this interaction levitate dust or ice above the ring to form the spokes, though after several decades no theory perfectly predicts the spokes. Continued Hubble observations may eventually help solve the mystery.


Video Credit: NASA, European Space Agency, STScI, A. Simon (NASA-GSFC), N. Bartmann

Duration: 30 seconds

Release Date: Jan. 17, 2023


#NASA #Hubble #Astronomy #Space #Science #Planet #Saturn #Rings #Spokes #SolarSystem #SpaceExploration #Voyager2Spacecraft #Cosmos #Universe #HST #HubbleSpaceTelescope #ESA #Europe #GSFC #STScI #UnitedStates #STEM #Education #HD #Video

Saturday, January 06, 2024

First NASA Artemis Robotic Launch to The Moon on New ULA Vulcan Rocket

First NASA Artemis Robotic Launch to The Moon on New ULA Vulcan Rocket

United Launch Alliance (ULA)'s first Vulcan Centaur launch vehicle (VC2S) was transported to Space Launch Complex-41 at Cape Canaveral Space Force Station, Florida, on January 5, 2024. For its first certification mission (Cert-1), Vulcan will launch Astrobotic's Peregrine Lunar Lander (Peregrine Mission One – PM1) and Celestis Memorial Spaceflights deep space Voyager mission (Enterprise Flight). They are currently targeting 2:18 a.m. EST Monday, Jan. 8, 2024, for the first commercial robotic launch to the Moon’s surface.

This launch is part of NASA’s Commercial Lunar Payload Services (CLPS) initiative and Artemis program. Carrying NASA science, liftoff of ULA’s Vulcan rocket and Astrobotic’s Peregrine lunar lander will happen from Launch Complex 41 at Cape Canaveral Space Force Station in Florida.

Launch of Astrobotic’s Peregrine Mission One will carry NASA and commercial payloads to study the lunar exosphere, thermal properties, and hydrogen abundance of the lunar regolith, magnetic fields, and the radiation environment of the lunar surface. 

Learn more about Astrobotic’s Peregrine Lunar Lander (Adobe PDF):

https://www.astrobotic.com/wp-content/uploads/2023/12/Peregrine-Launch_Info_Packet-Web-1.pdf

Learn about NASA's Commercial Lunar Payload Services (CLPS) - Astrobotic's Peregrine Mission One:

https://www.nasa.gov/commercial-lunar-payload-services/ 


Credit: NASA/Ben Smegelsky/United Launch Alliance

Acknowledgement: SciNews

Duration: 2 minutes

Release Date: Jan. 6, 2024


#NASA #Space #Astronomy #Science #ArtemisProgram #Moon #SouthPole #MonsMouton #WaterIce #Astrobotic #PeregrineLunarLander #Robotics #Engineering #SpaceTechnology #DeepSpace #SpaceExploration #SolarSystem #ULA #VulcanRocket #CLPS #Florida #UnitedStates #STEM #Education #HD #Video

Thursday, December 21, 2023

Planet Saturn | Hubble Space Telescope

Planet Saturn | Hubble Space Telescope

This photo of Saturn was taken by the NASA/European Space Agency Hubble Space Telescope on Oct. 22, 2023, when the ringed planet was approximately 1365 million kilometers from Earth. Hubble's ultra-sharp vision reveals a phenomenon called ring spokes.

Saturn's spokes are transient features that rotate along with the rings. Their ghostly appearance only persists for two or three rotations around Saturn. During active periods, freshly-formed spokes continuously add to the pattern.

In 1981, NASA's Voyager 2 first photographed the ring spokes. Hubble continues observing Saturn annually as the spokes come and go. This cycle has been captured by Hubble's Outer Planets Atmospheres Legacy (OPAL) program that began nearly a decade ago to annually monitor weather changes on all four gas-giant outer planets.

Hubble's crisp images show that the frequency of spoke apparitions is seasonally driven, first appearing in OPAL data in 2021 but only on the morning (left) side of the rings. Long-term monitoring shows that both the number and contrast of the spokes vary with Saturn's seasons. Saturn is tilted on its axis like Earth and has seasons lasting approximately seven years.

This year, these ephemeral structures appear on both sides of the planet simultaneously as they spin around the giant world. Although they look small compared with Saturn, their length and width can stretch longer than Earth's diameter!

The OPAL team notes that the leading theory is that spokes are tied to interactions between Saturn's powerful magnetic field and the sun. Planetary scientists think that electrostatic forces generated from this interaction levitate dust or ice above the ring to form the spokes, though after several decades no theory perfectly predicts the spokes. Continued Hubble observations may eventually help solve the mystery.


Image Credit: NASA, European Space Agency, STScI, A. Simon (NASA-GSFC)

Release Date: Dec. 21, 2023


#NASA #Hubble #Astronomy #Space #Science #Planet #Saturn #Rings #Spokes #SolarSystem #SpaceExploration #Voyager2Spacecraft #Cosmos #Universe #HST #HubbleSpaceTelescope #ESA #Europe #GSFC #STScI #UnitedStates #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

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

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, March 23, 2023

Planet Uranus: Nov. 2014 & Nov. 2022 | Hubble Space Telescope

Planet Uranus: Nov. 2014 & Nov. 2022 | Hubble Space Telescope

Planetary oddball Uranus rolls around the Sun on its side as it follows its 84-year orbit, rather than spinning in a more ’vertical’ position as Earth does. Its weirdly tilted ‘horizontal’ rotation axis is angled just eight degrees off the plane of the planet’s orbit. One recent theory proposes that Uranus once had a massive moon that gravitationally destabilized it and then crashed into it. Other possibilities include giant impacts during the formation of the planets, or even giant planets exerting resonant torques on each other over time. The consequences of Uranus’s tilt are that for stretches of time lasting up to 42 years, parts of one hemisphere are completely without sunlight. When the Voyager 2 spacecraft visited during the 1980s, the planet’s south pole was pointed almost directly at the Sun. Hubble’s latest view shows the northern pole now tipping toward the Sun.

[LEFT] - This is a Hubble view of Uranus taken in 2014, seven years after the northern spring equinox when the Sun was shining directly over the planet’s equator, and shows one of the first images from the OPAL program. Multiple storms with methane ice-crystal clouds appear at mid-northern latitudes above the planet’s cyan-tinted lower atmosphere. Hubble photographed the ring system edge-on in 2007, but the rings are seen starting to open up seven years later in this view. At this time, the planet had multiple small storms and even some faint cloud bands.

[RIGHT] - As seen in 2022, Uranus’s north pole shows a thickened photochemical haze that looks similar to the smog over cities. Several little storms can be seen near the edge of the polar haze boundary. Hubble has been tracking the size and brightness of the north polar cap and it continues to get brighter year after year. Astronomers are disentangling multiple effects—from atmospheric circulation, particle properties, and chemical processes—that control how the atmospheric polar cap changes with the seasons. At the Uranian equinox in 2007, neither pole was particularly bright. As the northern summer solstice approaches in 2028 the cap may grow brighter still, and will be aimed directly toward Earth, allowing good views of the rings and the north pole; the ring system will then appear face-on. This image was taken on November 10, 2022.

Image Description: Two views of the tipped planet Uranus appear side-by-side for comparison.


Credit: NASA, European Space Agency (ESA), STScI, A. Simon (NASA-GSFC), M. H. Wong (UC Berkeley), J. DePasquale (STScI)

Release Date: March 23, 2023


#NASA #ESA #Space #Astronomy #Science #Hubble #Planet #Jupiter #Moon #Io #SolarSystem #Exploration #HST #SpaceTelescope #GSFC #STScI #UnitedStates #Europe #Infographic #STEM #Education

Planet Jupiter & Io Moon: Nov. 2022 | Hubble Space Telescope

Planet Jupiter & Io Moon: Nov. 2022 | Hubble Space Telescope
The forecast for Jupiter is for stormy weather at low northern latitudes. A prominent string of alternating storms is visible, forming a ‘vortex street’ as some planetary astronomers call it. This is a wave pattern of nested cyclones and anticyclones, locked together like the alternating gears of a machine moving clockwise and counterclockwise. If the storms get close enough to each other and merge together, they could build an even larger storm, potentially rivalling the current size of the Great Red Spot. The staggered pattern of cyclones and anticyclones prevents individual storms from merging. Activity is also seen interior to these storms; in the 1990s Hubble did not see any cyclones or anticyclones with built-in thunderstorms, but these storms have sprung up in the last decade. Strong color differences indicate that Hubble is seeing different cloud heights and depths as well.

The orange moon Io photobombs this view of Jupiter’s multicolored cloud tops, casting a shadow toward the planet’s western limb. Hubble’s resolution is so sharp that it can see Io’s mottled-orange appearance, the result of its numerous active volcanoes. These volcanoes were first discovered when the Voyager 1 spacecraft flew by in 1979. The moon’s molten interior is overlaid by a thin crust through which the volcanoes eject material. Sulphur takes on various hues at different temperatures, which is why Io’s surface is so colorful. This photo was taken on November 12, 2022.

Image Description: Jupiter looms large in this image. Set against a black background, the planet is banded in stripes of brownish orange, light gray, soft yellow, and shades of cream. White and cream colored ovals punctuate the planet at all latitudes.

Credit: NASA, European Space Agency (ESA), Space Telescope Science Institute (STScI), A. Simon (NASA-GSFC), M. H. Wong (UC Berkeley), J. DePasquale (STScI)
Release Date: March 23, 2023

#NASA #ESA #Space #Astronomy #Science #Hubble #Planet #Jupiter #Moon #Io #SolarSystem #Exploration #HST #SpaceTelescope #GSFC #STScI #UnitedStates #Europe #STEM #Education

Tuesday, March 14, 2023

Jupiter's Moon Europa: Ocean Currents May Affect Rotation of Icy Crust | JPL

Jupiter's Moon Europa: Ocean Currents May Affect Rotation of Icy Crust | JPL

Research reveals a new explanation for how the icy shell of Jupiter’s moon Europa rotates at a different rate than its interior. NASA’s Europa Clipper Mission will take a closer look.

NASA scientists have strong evidence that Jupiter’s moon Europa has an internal ocean under its icy outer shell—an enormous body of salty water swirling around the moon’s rocky interior. New computer modeling suggests the water may actually be pushing the ice shell along, possibly speeding up and slowing down the rotation of the moon’s icy shell over time.

Image Description: This view of Jupiter’s icy moon Europa was captured by the JunoCam imager aboard NASA’s Juno spacecraft during the mission’s close flyby on Sept. 29, 2022. The agency’s Europa Clipper spacecraft will explore the moon when it reaches orbit around Jupiter in 2030. 

Scientists have known that Europa’s shell is probably free-floating, rotating at a different rate than the ocean below and the rocky interior. The new modeling is the first to show that Europa’s ocean currents could be contributing to the rotation of its icy shell.

A key element of the study involved calculating drag—the horizontal force that the moon’s ocean exerts on the ice above it. The research hints at how the power of the ocean flow and its drag against the ice layer could even account for some of the geology seen on Europa’s surface. Cracks and ridges could result from the icy shell slowly stretching and collapsing over time as it is pushed and tugged by the ocean currents.

“Before this, it was known through laboratory experiments and modeling that heating and cooling of Europa’s ocean may drive currents,” said Hamish Hay, a researcher at the University of Oxford and lead author of the study published in JGR: Planets. Hay performed the research while a postdoctoral research associate at NASA’s Jet Propulsion Laboratory in Southern California. “Now our results highlight a coupling between the ocean and the rotation of the icy shell that was never previously considered.”

It might even be possible, using measurements gathered by NASA’s upcoming Europa Clipper mission, to determine with precision how fast the icy shell rotates. When scientists compare images gathered by Europa Clipper with those captured in the past by NASA’s Galileo and Voyager missions, they will be able to examine locations of ice surface features and potentially determine if the position of the moon’s icy shell has changed over time.

For decades, planetary scientists have debated whether Europa’s icy shell might be rotating faster than the deep interior. However, rather than tying it to the ocean’s movement, scientists focused on an outside force: Jupiter. They theorized that as the gas giant’s gravity pulls on Europa, it also tugs on the moon’s shell and causes it to spin slightly faster.

“To me, it was completely unexpected that what happens in the ocean’s circulation could be enough to affect the icy shell. That was a huge surprise,” said co-author and Europa Clipper Project Scientist Robert Pappalardo of NASA's Jet Propulsion Laboratory (JPL). “And the idea that the cracks and ridges we see on Europa’s surface could be tied to the circulation of the ocean below—geologists don’t usually think, ‘Maybe it’s the ocean doing that.’”

Europa Clipper, now in its assembly, test, and launch operations phase at JPL, is set to launch in 2024. The spacecraft will begin orbiting Jupiter in 2030, and will use its suite of sophisticated instruments to gather science data as it flies by the moon about 50 times. The mission aims to determine if Europa, with its deep internal ocean, has conditions that could be suitable for life.

Download Europa Clipper Ocean World poster: go.nasa.gov/3Gsjzt5

Like a Pot of Water

Using techniques developed to study Earth’s ocean, the paper’s authors relied on NASA supercomputers to make large-scale models of Europa’s ocean. They explored the complexities of how the water circulates, and how heating and cooling affects that movement.

Scientists believe that Europa’s internal ocean is heated from below, due to radioactive decay and tidal heating within the moon’s rocky core. Like water heating in a pot on a stove, Europa’s warm water rises to the top of the ocean.

In the simulations, the circulation initially moved vertically, but the rotation of the moon as a whole caused the flowing water to veer in a more horizontal direction—in east-west and west-east currents. The researchers, by including drag in their simulations, were able to determine that if the currents are fast enough, there could be adequate drag on the ice above to speed up or slow down the shell’s rotation speed. The amount of interior heating—and thus, circulation patterns in the ocean—may change over time, potentially speeding up or slowing rotation of the icy shell above.

“The work could be important in understanding how other ocean worlds’ rotation speeds may have changed over time,” Hay said. “And now that we know about the potential coupling of interior oceans with the surfaces of these bodies, we may learn more about their geological histories as well as Europa’s.”

More information about Europa can be found here: europa.nasa.gov

More About the Mission

Europa Clipper’s main science goal is to determine whether there are places below the surface of Jupiter’s icy moon, Europa, that could support life. The mission’s three main science objectives are to understand the nature of the ice shell and the ocean beneath it, along with their composition and geology. The mission’s detailed exploration of Europa will help scientists better understand the astrobiological potential for habitable worlds beyond our planet.

Managed by Caltech in Pasadena, California, JPL leads the development of the Europa Clipper mission in partnership with the Johns Hopkins Applied Physics Laboratory (APL) in Laurel, Maryland, for NASA’s Science Mission Directorate in Washington. APL designed the main spacecraft body in collaboration with JPL and NASA’s Goddard Space Flight Center in Greenbelt, Maryland. The Planetary Missions Program Office at NASA’s Marshall Space Flight Center in Huntsville, Alabama, executes program management of the Europa Clipper mission.


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

Image Data: NASA/JPL-Caltech/SwRI/MSSS

Image Processing: Kevin M. Gill CC BY 3.0 Full Image Details

Release Date: March 13, 2023


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

Monday, February 20, 2023

Saturn's Rings & Titan Moon | NASA Cassini Mission

Saturn's Rings & Titan Moon | NASA Cassini Mission

Atlas is an inner satellite of Saturn which was discovered by Richard Terrile in 1980 from NASA Voyager spacecraft photos and was designated S/1980 S 28. In 1983, it was officially named after Atlas of Greek mythology, because it "holds the rings on its shoulders" like the Titan Atlas held the sky up above the Earth. The moon is also designated Saturn XV. Atlas has a roughly spherical center surrounded by a large and smooth equatorial ridge.
 
The Cassini spacecraft ended its mission on Sept. 15, 2017. Cassini's end involved a series of close Saturn passes, approaching within the rings, then an entry into Saturn's atmosphere to destroy the spacecraft. 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.

For more information about the Cassini-Huygens mission visit: https://saturn.jpl.nasa.gov and www.nasa.gov/cassini

The Cassini-Huygens mission was a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, California, managed the mission for NASA's Science Mission Directorate, Washington, D.C. 


Credit: NASA/Jet Propuslion Laboratory-Caltech/Space Science Institute (SSI)/Cassini Imaging Central Laboratory for Operations (CICLOPS)

Processing: Kevin M. Gill

Release Date: Feb. 17, 2023


#NASA #Astronomy #Science #Space #Saturn #Planet #Rings #Moon #Atlas #SaturnXV #SolarSystem #Exploration #Cassini #Spacecraft #JPL #California #UnitedStates #ESA #Europe #ASI #History #KevinGill #CitizenScience #STEM #Education

Saturday, February 18, 2023

Exploring the Solar System's Ice Giants | Johns Hopkins Applied Physics Laboratory

Exploring the Solar System's Ice Giants | Johns Hopkins Applied Physics Laboratory

The ice giants, Uranus and Neptune, are two of the solar system’s largest planets, yet they have hardly been explored. The only spacecraft to visit them was Voyager 2 more than 30 years ago

A mission to Uranus was prioritized in a recent study by the National Academies of Sciences. It would explore how Uranus formed, its interior structure, and its atmosphere.

It will solve mysteries about its rings and moons, including if some have liquid water oceans beneath their surfaces. Five of Uranus’ largest moons  show evidence of recent resurfacing, suggesting ongoing geologic activity. They may even have liquid water oceans under an ice shell, making them 'ocean worlds.'

Learn more about APL's research on ice giants: https://jhuapl.link/eho

Learn more about Uranus:

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

Learn more about Neptune:

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


Credit: Johns Hopkins Applied Physics Laboratory 

Duration: 1 minute

Release Date: Feb. 17, 2023


#NASA #Space #Astronomy #Science #SolarSystem #Planets #Uranus #Neptune #Spacecraft #Voyager2 #Exploration #Uranus #Neptune #IceGiants #Baltimore #Maryland #JHUAPL #UnitedStates #History #STEM #Education #HD #Video

Thursday, February 09, 2023

Saturn's Rings are Acting Strange | Hubble

Saturn's Rings are Acting Strange | Hubble

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.


Credit: NASA's Goddard Space Flight Center 

Paul Morris: Lead Producer 

Duration: 2 minutes, 38 seconds

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 #STEM #Education #HD #Video

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, October 06, 2022

Citizen Scientists Enhance New Europa Images from NASA’s Juno Spacecraft | JPL

Citizen Scientists Enhance New Europa Images from NASA’s Juno Spacecraft | JPL

Science enthusiasts have processed the new JunoCam images of Jupiter’s icy ocean moon, Europa, with results that are out of this world.

This view of Jovian moon Europa was created by processing an image JunoCam captured during Juno’s close flyby on Sept. 29, 2022. 

Citizen scientists have provided unique perspectives of the recent close flyby of Jupiter’s icy moon Europa by NASA’s Juno spacecraft. By processing raw images from JunoCam, the spacecraft’s public-engagement camera, members of the general public have created deep-space portraits of the Jovian moon that are not only awe-inspiring, but also worthy of further scientific scrutiny.

“Starting with our flyby of Earth back in 2013, Juno citizen scientists have been invaluable in processing the numerous images we get with Juno,” said Scott Bolton, Juno principal investigator from the Southwest Research Center in San Antonio. “During each flyby of Jupiter, and now its moons, their work provides a perspective that draws upon both science and art. They are a crucial part of our team, leading the way by using our images for new discoveries. These latest images from Europa do just that, pointing us to surface features that reveal details on how Europa works and what might be lurking both on top of the ice and below.”

Europa Up Close

JunoCam took its closest image at an altitude of 945 miles (1,521 kilometers) over a region of the moon called Annwn Regio. In the image, terrain beside the day-night boundary is revealed to be rugged, with pits and troughs. Numerous bright and dark ridges and bands stretch across a fractured surface, revealing the tectonic stresses that the moon has endured over millennia. The circular dark feature in the lower right is Callanish Crater.

Such JunoCam images help fill in gaps in the maps from images obtained by NASA’s Voyager and Galileo missions. Citizen scientist Björn Jónsson processed the image to enhance the color and contrast. The resolution is about 0.6 miles (1 kilometer) per pixel.

“Juno’s citizen scientists are part of a global united effort, which leads to both fresh perspectives and new insights,” said Candy Hansen, lead co-investigator for the JunoCam camera at the Planetary Science Institute in Tucson, Arizona. “Many times, citizen scientists will skip over the potential scientific applications of an image entirely, and focus on how Juno inspires their imagination or artistic sense, and we welcome their creativity.”

With a relative velocity of about 14.7 miles per second (23.6 kilometers per second), the Juno spacecraft only had a few minutes to collect data and images during its close flyby of Europa. As planned, the gravitational pull of the moon modified Juno’s trajectory, reducing the time it takes to orbit Jupiter from 43 to 38 days. The close approach 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.

Juno’s observations of Europa’s geology will not only contribute to our understanding of Europa, but also complement future missions to the Jovian moon. NASA’s Europa Clipper mission, set to launch in 2024, will study the moon’s atmosphere, surface, and interior, with a primary science goal to determine whether there are places below Europa’s surface that could support life.

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.

JunoCam’s raw images are available for the public to peruse and process into image products at:

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

More information about NASA citizen science can be found at:

https://science.nasa.gov/citizenscience

More information about Juno is available at:

https://www.nasa.gov/juno

and

https://www.missionjuno.swri.edu


Credits: 

Image data: NASA/JPL-Caltech/SwRI/MSSS

Image processing by Björn Jónsson CC BY-NC-SA 2.0

Release Date: October 6, 2022


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