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Rock Sampled by NASA’s Perseverance Embodies Why Rover Came to Mars
The 24th sample taken by the six-wheeled scientist offers new clues about Jezero Crater and the lake it may have once held.
Analysis by instruments aboard NASA’s Perseverance Mars rover indicate that the latest rock core taken by the rover was awash in water for an extended period of time in the distant past, perhaps as part of an ancient Martian beach. Collected on March 11, the sample is the rover’s 24th – a tally that includes 21 sample tubes filled with rock cores, two filled with regolith (broken rock and dust), and one with Martian atmosphere.
“To put it simply, this is the kind of rock we had hoped to find when we decided to investigate Jezero Crater,” said Ken Farley, project scientist for Perseverance at Caltech in Pasadena, California. “Nearly all the minerals in the rock we just sampled were made in water; on Earth, water-deposited minerals are often good at trapping and preserving ancient organic material and biosignatures. The rock can even tell us about Mars climate conditions that were present when it was formed.”
The presence of these specific minerals is considered promising for preserving a rich record of an ancient habitable environment on Mars. Such collections of minerals are important for guiding scientists to the most valuable samples for eventual return to Earth with the Mars Sample Return campaign.
Edge of the Crater’s RimNicknamed “Bunsen Peak” for the Yellowstone National Park landmark, the rock – about 5.6 feet wide and 3.3 feet high (1.7 meters by 1 meter) – intrigued Perseverance scientists because the outcrop stands tall amid the surrounding terrain and has an interesting texture on one of its faces. They were also interested in Bunsen Peak’s vertical rockface, which offers a nice cross-section of the rock and, because it’s not flat-lying, is less dusty and therefore easier for science instruments to investigate.
Meet the 24th Martian sample collected by NASA’s Mars Perseverance rover – “Comet Geyser,” a sample taken from a region of Jezero Crater that is especially rich in carbonate, a mineral linked to habitability.Before taking the sample, Perseverance scanned the rock using the rover’s SuperCam spectrometers and the X-ray spectrometer PIXL, short for Planetary Instrument for X-ray Lithochemistry. Then the rover used the rotor on the end of its robotic arm to grind (or abrade) a portion of the surface and scanned the rock again. The results: Bunsen Peak looks to be composed of about 75% carbonate grains cemented together by almost pure silica.
“The silica and parts of the carbonate appear microcrystalline, which makes them extremely good at trapping and preserving signs of microbial life that might have once lived in this environment,” said Sandra Siljeström, a Perseverance scientist from the Research Institutes of Sweden (RISE) in Stockholm. “That makes this sample great for biosignature studies if returned to Earth. Additionally, the sample might be one of the older cores collected so far by Perseverance, and that is important because Mars was at its most habitable early in its history.” A potential biosignature is a substance or structure that could be evidence of past life but may also have been produced without the presence of life.
The Bunsen Peak sample is the third that Perseverance has collected while exploring the “Margin Unit,” a geologic area that hugs the inner edge of Jezero Crater’s rim.
This mosaic shows a rock called “Bunsen Peak” where NASA’s Perseverance Mars rover extracted its 21st rock core and abraded a circular patch to investigate the rock’s composition.NASA/JPL-Caltech/ASU/MSSS Perseverance’s CacheCam captured this image of the rover’s latest cored sample – taken from an intriguing rock called “Bunsen Peak” – on March 11. NASA/JPL-Caltech“We’re still exploring the margin and gathering data, but results so far may support our hypothesis that the rocks here formed along the shores of an ancient lake,” said Briony Horgan, a Perseverance scientist from Purdue University, in West Lafayette, Indiana. “The science team is also considering other ideas for the origin of the Margin Unit, as there are other ways to form carbonate and silica. But no matter how this rock formed, it is really exciting to get a sample.”
The rover is working its way toward the westernmost portion of the Margin Unit. At the base of Jezero Crater’s rim, a location nicknamed “Bright Angel” is of interest to the science team because it may offer the first encounter with the much older rocks that make up the crater rim. Once it’s done exploring Bright Angel, Perseverance will begin an ascent of several months to the rim’s top.
More About the MissionA key objective for Perseverance’s mission on Mars is astrobiology, including caching samples that may contain signs of ancient microbial life. The rover will characterize the planet’s geology and past climate, pave the way for human exploration of the Red Planet, and be the first mission to collect and cache Martian rock and regolith.
Subsequent NASA missions, in cooperation with ESA (European Space Agency), would send spacecraft to Mars to collect these sealed samples from the surface and return them to Earth for in-depth analysis.
The Mars 2020 Perseverance mission is part of NASA’s Moon to Mars exploration approach, which includes Artemis missions to the Moon that will help prepare for human exploration of the Red Planet.
NASA’s Jet Propulsion Laboratory, which is managed for the agency by Caltech, built and manages operations of the Perseverance rover.
For more about Perseverance:
https://mars.nasa.gov/mars2020/
News Media ContactsDC Agle
Jet Propulsion Laboratory, Pasadena, Calif.
818-393-9011
agle@jpl.nasa.gov
Karen Fox / Charles Blue
NASA Headquarters, Washington
301-286-6284 / 202-802-5345
karen.c.fox@nasa.gov / charles.e.blue@nasa.gov
2024-036
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How NASA Spotted El Niño Changing the Saltiness of Coastal Waters
New findings have revealed a coastal realm highly sensitive to changes in runoff and rainfall on land.
After helping stoke record heat in 2023 and drenching major swaths of the United States this winter, the current El Niño is losing steam this spring. Scientists have observed another way that the climate phenomenon can leave its mark on the planet: altering the chemistry of coastal waters.
A team at NASA’s Jet Propulsion Laboratory in Southern California used satellite observations to track the dissolved salt content, or salinity, of the global ocean surface for a decade, from 2011 to 2022. At the sea surface, salinity patterns can tell us a lot about how freshwater falls, flows, and evaporates between the land, ocean, and atmosphere – a process known as the water cycle.
The JPL team showed that year-to-year-variations in salinity near coastlines strongly correlate with El Niño Southern Oscillation (ENSO), the collective term for El Niño and its counterpart, La Niña. ENSO affects weather around the world in contrasting ways. El Niño, linked to warmer-than-average ocean temperatures in the equatorial Pacific, can lead to more rain and snowfall than normal in the southwestern U.S., as well as drought in Indonesia. These patterns are somewhat reversed during La Niña.
During the exceptional El Niño event of 2015, for example, the scientists traced a particularly distinct global water cycle effect: Less precipitation over land led to a decrease in river discharge on average, which in turn led to notably higher salinity levels in areas as far as 125 miles (200 kilometers) from shore.
Instruments in space can track how salinity varies by region and season. Using NASA satellite data, this map shows how monsoon rains and freshwater flowing into the Bay of Bengal keep it far less salty than the Arabian Sea to the west. (Areas of low and high salinity are shown in blue and yellow, respectively.)NASA’s Scientific Visualization Studio The Amazon River delivers millions of gallons of water to the ocean every second – enough to change global average surface salinity. A plume of low salinity water is shown here in dark blue, drifting away from the river mouth on ocean currents. The blue blob to the northwest is the Orinoco River plume.NASA’s Scientific Visualization StudioAt other times, the opposite was found: Areas with higher-than-normal rainfall over land saw increased river discharge, reducing salinity near those coasts.
“We’re able to show coastal salinity responding to ENSO on a global scale,” said lead author Severine Fournier, an ocean physicist at JPL.
The team found that salinity is at least 30 times more variable in these dynamic zones near coasts than in the open ocean. The link between rain, rivers, and salt is especially pronounced at the mouths of large river systems such as the Mississippi and Amazon, where freshwater plumes can be mapped from space as they gush into the ocean.
Salt as SignalWith global warming, researchers have been observing changes in the water cycle, including increases in extreme precipitation events and runoff. At the intersection of land and sea, coastal waters may be where the impacts are most detectable.
“Given the sensitivity to rainfall and runoff, coastal salinity could serve as a kind of bellwether, indicating other changes unfolding in the water cycle,” Fournier said.
She noted that some of the world’s coastal waters are not well studied, despite the fact that about 40% of the human population lives within about 60 miles (100 kilometers) of a coastline. One reason is that river gauges and other on-sitemonitors can be costly to maintain and cannot provide coverage of the whole planet, especially in more remote regions.
That’s where satellite instruments come in. Launched in 2011, the Aquarius mission made some of the first space-based global observations of sea surface salinity using extremely sensitive radiometers to detect subtle changes in the ocean’s microwave radiation emissions. Aquarius was a collaboration between NASA and Argentina’s space agency, CONAE (Comisión Nacional de Actividades Espaciales).
Today, two higher-resolution tools – the ESA (European Space Agency) Soil Moisture and Ocean Salinity (SMOS) mission and NASA’s Soil Moisture Active Passive (SMAP) mission – allow scientists to zoom to within 25 miles (40 kilometers) of coastlines.
Using data from all three missions, the researchers found that surface salinity in coastal waters reached a maximum global average (34.50 practical salinity units, or PSU) each March and fell to a minimum global average (34.34 PSU) around September. (PSU is roughly equal to parts per thousand grams of water.) River discharge, especially from the Amazon, drives this timing.
In the open ocean, the cycle is different, with surface salinity reaching a global average minimum (34.95 PSU) from February to April and a global average maximum (34.97 PSU) from July to October. The open ocean does not show as much variability between seasons or years because it contains a significantly larger volume of water and is less sensitive to river discharge and ENSO. Instead, changes are governed by planet-scale precipitation minus total global evaporation, plus other factors like large-scale ocean circulation.
The study was published in the journal Geophysical Research Letters.
NASA Analysis Sees Spike in 2023 Global Sea Level Due to El Niño NASA Analysis Finds Strong El Niño Could Bring Extra Floods This Winter News Media ContactsJane J. Lee / Andrew Wang
Jet Propulsion Laboratory, Pasadena, Calif.
818-354-0307 / 626-379-6874
jane.j.lee@jpl.nasa.gov / andrew.wang@jpl.nasa.gov
Written by Sally Younger
2024-035
Share Details Last Updated Apr 03, 2024 Related Terms Explore More 5 min read Rock Sampled by NASA’s Perseverance Embodies Why Rover Came to Mars Article 8 hours ago 9 min read Veronica T. Pinnick Put NASA’s PACE Mission through Its Paces Article 1 day ago 5 min read NASA’s Europa Clipper Survives and Thrives in ‘Outer Space’ on Earth Article 1 week agoNASA Invites Media to Annual FIRST Robotics Competition in Rocket City
2 min read
Preparations for Next Moonwalk Simulations Underway (and Underwater) Students from the Power Struck Girls Team 5965 – an all-girls FIRST Robotics team from the Academy of Our Lady high school in Marrero, Louisiana, and sponsored by NASA’s Stennis Space Center – make final engineering adjustments to their robot during the 2023 Rocket City Regional FIRST Robotics tournaments in Huntsville.NASA/Joel WallaceThe Rocket City Regional – Alabama’s annual For Inspiration and Recognition of Science and Technology (FIRST) Robotics Competition – is scheduled for Friday, April 5, through Saturday, April 6, at the Von Braun Center South Hall in Huntsville, Alabama, known as the Rocket City. This event is free for the public.
FIRST Robotics is a global robotics competition for students in grades 9-12. Teams are challenged to raise funds, design a team brand, hone teamwork skills, and build and program industrial-sized robots to play a difficult field game against competitors.
More than 1,000 high school students on 47 teams from 10 states and 4 countries will compete in a new robotics game called, “CRESCENDO.”
Opening ceremonies begin at 8:30 a.m. CDT followed by qualification matches on April 5 and April 6. The Friday awards ceremony will begin at 6 p.m., while the Saturday awards ceremony will begin at 2:30 p.m.
District and regional competitions – such as the Rocket City Regional – are held across the country during March and April, providing teams a chance to qualify for the 2024 FIRST Robotics Competition Championship events held in late April in Houston.
NASA and its Robotics Alliance Project provide grants for high school teams and support for FIRST Robotics competitions to address the critical national shortage of students pursuing STEM (Science, Technology, Engineering, and Mathematics) careers. This FIRST Robotics Competition, The Rocket City Regional, is supported by NASA’s Marshall Space Flight Center in Huntsville, Alabama, and NASA’s Office of STEM Engagement.
News media interested in covering this event should respond no later than 4 p.m. on Thursday, April 4 by contacting Taylor Goodwin at 256-544-0034 or taylor.goodwin@nasa.gov.
Learn more about the Rocket City Regional event.
Find more information about Marshall’s support for education programs:
https://www.nasa.gov/marshall/marshall-stem-engagement/
Taylor Goodwin
256-544-0034
Marshall Space Flight Center, Huntsville, Alabama
taylor.goodwin@nasa.gov
On Monday, April 8, NASA and its partners will celebrate the wonders of the total…
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A Robot Hopper to Explore the Moon’s Dangerous Terrain
Intuitive Machines recently had a major breakthrough, successfully becoming the first non-governmental entity to land on the Moon in February. At least the landing was partially successful – the company’s Odysseus lander ended up on its side, though its instruments and communication links remained at least partially functional. That mission, dubbed IM-1, was the first in a series of ambitious missions the company has planned. And they recently released a paper detailing features of a unique hopping robot that will hitch a ride on its next Moon mission.
Known as South Pole Hopper (or S.P. Hopper), the robot will be the first of a new class called µNova. Weighing in at only 35 kg and standing only 70 cm tall, this miniaturized craft is a stand-alone spacecraft that can operate entirely autonomously. It must do this to complete its mission of exploring the region around the permanently shadowed regions (PSRs) at the lunar south pole.
Specifically, the craft has four distinct objectives:
- Determine the geologic properties of a specific ridge at the south pole, including inside a PSR
- Determine the surface brightness temperatures of both areas bathed at least partially in the Sun’s rays and also in the PSR.
- Research the “surface roughness” and “thermal inertia” of the Moon’s regolith at its landing location.
- Determine how much hydrogen there is in the general area – with the understanding that, most likely, it will be tied up in water.
Credit – NASASpaceNews
None of those objectives individually require S.P. Hopper’s most notable feature – but it sure would be helpful to complete them – it can “hop” by thrusting itself off the lunar surface and landing in an area it chooses completely autonomously – even in a PSR. It can do so at an angle of up to 10 degrees, the company is quick to point out, given its recent difficulties with spacecraft angle.
The paper describes several technical features of the hopper – including the fact that it will use a wireless LTE system to communicate. To collect the data required for its mission, it has three main scientific instruments: a set of CMOS cameras, whose primary task is to help with autonomous navigation but can also send pictures back to Earth to be analyzed; the LRAD thermopile sensor system; designed to capture brightness measurements of the regolith, and the PLWS, a miniature neutron spectrometer, specifically designed to look for hydrogen in space.
However, perhaps the most interesting part of the paper details its flight plan. S. P. Hopper is designed to make 5 – possibly 6 – hops when it lands at the lunar south pole. The first will be a “commissioning hop” that will only traverse 20 m or so. Next will be a 100 m “proof of concept” hop that will demonstrate that a hopping robot is a viable mode of transportation on the Moon.
Following those initial flights, S. P. Hopper will fly about 300 m to the rim of Marston crater, part of the Shackleton – de Gerlache ridge. It will then fly into the crater itself, which is a PSR, and then fly back out to the ridge again. If there’s enough fuel left, Intuitive Machines plans a 6th exploratory flight to look at anything interesting in the vicinity.
Fraser discusses Intuitive Machine’s lunar landing.Currently, IM-2, the flight that will take S.P. Hopper to the South Pole, is scheduled for launch sometime this year. Given Intuitive Machine’s relative success with the Odysseus lander, there’s a lot of optimism about the success of this mission as well. For now, though, we’ll have to wait and see if the company can pull off an even more successful follow-on mission.
Learn More:
Martin et al – S.P. HOPPER: IN-SITU EXPLORATION OF THE SHACKLETON DE GERLACHE RIDGE
UT – NASA is Going Ahead With a Hopping Lander to Explore the Lunar Surface
UT – China’s Chang’e-7 Will Deploy a Hopper that Jumps into a Crater in Search of Water Ice
UT – Drones Could Help Map the Lunar Surface with Extreme Precision
Lead Image:
View of the S.P Hopper.
Credit – Martin et al.
The post A Robot Hopper to Explore the Moon’s Dangerous Terrain appeared first on Universe Today.
Inside a Week to Totality: Weather Prospects, Solar Activity and More
Looking at prospects for eclipse day and totality.
Have you picked out your site to observe the eclipse on April 8th? Next Monday, the shadow of the Moon crosses Mexico, the contiguous United States from Texas to Maine, and the Canadian Maritimes for the last time for this generation. And while over 30 million people live in the path of totality, millions more live within an easy day drive of the path. I’m expecting that many folks will decide to make a three-day weekend of it, and eclipse travel traffic will really pick up this coming Saturday, April 6th.
We’ve written previously on observing and safety in our big guide to the April 8th total solar eclipse, and the science campaigns underway to meet the eclipse.
So, what can we expect on the big day? While eclipses and celestial mechanics are a definite, not all eclipses are the same, as key variables both cosmic and terrestrial play a role in the experience.
Watching the WeatherOf course, the major question mark that everyone is watching is weather and cloud cover. As the day nears, weather models begin to merge and agree. While climate models typically favor clear skies in early April for the southwest portion of the track and clouds to the northeast, predictions now actually show a reverse trend for the afternoon of the 8th. This means clear skies for New England, and clouds (and perhaps, even afternoon storm and tornado warnings) to the south towards Texas. Keep in mind, a Nor’easter is also inbound for New England late this week… we actually opted to head to northern Maine early for this very reason. Good sites to check include Pivotal Weather, and NOAA’s cloud cover forecast. On eclipse day, we’re watching the GOES-East live view page on North America to see what’s actually occurring.
Cloud cover prospects of April 8th, versus the eclipse path. Credit: Pivotal Weather.It’s always tough to know if the Sun will be obscured by a cloud for the scant few minutes of totality days prior. Remember: you don’t need a pristine clear sky for a solar eclipse… just a good view of the Sun and Moon. April over North America can be a fickle month.
Sometimes, seeing the eclipsed Sun through thick fast-moving clouds can provide a memorable view. This was the case for us in 2017 when we caught the eclipse from PARI, North Carolina in the Smoky Mountains.
Solar ActivityWe’re now headed towards the peak of Solar Cycle No. 25, so expect the Sun to be active, come eclipse day. Sunspots rotating into view now will also be visible during the partial phases of the eclipse leading up to totality. The Sun is uncharacteristically quiet this week, but we do have a few sunspots rotating into view to add a photogenic look to the Sun.
Sunspot activity rotating into view as of April 3rd. NASA/ESA/SOHO The Corona’s AppearanceDid you know: long-time eclipse chasers can actually identify which eclipse a given photo is from… just from the appearance of the corona. Predictive Science Incorporated actually runs a forecast for the appearance of the corona come eclipse day, and it looks like we’re in for a memorable one:
The latest prediction for the appearance of the solar corona on eclipse day. Credit: Predictive Science Inc.Catching the International Space Station transiting the partially eclipsed Sun can be a memorable observation. ISS Transit Finder is a good site to predict transits of the station for a given location.
A transit of the ISS captured during the 2015 partial solar eclipse. Credit: Thierry Legault. Last Minute PlansMobility is key, come eclipse day. Plan your eclipse expedition like a heist, complete with a plan to go mobile and an escape route. Tales of totality are replete with stories of eclipse chasers driving down back roads and even taking off running on foot to stay ahead of incoming clouds.
Skywatching During TotalityThough totality is fleeting, do take about half a minute to stargaze. Jupiter and Venus will be visible, along with several +1st magnitude stars. Comet 12P Pons-Brooks is also at +4.5 magnitude in the constellation Aries, 25 degrees from the Sun. A well-placed outburst from this tempestuous comet could always vault it into binocular or even naked eye visibility.
Skywatching during totality. Credit: Stellarium. Animal Activity During TotalityFinally, keep an eye (and ear) out for any anomalous phenomena during totality. Temperatures may drop, roosters may crow, and nocturnal creatures may briefly emerge, fooled by the false twilight. In 2017, we faced a sudden onslaught of mosquitoes as midday darkness descended.
If you have the means, do make sure you’re in the path of totality come eclipse day. This one has a special significance for us, as it’s the only total solar eclipse that passes over our hometown of Mapleton, Maine in our lifetimes.
Good luck, safe travels to totality, and clear skies!
The post Inside a Week to Totality: Weather Prospects, Solar Activity and More appeared first on Universe Today.
Microsoft and Quantinuum’s quantum computer may be most reliable yet
Microsoft and Quantinuum’s quantum computer may be most reliable yet
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NASA’s Webb Probes an Extreme Starburst Galaxy
Amid a site teeming with new and young stars lies an intricate substructure.
A team of astronomers has used NASA’s James Webb Space Telescope to survey the starburst galaxy Messier 82 (M82). Located 12 million light-years away in the constellation Ursa Major, this galaxy is relatively compact in size but hosts a frenzy of star formation activity. For comparison, M82 is sprouting new stars 10 times faster than the Milky Way galaxy.
Led by Alberto Bolatto at the University of Maryland, College Park, the team directed Webb’s NIRCam (Near-Infrared Camera) instrument toward the starburst galaxy’s center, attaining a closer look at the physical conditions that foster the formation of new stars.
“M82 has garnered a variety of observations over the years because it can be considered as the prototypical starburst galaxy,” said Bolatto, lead author of the study. “Both NASA’s Spitzer and Hubble space telescopes have observed this target. With Webb’s size and resolution, we can look at this star-forming galaxy and see all of this beautiful, new detail.”
Image: M82 observed by the Hubble and Webb Telescopes On the left is the starburst galaxy M82 as observed by NASA’s Hubble Space Telescope in 2006. The small box at the galaxy’s core corresponds to the area captured so far by the NIRCam (Near-Infrared Camera) instrument on NASA’s James Webb Space Telescope. The red filaments as seen by Webb are the polycyclic aromatic hydrocarbon emission, which traces the shape of the galactic wind. In the Hubble image, light at .814 microns is colored red, .658 microns is red-orange, .555 microns is green, and .435 microns is blue (filters F814W, F658N, F555W, and F435W, respectively). In the Webb image, light at 3.35 microns is colored red, 2.50 microns is green, and 1.64 microns is blue (filters F335M, F250M, and F164N, respectively). NASA, ESA, CSA, STScI, A. Bolatto (University of Maryland) A Vibrant Community of StarsStar formation continues to maintain a sense of mystery because it is shrouded by curtains of dust and gas, creating an obstacle in observing this process. Fortunately, Webb’s ability to peer in the infrared is an asset in navigating these murky conditions. Additionally, these NIRCam images of the very center of the starburst were obtained using an instrument mode that prevented the very bright source from overwhelming the detector.
While dark brown tendrils of heavy dust are threaded throughout M82’s glowing white core even in this infrared view, Webb’s NIRCam has revealed a level of detail that has historically been obscured. Looking closer toward the center, small specks depicted in green denote concentrated areas of iron, most of which are supernova remnants. Small patches that appear red signify regions where molecular hydrogen is being lit up by a nearby young star’s radiation.
“This image shows the power of Webb,” said Rebecca Levy, second author of the study at the University of Arizona, Tucson. “Every single white dot in this image is either a star or a star cluster. We can start to distinguish all of these tiny point sources, which enables us to acquire an accurate count of all the star clusters in this galaxy.”
Finding Structure in Lively ConditionsLooking at M82 in slightly longer infrared wavelengths, clumpy tendrils represented in red can be seen extending above and below the galaxy’s plane. These gaseous streamers are a galactic wind rushing out from the core of the starburst.
One area of focus for this research team was understanding how this galactic wind, which is caused by the rapid rate of star formation and subsequent supernovae, is being launched and influencing its surrounding environment. By resolving a central section of M82, scientists could examine where the wind originates, and gain insight on how hot and cold components interact within the wind.
Webb’s NIRCam instrument was well-suited to trace the structure of the galactic wind via emission from sooty chemical molecules known as polycyclic aromatic hydrocarbons (PAHs). PAHs can be considered as very small dust grains that survive in cooler temperatures but are destroyed in hot conditions.
Much to the team’s surprise, Webb’s view of the PAH emission highlights the galactic wind’s fine structure – an aspect previously unknown. Depicted as red filaments, the emission extends away from the central region where the heart of star formation is located. Another unanticipated find was the similar structure between the PAH emission and that of hot, ionized gas.
“It was unexpected to see the PAH emission resemble ionized gas,” said Bolatto. “PAHs are not supposed to live very long when exposed to such a strong radiation field, so perhaps they are being replenished all the time. It challenges our theories and shows us that further investigation is required.”
Video: Tour of the M82 Image Credit: NASA’s Goddard Space Flight Center Lighting a Path ForwardWebb’s observations of M82 in near-infrared light spur further questions about star formation, some of which the team hopes to answer with additional data gathered with Webb, including that of another starburst galaxy. Two other papers from this team characterizing the stellar clusters and correlations among wind components of M82 are almost finalized.
In the near future, the team will have spectroscopic observations of M82 from Webb ready for their analysis, as well as complementary large-scale images of the galaxy and wind. Spectral data will help astronomers determine accurate ages for the star clusters and provide a sense of timing for how long each phase of star formation lasts in a starburst galaxy environment. On a broader scale, inspecting the activity in galaxies like M82 can deepen astronomers’ understanding of the early universe.
“Webb’s observation of M82, a target closer to us, is a reminder that the telescope excels at studying galaxies at all distances,” said Bolatto. “In addition to looking at young, high-redshift galaxies, we can look at targets closer to home to gather insight into the processes that are happening here – events that also occurred in the early universe.”
These findings have been accepted for publication in The Astrophysical Journal.The James Webb Space Telescope is the world’s premier space science observatory. Webb is solving mysteries in our solar system, looking beyond to distant worlds around other stars, and probing the mysterious structures and origins of our universe and our place in it. Webb is an international program led by NASA with its partners, ESA (European Space Agency) and the Canadian Space Agency.
DownloadsRight click the images in this article to open a larger version in a new tab/window.
Download full resolution images for this article from the Space Telescope Science Institute.
These findings have been accepted for publication in The Astrophysical Journal.
Laura Betz – laura.e.betz@nasa.gov, Rob Gutro – rob.gutro@nasa.gov
NASA’s Goddard Space Flight Center, Greenbelt, Md.
Christine Pulliam – cpulliam@stsci.edu
Space Telescope Science Institute, Baltimore, Md.
More about starburst galaxy M82
More Webb News – https://science.nasa.gov/mission/webb/latestnews/
More Webb Images – https://science.nasa.gov/mission/webb/multimedia/images/
Webb Mission Page – https://science.nasa.gov/mission/webb/
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ESA's solar eclipse maker, Proba-3
Hundreds of millions of people will witness next week’s total solar eclipse across North America, and solar physicists from around the globe are flocking to join them. Eclipses offer a brief glimpse of the Sun’s ghostly surrounding atmosphere – the solar corona – normally kept invisible by the Sun’s sheer glare. But the corona will soon be opened up for more sustained study: today in Belgium ESA has unveiled the pair of spacecraft making up its new Proba-3 mission, planned to produce orbital solar eclipse events on demand.