mercredi 26 avril 2023

First direct image of a black hole expelling a powerful jet

 







ESO - European Southern Observatory logo.


April 26, 2023

A view of the jet and shadow of M87’s black hole

For the first time, astronomers have observed, in the same image, the shadow of the black hole at the centre of the galaxy Messier 87 (M87) and the powerful jet expelled from it. The observations were done in 2018 with telescopes from the Global Millimetre VLBI Array (GMVA), the Atacama Large Millimeter/submillimeter Array (ALMA), of which ESO is a partner, and the Greenland Telescope (GLT). Thanks to this new image, astronomers can better understand how black holes can launch such energetic jets.

Artist’s impression of the black hole in the M87 galaxy and its powerful jet

Most galaxies harbour a supermassive black hole at their centre. While black holes are known for engulfing matter in their immediate vicinity, they can also launch powerful jets of matter that extend beyond the galaxies that they live in. Understanding how black holes create such enormous jets has been a long standing problem in astronomy. “We know that jets are ejected from the region surrounding black holes,” says Ru-Sen Lu from the Shanghai Astronomical Observatory in China, “but we still do not fully understand how this actually happens. To study this directly we need to observe the origin of the jet as close as possible to the black hole.”

Messier 87 Captured by ESO’s Very Large Telescope

The new image published today shows precisely this for the first time: how the base of a jet connects with the matter swirling around a supermassive black hole. The target is the galaxy M87, located 55 million light-years away in our cosmic neighbourhood, and home to a black hole 6.5 billion times more massive than the Sun. Previous observations had managed to separately image the region close to the black hole and the jet, but this is the first time both features have been observed together. “This new image completes the picture by showing the region around the black hole and the jet at the same time,” adds Jae-Young Kim from the Kyungpook National University in South Korea and the Max Planck Institute for Radio Astronomy in Germany.

Anatomy of a Black Hole

The image was obtained with the GMVA, ALMA and the GLT, forming a network of radio-telescopes around the globe working together as a virtual Earth-sized telescope. Such a large network can discern very small details in the region around M87’s black hole.

Messier 87 in the Constellation of Virgo

The new image shows the jet emerging near the black hole, as well as what scientists call the shadow of the black hole. As matter orbits the black hole, it heats up and emits light. The black hole bends and captures some of this light, creating a ring-like structure around the black hole as seen from Earth. The darkness at the centre of the ring is the black hole shadow, which was first imaged by the Event Horizon Telescope (EHT) in 2017. Both this new image and the EHT one combine data taken with several radio-telescopes worldwide, but the image released today shows radio light emitted at a longer wavelength than the EHT one: 3.5 mm instead of 1.3 mm. “At this wavelength, we can see how the jet emerges from the ring of emission around the central supermassive black hole,” says Thomas Krichbaum of the Max Planck Institute for Radio Astronomy.

The size of the ring observed by the GMVA network is roughly 50% larger in comparison to the Event Horizon Telescope image. "To understand the physical origin of the bigger and thicker ring, we had to use computer simulations to test different scenarios,” explains Keiichi Asada from the Academia Sinica in Taiwan. The results suggest the new image reveals more of the material that is falling towards the black hole than what could be observed with the EHT.

First image of a black hole expelling a powerful jet (ESOcast 260 Light)

These new observations of M87’s black hole were conducted in 2018 with the GMVA, which consists of 14 radio-telescopes in Europe and North America [1]. In addition, two other facilities were linked to the GMVA: the Greenland Telescope and ALMA, of which ESO is a partner. ALMA consists of 66 antennas in the Chilean Atacama desert, and it played a key role in these observations. The data collected by all these telescopes worldwide are combined using a technique called interferometry, which synchronises the signals taken by each individual facility. But to properly capture the actual shape of an astronomical object it’s important that the telescopes are spread all over the Earth. The GMVA telescopes are mostly aligned East-to-West, so the addition of ALMA in the Southern hemisphere proved essential to capture this image of the jet and shadow of M87’s black hole. “Thanks to ALMA’s location and sensitivity, we could reveal the black hole shadow and see deeper into the emission of the jet at the same time,” explains Lu.

Zooming in on the black hole and jet of Messier 87

Future observations with this network of telescopes will continue to unravel how supermassive black holes can launch powerful jets. “We plan to observe the region around the black hole at the centre of M87 at different radio wavelengths to further study the emission of the jet,” says Eduardo Ros from the Max Planck Institute for Radio Astronomy. Such simultaneous observations would allow the team to disentangle the complicated processes that happen near the supermassive black hole. “The coming years will be exciting, as we will be able to learn more about what happens near one of the most mysterious regions in the Universe,” concludes Ros.

Notes

[1] The Korean VLBI Network is now also part of the GMVA, but did not participate in the observations reported here.

More information

This research was presented in the paper "A ring-like accretion structure in M87 connecting its black hole and jet" to appear in Nature (doi: https://www.nature.com/articles/s41586-023-05843-w).

The team is composed of Ru-Sen Lu (Shanghai Astronomical Observatory, People’s Republic of China [Shanghai]; Key Laboratory of Radio Astronomy, People’s Republic of China [KLoRA]; Max-Planck-Institut für Radioastronomie, Germany [MPIfR]), Keiichi Asada (Institute of Astronomy and Astrophysics, Academia Sinica, Taiwan, ROC [IoAaA]), Thomas P. Krichbaum (MPIfR), Jongho Park (IoAaA;  Korea Astronomy and Space Science Institute, Republic of Korea [KAaSSI]), Fumie Tazaki (Simulation Technology Development Department, Tokyo Electron Technology Solutions Ltd., Japan; Mizusawa VLBI Observatory, National Astronomical Observatory of Japan, Japan [Mizusawa]), Hung-Yi Pu (Department of Physics, National Taiwan Normal University, Taiwan, ROC; IoAaA; Center of Astronomy and Gravitation, National Taiwan Normal University, Taiwan, ROC), Masanori Nakamura (National Institute of Technology, Hachinohe College, Japan; IoAaA), Andrei Lobanov (MPIfR), Kazuhiro Hada (Mizusawa; Department of Astronomical Science, The Graduate University for Advanced Studies, Japan), Kazunori Akiyama (Black Hole Initiative at Harvard University, USA; Massachusetts Institute of Technology Haystack Observatory, USA [Haystack]; National Astronomical Observatory of Japan, Japan [NAOoJ]), Jae-Young Kim (Department of Astronomy and Atmospheric Sciences, Kyungpook National University, Republic of Korea; KAaSSI; MPIfR), Ivan Marti-Vidal (Departament d’Astronomia i Astrofísica, Universitat de València, Spain; Observatori Astronòmic, Universitat de València, Spain), Jose L. Gomez (Instituto de Astrofísica de Andalucía-CSIC, Spain [IAA]), Tomohisa Kawashima (Institute for Cosmic Ray Research, The University of Tokyo, Japan), Feng Yuan (Shanghai; Key Laboratory for Research in Galaxies and Cosmology, Chinese Academy of Sciences, People’s Republic of China; School of Astronomy and Space Sciences, University of Chinese Academy of Sciences, People’s Republic of China [SoAaSS]), Eduardo Ros (MPIfR), Walter Alef (MPIfR), Silke Britzen (MPIfR), Michael Bremer (Institut de Radioastronomie Millimétrique, France [IRAMF]), Avery E. Broderick (Department of Physics and Astronomy, University of Waterloo, Canada [Waterloo]; Waterloo Centre for Astrophysics, University of Waterloo, Canada; Perimeter Institute for Theoretical Physics, Canada), Akihiro Doi (The Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, Japan; Department of Space and Astronautical Science, SOKENDAI, Japan [SOKENDAI]), Gabriele Giovannini (Dipartimento di Fisica e Astronomia, Università di Bologna, Italy; Istituto di Radio Astronomia, INAF, Bologna, Italy [INAF]), Marcello Giroletti (INAF), Paul T. P. Ho (IoAaA), Mareki Honma (Mizusawa; Hachinohe; Department of Astronomy, The University of Tokyo, Japan), David H. Hughes (Instituto Nacional de Astrofísica, Mexico), Makoto Inoue (IoAaA), Wu Jiang (Shanghai), Motoki Kino (NAOoJ; Kogakuin University of Technology and Engineering, Japan), Shoko Koyama (Niigata University, Japan; IoAaA), Michael Lindqvist (Department of Space, Earth and Environment, Chalmers University of Technology, Sweden [Chalmers]), Jun Liu (MPIfR), Alan P. Marscher (Institute for Astrophysical Research, Boston University, USA), Satoki Matsushita (IoAaA), Hiroshi Nagai (NAOoJ; SOKENDAI), Helge Rottmann (MPIfR), Tuomas Savolainen (Department of Electronics and Nanoengineering, Aalto University, Finland; Metsähovi Radio Observatory, Finland [Metsähovi]; MPIfR), Karl-Friedrich Schuster (IRAMF), Zhi-Qiang Shen (Shanghai; KLoRA), Pablo de Vicente (Observatorio de Yebes, Spain [Yebes]), R. Craig Walker (National Radio Astronomy Observatory, Socorro, USA), Hai Yang (Shanghai; SoAaSS), J. Anton Zensus (MPIfR), Juan Carlos Algaba (Department of Physics, Universiti Malaya, Malaysia), Alexander Allardi (University of Vermont, USA), Uwe Bach (MPIfR), Ryan Berthold (East Asian Observatory, USA [EAO]), Dan Bintley (EAO), Do-Young Byun (KAaSSI; University of Science and Technology, Daejeon, Republic of Korea), Carolina Casadio (Institute of Astrophysics, Heraklion, Greece; Department of Physics, University of Crete, Greece), Shu-Hao Chang (IoAaA), Chih-Cheng Chang (National Chung-Shan Institute of Science and Technology, Taiwan, ROC [Chung-Shan]), Song-Chu Chang (Chung-Shan), Chung-Chen Chen (IoAaA), Ming-Tang Chen (Institute of Astronomy and Astrophysics, Academia Sinica, USA [IAAAS]), Ryan Chilson (IAAAS), Tim C. Chuter (EAO), John Conway (Chalmers), Geoffrey B. Crew (Haystack), Jessica T. Dempsey (EAO; Astron, The Netherlands [Astron]), Sven Dornbusch (MPIfR), Aaron Faber (Western University, Canada), Per Friberg (EAO), Javier González García (Yebes), Miguel Gómez Garrido (Yebes), Chih-Chiang Han (IoAaA), Kuo-Chang Han (System Development Center, National Chung-Shan Institute of Science and Technology, Taiwan, ROC), Yutaka Hasegawa (Osaka Metropolitan University, Japan [Osaka]), Ruben Herrero-Illana (European Southern Observatory, Chile), Yau-De Huang (IoAaA), Chih-Wei L. Huang (IoAaA), Violette Impellizzeri (Leiden Observatory, the Netherlands; National Radio Astronomy Observatory, Charlottesville, USA [NRAOC]), Homin Jiang (IoAaA), Hao Jinchi (Electronic Systems Research Division, National Chung-Shan Institute of Science and Technology, Taiwan, ROC), Taehyun Jung (KAaSSI), Juha Kallunki (Metsähovi), Petri Kirves (Metsähovi), Kimihiro Kimura (Japan Aerospace Exploration Agency, Japan), Jun Yi Koay (IoAaA), Patrick M. Koch (IoAaA), Carsten Kramer (IRAMF), Alex Kraus (MPIfR), Derek Kubo (IAAAS), Cheng-Yu Kuo (National Sun Yat-Sen University, Taiwan, ROC), Chao-Te Li (IoAaA), Lupin Chun-Che Lin (Department of Physics, National Cheng Kung University, Taiwan, ROC ), Ching-Tang Liu (IoAaA), Kuan-Yu Liu (IoAaA), Wen-Ping Lo (Department of Physics, National Taiwan University, Taiwan, ROC; IoAaA), Li-Ming Lu (Chung-Shan), Nicholas MacDonald (MPIfR), Pierre Martin-Cocher (IoAaA), Hugo Messias (Joint ALMA Observatory, Chile; Osaka), Zheng Meyer-Zhao (Astron; IoAaA), Anthony Minter (Green Bank Observatory, USA), Dhanya G. Nair (Astronomy Department, Universidad de Concepción, Chile), Hiroaki Nishioka (IoAaA), Timothy J. Norton (Center for Astrophysics | Harvard & Smithsonian, USA [CfA]), George Nystrom (IAAAS), Hideo Ogawa (Osaka), Peter Oshiro (IAAAS), Nimesh A. Patel (CfA), Ue-Li Pen (IoAaA), Yurii Pidopryhora (MPIfR; Argelander-Institut für Astronomie, Universität Bonn, Germany), Nicolas Pradel (IoAaA), Philippe A. Raffin (IAAAS), Ramprasad Rao (CfA), Ignacio Ruiz (Institut de Radioastronomie Millimétrique, Granada, Spain [IRAMS]), Salvador Sanchez (IRAMS), Paul Shaw (IoAaA), William Snow (IAAAS), T. K. Sridharan (NRAOC; CfA), Ranjani Srinivasan (CfA; IoAaA), Belén Tercero (Yebes), Pablo Torne (IRAMS), Thalia Traianou (IAA; MPIfR), Jan Wagner (MPIfR), Craig Walther (EAO), Ta-Shun Wei (IoAaA), Jun Yang (Chalmers), Chen-Yu Yu (IoAaA).

This research has made use of data obtained with the Global Millimeter VLBI Array (GMVA), which consists of telescopes operated by the Max-Planck-Institut für Radioastronomie (MPIfR), Institut de Radioastronomie Millimétrique (IRAM), Onsala Space Observatory (OSO), Metsähovi Radio Observatory (MRO), Yebes, the Korean VLBI Network (KVN), the Green Bank Telescope (GBT) and the Very Long Baseline Array (VLBA).

The Atacama Large Millimeter/submillimeter Array (ALMA), an international astronomy facility, is a partnership of ESO, the U.S. National Science Foundation (NSF) and the National Institutes of Natural Sciences (NINS) of Japan in cooperation with the Republic of Chile. ALMA is funded by ESO on behalf of its Member States, by NSF in cooperation with the National Research Council of Canada (NRC) and the National Science and Technology Council (NSTC) in Taiwan and by NINS in cooperation with the Academia Sinica (AS) in Taiwan and the Korea Astronomy and Space Science Institute (KASI). ALMA construction and operations are led by ESO on behalf of its Member States; by the National Radio Astronomy Observatory (NRAO), managed by Associated Universities, Inc. (AUI), on behalf of North America; and by the National Astronomical Observatory of Japan (NAOJ) on behalf of East Asia. The Joint ALMA Observatory (JAO) provides the unified leadership and management of the construction, commissioning and operation of ALMA.

The Greenland Telescope (GLT) retrofit, rebuild, and operation are led by the Academia Sinica, Institute of Astronomy and Astrophysics (ASIAA) and the Smithsonian Astrophysical Observatory (SAO).

The European Southern Observatory (ESO) enables scientists worldwide to discover the secrets of the Universe for the benefit of all. We design, build and operate world-class observatories on the ground — which astronomers use to tackle exciting questions and spread the fascination of astronomy — and promote international collaboration in astronomy. Established as an intergovernmental organisation in 1962, today ESO is supported by 16 Member States (Austria, Belgium, the Czech Republic, Denmark, France, Finland, Germany, Ireland, Italy, the Netherlands, Poland, Portugal, Spain, Sweden, Switzerland and the United Kingdom), along with the host state of Chile and with Australia as a Strategic Partner. ESO’s headquarters and its visitor centre and planetarium, the ESO Supernova, are located close to Munich in Germany, while the Chilean Atacama Desert, a marvellous place with unique conditions to observe the sky, hosts our telescopes. ESO operates three observing sites: La Silla, Paranal and Chajnantor. At Paranal, ESO operates the Very Large Telescope and its Very Large Telescope Interferometer, as well as survey telescopes such as VISTA. Also at Paranal ESO will host and operate the Cherenkov Telescope Array South, the world’s largest and most sensitive gamma-ray observatory. Together with international partners, ESO operates ALMA on Chajnantor, a facility that observes the skies in the millimetre and submillimetre range. At Cerro Armazones, near Paranal, we are building “the world’s biggest eye on the sky” — ESO’s Extremely Large Telescope. From our offices in Santiago, Chile we support our operations in the country and engage with Chilean partners and society.
 
Links:

Research paper: https://www.eso.org/public/archives/releases/sciencepapers/eso2305/eso2305a.pdf

Photos of ALMA: https://www.eso.org/public/images/archive/category/alma/

For journalists: subscribe to receive our releases under embargo in your language: https://www.eso.org/public/outreach/pressmedia/#epodpress_form

For scientists: got a story? Pitch your research: http://www.eso.org/sci/publications/announcements/sciann17463.html

Images Credit: R.-S. Lu (SHAO), E. Ros (MPIfR), S. Dagnello (NRAO/AUI/NSF)/S. Dagnello (NRAO/AUI/NSF)/ESO/IAU and Sky & Telescope/Videos Credits: ESO/L. Calçada, M. Kornmesser, Digitized Sky Survey 2, ESA/Hubble, RadioAstron, De Gasperin et al., Kim et al., S. Dagnello (NRAO/AUI/NSF), R. S. Lu (SHAO), E. Ros and H. Rottmann/MPIfR,  Nicolle R. Fuller/NSF, A. Duro/ESO/L. Calçada, Digitized Sky Survey 2, ESA/Hubble, RadioAstron, De Gasperin et al., Kim et al., R.-S. Lu (SHAO), E. Ros (MPIfR), S. Dagnello (NRAO/AUI/NSF). Music: astral electronic/Text Credits: ESO/Juan Carlos Muñoz Mateos/National Astronomical Observatory of Japan/Kazuhiro Hada/Max-Planck-Institut für Radioastronomie/Thomas P. Krichbaum/Institute of Astronomy and Astrophysics, Academia Sinica/Keiichi Asada/Shanghai Astronomical Observatory, Chinese Academy of Sciences/Ru-Sen Lu.

Best regards, Orbiter.ch


ispace fails to land on the Moon

 







ispace - Hakuto-R Lunar Lander Mission logo.


April 26, 2023

The craft of a Japanese start-up, which was trying to become the first private company to successfully land on the Moon, probably crashed during a “brutal Moon landing”.

Image above: The disappointment is immense for the ispace team. Image Credit: REUTERS

“It has been concluded that there is a high probability that the lander ultimately made a hard landing on the surface” of Earth's natural satellite, ispace said in a statement on Tuesday, indicating that the engineers of the start -up are working to understand the reasons for this failure. The start-up had announced earlier that it had lost contact with the craft when it was scheduled to land.

The Hakuto-R program lander, which had been in orbit some 100 kilometers above the Moon for a month, had begun its descent to the lunar surface about an hour earlier. A complex maneuver that was performed entirely automatically.


Video above: ispace CEO Takeshi Hakamada assumes his company's cargo lander crashed into the moon. The Japanese lunar company lost communication at the "very end" of the landing attempt today and is investigating. "We are very proud" of Mission 1 achievements.

Everything seemed to be going according to plan, but after the planned moment of landing, around 4:40 p.m. GMT on Tuesday (6:40 p.m. in Switzerland), several tens of minutes of anxious waiting followed, during which the company's teams tried to re-establish communication with the lander, in vain.

"Even though we don't think we can make the moon landing this time, we believe that this mission has proven to be of great importance, thanks to the acquisition of a lot of data and experience," said the boss and founder. of the start-up Takeshi Hakamada. “What is important is to use this knowledge and learning for Mission 2 and beyond,” he added.


Hakuto-R lander crash on the Moon. Illustration by India Today

The start-up is preparing two new missions to try to land on the Moon, and this setback will not change anything, defended the boss of ispace.

The success of this mission was far from guaranteed. In April 2019, the Israeli organization SpaceIL saw its probe crash into the surface of the Moon. So far, only the United States, Russia and China have managed to land robots on the Moon, located about 384,400 km from Earth. India had also tried in 2019 to land a probe, named Vikram, but it crashed.

Rovers on board

Measuring 2 by 2.5 meters, the lander was launched in December from the US base at Cape Canaveral, Florida, aboard a SpaceX rocket. It carried several small lunar vehicles, including a miniature Japanese model developed by the Japanese Space Agency in collaboration with toymaker Takara Tomy. Another lunar vehicle (“rover”) built by the United Arab Emirates was also on board.

This Gulf country, a newcomer to the space race, sent an orbital probe to Mars in 2021. If its small 10-kilo vehicle, named Rashid, had succeeded in being deployed, it would have carried out the first lunar mission of the Arab World.

The Japanese firm's Hakuto ("white rabbit" in Japanese) project was one of five finalists in the international Google Lunar XPrize competition, which ended without a winner, no company having managed to land a robot before the date set (2018). Two other companies, American companies Astrobotic and Intuitive Machines, are due to take off later this year in an attempt to land on the Moon.

HAKUTO-R M1 Moon landing

These missions are carried out in partnership with NASA, which intends to develop the lunar economy and has commissioned private companies to transport equipment and scientific experiments to the Moon.

The American space agency plans, with its Artemis program, to re-land astronauts on the lunar surface in the coming years, to establish a base there, and to build a space station in orbit around the Moon. Japan and the United States announced last year that they would cooperate to send a Japanese astronaut to the Moon by the end of the decade.

Related articles:

ispace - Moon lander targeting April 25 for historic touchdown try
https://orbiterchspacenews.blogspot.com/2023/04/ispace-moon-lander-targeting-april-25.html

Hakuto-R spacecraft sends a stunning image from the orbit of the Moon
https://orbiterchspacenews.blogspot.com/2023/04/hakuto-r-spacecraft-sends-stunning.html

ispace - Private Japanese Moon lander Hakuto-R reaches lunar orbit
https://orbiterchspacenews.blogspot.com/2023/03/ispace-private-japanese-moon-lander.html

ESA ground stations to support first commercial Moon landing
https://orbiterchspacenews.blogspot.com/2023/03/esa-ground-stations-to-support-first.html

ESA to touch Moon from wheels of UAE Rashid rover
https://orbiterchspacenews.blogspot.com/2023/01/esa-to-touch-moon-from-wheels-of-uae.html

ispace - Hakuto-R Lunar Lander Successfully Performs Maneuver
https://orbiterchspacenews.blogspot.com/2023/01/ispace-hakuto-r-lunar-lander.html

NASA’s Lunar Flashlight Has Launched – Follow the Mission in Real Time
https://orbiterchspacenews.blogspot.com/2022/12/nasas-lunar-flashlight-has-launched.html

SpaceX - Falcon 9 launches HAKUTO-R M1 and Lunar Flashlight
https://orbiterchspacenews.blogspot.com/2022/12/spacex-falcon-9-launches-hakuto-r-m1.html

Related links:

ispace: https://ispace-inc.com/

HAKUTO-R M1 Mission: https://ispace-inc.com/m1

Emirates Lunar Mission: https://en.wikipedia.org/wiki/Emirates_Lunar_Mission

Images (mentioned), Videos, Text, Credits: ispace/AFP/SciNews/Orbiter.ch Aerospace/Roland Berga.

Greetings, Orbiter.ch

Spacewalk Preps and Science Cleaning Aboard Station on Tuesday

 







ISS - Expedition 69 Mission patch.


April 26, 2023

Four Expedition 69 astronauts aboard the International Space Station worked throughout Tuesday preparing for a spacewalk and cleaning space biology hardware. Meanwhile, the orbiting lab’s three cosmonauts had an off-duty day following several days of their own spacewalk preparations.

Image above: Expedition 69 Flight Engineers (from left) Stephen Bowen and Sultan Alneyadi prepare their spacesuits for an upcoming spacewalk to continue station power upgrades. Image Credit: NASA.

Flight Engineers Stephen Bowen of NASA and Sultan Alneyadi of UAE (United Arab Emirates) spent Tuesday configuring their Extravehicular Mobility Units, or spacesuits, to get ready for a spacewalk set for 9:15 a.m. EDT on Friday. The duo also organized their spacewalking tools and inspected the tethers that will keep the spacewalkers safely attached to the station. The pair were joined in the afternoon by NASA Flight Engineers Woody Hoburg and Frank Rubio reviewing spacewalk procedures with mission controllers on the ground. The two spacewalkers will spend about six-and-a-half hours in the vacuum of space continuing the process of upgrading the station’s power generation system.

Hoburg and Rubio began their day deactivating and cleaning space biology hardware inside the Kibo laboratory module. The pair disconnected power cables and wiped down the Cell Biology Experiment Facility, a research incubator that housed samples that have since returned to Earth for analysis aboard the SpaceX Dragon cargo craft.

International Space Station (ISS). Animation Credit: ESA

Three cosmonauts are relaxing today after a busy period getting ready for a spacewalk that was originally planned for Tuesday. Roscosmos mission controllers opted to postpone the spacewalk for a few more days and continue studying the procedures necessary to move an experiment airlock from the Rassvet module to the Nauka science module. Commander Sergey Prokopyev and Flight Engineer Dmitri Petelin will exit the Poisk airlock in their Orlan spacesuits to perform the logistics spacewalk. Flight Engineer Andrey Fedyaev will assist the spacewalkers from inside the station and operate the European robotic arm with the experiment airlock in its grip.

Related links:

Expedition 69: https://www.nasa.gov/mission_pages/station/expeditions/expedition69/index.html

Kibo laboratory module: https://www.nasa.gov/mission_pages/station/structure/elements/japan-kibo-laboratory

Cell Biology Experiment Facility: https://www.nasa.gov/mission_pages/station/research/experiments/explorer/Facility.html?#id=333

Rassvet module: https://www.nasa.gov/mission_pages/station/structure/elements/rassvet

Poisk airlock: https://www.nasa.gov/mission_pages/station/structure/elements/poisk-mini-research-module-2

Space Station Research and Technology: https://www.nasa.gov/mission_pages/station/research/overview.html

International Space Station (ISS): https://www.nasa.gov/mission_pages/station/main/index.html

Image (mentioned), Animation (mentioned), Text, Credits: NASA/Mark Garcia.

Best regards, Orbiter.ch

NASA InSight Study Provides Clearest Look Ever at Martian Core

 






NASA - InSight Mission patch.


April 26, 2023

A pair of quakes in 2021 sent seismic waves deep into the Red Planet’s core, giving scientists the best data yet on its size and composition.

Image above: This is one of the last images ever taken by NASA’s InSight Mars lander. Captured on Dec. 11, 2022, the 1,436th Martian day, or sol, of the mission, it shows InSight’s seismometer on the Red Planet’s surface. Image Credits: NASA/JPL-Caltech.

While NASA retired its InSight Mars lander in December, the trove of data from its seismometer will be pored over for decades to come. By looking at seismic waves the instrument detected from a pair of temblors in 2021, scientists have been able to deduce that Mars’ liquid iron core is smaller and denser than previously thought.

The findings, which mark the first direct observations ever made of another planet’s core, were detailed in a paper published April 24 in the Proceedings of the National Academies of Sciences. Occurring on Aug. 25 and Sept. 18, 2021, the two temblors were the first identified by the InSight team to have originated on the opposite side of the planet from the lander – so-called farside quakes. The distance proved crucial: The farther a quake happens from InSight, the deeper into the planet its seismic waves can travel before being detected.

“We needed both luck and skill to find, and then use, these quakes,” said lead author Jessica Irving, an Earth scientist at the University of Bristol in the United Kingdom. “Farside quakes are intrinsically harder to detect because a great deal of energy is lost or diverted away as seismic waves travel through the planet.”

Irving noted that the two quakes occurred after the mission had been operating on the Red Planet for well over a full Martian year (about two Earth years), meaning the Marsquake Service – the scientists who initially scrutinize seismographs – had already honed their skills. It also helped that a meteoroid impact caused one of the two quakes; impacts provide a precise location and more accurate data for a seismologist to work with. (Because Mars has no tectonic plates, most marsquakes are caused by faults, or rock fractures, that form in the planet’s crust due to heat and stress.) The quakes’ size was also a factor in the detections.

Image above: This artist’s concept shows a cutaway of Mars, along with the paths of seismic waves from two separate quakes in 2021. Detected by NASA’s InSight mission, these seismic waves were the first ever identified to enter another planet’s core. Image Credits: NASA/JPL-Caltech/University of Maryland.

“These two farside quakes were among the larger ones heard by InSight,” said Bruce Banerdt, InSight’s principal investigator at NASA’s Jet Propulsion Laboratory in Southern California. “If they hadn’t been so big, we couldn’t have detected them.”

One of the challenges in detecting these particular quakes was that they’re in a “shadow zone” – a part of the planet from which seismic waves tend to be refracted away from InSight, making it hard for a quake’s echo to reach the lander unless it is very large. Detecting seismic waves that cross through a shadow zone is exceptionally difficult; it’s all the more impressive that the InSight team did so using just the one seismometer they had on Mars. (In contrast, many seismometers are distributed on Earth.)

“It took a lot of seismological expertise from across the InSight team to tease the signals out from the complex seismograms recorded by the lander,” Irving said.

A previous paper that offered a first glimpse of the planet’s core relied on seismic waves that reflected off its outer boundary, providing less precise data. Detecting seismic waves that actually traveled through the core allows scientists to refine their models of what the core looks like. Based on the findings documented in the new paper, about a fifth of the core is composed of elements such as sulfur, oxygen, carbon, and hydrogen.

“Determining the amount of these elements in a planetary core is important for understanding the conditions in our solar system when planets were forming and how these conditions affected the planets that formed,” said one of the paper’s co-authors, Doyeon Kim of ETH Zurich.

That was always the central goal of InSight’s mission: to study the deep interior of Mars and help scientists understand how all rocky worlds form, including Earth and its Moon.

More About the Mission

JPL manages InSight for NASA’s Science Mission Directorate. InSight is part of NASA’s Discovery Program, managed by the agency’s Marshall Space Flight Center in Huntsville, Alabama. Lockheed Martin Space in Denver built the InSight spacecraft, including its cruise stage and lander, and supported spacecraft operations for the mission.

A number of European partners, including France’s Centre National d’Études Spatiales (CNES) and the German Aerospace Center (DLR), are supporting the InSight mission. CNES provided the Seismic Experiment for Interior Structure (SEIS) instrument to NASA, with the principal investigator at IPGP (Institut de Physique du Globe de Paris). Significant contributions for SEIS came from IPGP; the Max Planck Institute for Solar System Research (MPS) in Germany; the Swiss Federal Institute of Technology (ETH Zurich) in Switzerland; Imperial College London and Oxford University in the United Kingdom; and JPL. The Marsquake Service is headed by ETH Zurich, with significant contributions from IPGP; the University of Bristol; Imperial College; ISAE (Institut Supérieur de l'Aéronautique et de l’Espace); MPS; and JPL. DLR provided the Heat Flow and Physical Properties Package (HP3) instrument, with significant contributions from the Space Research Center (CBK) of the Polish Academy of Sciences and Astronika in Poland. Spain’s Centro de Astrobiología (CAB) supplied the temperature and wind sensors.

Related links:

National Academies of Sciences: https://www.pnas.org/doi/10.1073/pnas.2217090120

InSight Mars Lander: https://www.nasa.gov/mission_pages/insight/main/index.html

Images (mentioned), Text, Credits: NASA/Tony Greicius/Karen Fox/Alana Johnson/JPL/Andrew Good.

Greetings, Orbiter.ch

NASA Retires Mineral Mapping Instrument on Mars Orbiter

 







NASA - Mars Reconnaissance Orbiter (MRO) patch.


April 26, 2023

One of six instruments aboard the agency’s Mars Reconnaissance Orbiter, CRISM produced global maps of minerals on the Red Planet’s surface.


Image above: CRISM data was superimposed onto an image of Mars’ Alga Crater captured by another MRO instrument, HiRISE. Each color represents a different material: blue for pyroxene, red for olivine, and green for impact glass, which forms in the heat of a violent impact that excavates a crater. Image Credits: NASA/JPL-Caltech/JHUAPL/Univ. of Arizona.

NASA switched off one of its oldest instruments studying Mars on April 3, a step that’s been planned since last year. Riding aboard NASA’s Mars Reconnaissance Orbiter, CRISM, or the Compact Reconnaissance Imaging Spectrometer for Mars, revealed minerals such as clays, hematite (otherwise known as iron oxide), and sulfates across the Red Planet’s surface for 17 years.

Led by Johns Hopkins University’s Applied Physics Laboratory (APL) in Laurel, Maryland, CRISM produced high-resolution mineral maps crucial in helping scientists understand how lakes, streams, and groundwater shaped the planet billions of years ago. The instrument’s two detectors saw in visible and infrared light, spotting the chemical fingerprints, or spectra, of minerals that form in the presence of water.

“Shutting down CRISM marks the end of an era for us,” said Rich Zurek, MRO’s project scientist at NASA’s Jet Propulsion Laboratory, which manages the mission. “It’s revealed where and how water transformed ancient Mars. The CRISM data products will be mined by scientists for years to come.”

Image above: This image shows six views of the Nili Fossae region of Mars captured by the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM), one of the instruments aboard NASA’s Mars Reconnaissance Orbiter. The varying colors represent minerals on the Martian surface seen in diffenrent wavelengths of light. Image Credits: NASA/JPL-Caltech/JHU-APL.

NASA has also relied on CRISM maps to figure out where the most scientifically interesting landing sites are, as with Gale Crater, which Curiosity has been exploring since 2012, and Jezero Crater, where NASA’s Perseverance rover recently collected its 19th sample.

In order to study infrared light, which is radiated by warm objects and is invisible to the human eye, CRISM relied on cryocoolers to isolate one of its spectrometers from the warmth of the spacecraft. Three cryocoolers were used in succession, and the last completed its lifecycle in 2017.

The CRISM team then looked for ways to continue producing data without the use of cryocoolers, deciding to create two new, nearly global maps. The first of these relied on data previously collected by the infrared spectrometer and by the second spectrometer on the instrument, which viewed a more limited range of minerals in visible and near-infrared light. This first map of water-related minerals, containing 5.6 gigapixels, has a spatial resolution of 600 feet (180 meters) per pixel and covers 86% of Mars. Scientists began releasing it in sections last year.

Image above: This impact crater in south Syrtis Major was captured by the HiRISE instrument on NASA’s MRO. Afterward, CRISM data was layered on top to reveal which minerals were present. Image Credits: NASA/JPL-Caltech/JHU-APL/University of Arizona.

For the second map, CRISM’s remaining spectrometer gathered data at an even higher spatial resolution (300 feet, or 90 meters per pixel). This map is slated for release in September.

“With these new maps, researchers can easily tie mineral deposits observed in high-resolution images to regional scale trends, landscape features, and geology,” said Kim Seelos, CRISM’s deputy principal investigator at APL. “Even though the CRISM investigation is formally coming to a close, I hope and expect to see many future scientists taking advantage of CRISM data for their research.”

NASA’s JPL, a division of Caltech in Pasadena, California, manages MRO for NASA’s Science Mission Directorate in Washington.

Related links:

Compact Reconnaissance Imaging Spectrometer for Mars (CRISM): https://civspace.jhuapl.edu/destinations/instruments/crism

Mars Reconnaissance Orbiter (MRO): https://mars.nasa.gov/mro/

Images (mentioned), Text, Credits: NASA/Karen Fox/Alana Johnson/JPL/Andrew Good.

Best regards, Orbiter.ch

SOHO chases asteroid's tail

 







NASA / ESA - SOHO Mission patch.


April 26, 2023

The ESA/NASA SOHO observatory has overturned 14 years of thinking about the strange Sun-skirting ‘rock comet’ known as Phaethon that could reopen the mystery of how the Geminid meteor shower was born.

Every December, the Geminid meteor shower lights up Earth's skies as our planet plunges through a vast cloud of dust in space. For years, the parent body of this meteor shower was unknown. Most of the annual meteor showers are associated with comets, which leave clouds of dust trailing behind them in the form of their tails. But the Geminids were different: no parent body was obvious.

When Phaethon was discovered in 1983 by the joint US/UK/Netherlands IRAS satellite, astronomers thought the mystery was solved. This small 5.8 km-wide object circled the Sun in an orbit very similar to that of the Geminid dust cloud, providing near-certain proof that Phaethon was the meteor shower's parent body even though Phaethon was an asteroid not a comet.

Phaethon shines and vanishes

Each orbit of Phaethon, lasting 524 days, consists of an unusually close approach to the Sun. At a closest approach (perihelion) distance of 21 million km, Phaethon is hidden from observatories on Earth by the blinding glare of the Sun. Therefore, solar observatories provide the only way to capture vital images to study the extreme activity of the asteroid at perihelion.

Since 2009, the NASA Solar Terrestrial Relations Observatory (STEREO) has observed a sudden brightening of the asteroid a few hours after perihelion. At this close approach, Phaethon also sports a tail, hundreds of kilometres in length, facing away from the Sun. This activity was originally thought to be caused by the release of small dust grains from the cracking of the asteroid’s surface as it passes the Sun. This led to Phaethon being dubbed a ‘rock comet’.

Now, new observations from SOHO recorded in May 2022 have shown for the first time that, contrary to 14 years of previous thought, the emission of sodium atoms is likely responsible for this activity.

Phaethon’s journey at perihelion

As part of a special observing plan devised by Qicheng Zhang and Karl Battams, long-exposure, filtered images were taken by SOHO’s Large Angle and Spectrometric Coronagraph (LASCO) telescope. Phaethon and its tail are absent from images taken with LASCO’s blue filter, which can detect dust. But, it is bright in the sodium-sensitive orange filter, offering compelling evidence that sodium emission is occurring. The emission is caused by fluorescence, when sodium atoms get excited by the Sun and glow orange, similar to a street lamp.

“Our unique observing plan found the mysterious asteroid Phaethon for the first time in SOHO data,” says PhD student Qicheng Zhang, who led the study. “The distinctive filters of the 27-year-old LASCO camera were used in a special interruption to the regular observing schedule to uncover these hidden secrets. By digging in the treasure chest of SOHO, we showed that Phaethon is visible in LASCO images from 18 different orbits back to 1997.”

SOHO spots Phaethon at perihelion

Phaethon is not the only object near the Sun to be releasing sodium. The planet Mercury also exhibits a bright sodium tail that peaks around two weeks after perihelion – something that the joint ESA/JAXA BepiColombo mission will investigate once in orbit around Mercury. Observations of Mercury’s sodium tail from the STEREO H1-1 heliospheric imager were used as a calibration standard, like a standard lamp, to study this emission from Phaethon to support Zhang’s theory.

SOHO has observed hundreds of tiny Sun-skirting objects that are classified as comets – icy bodies which appear to brighten when very close to the Sun. These can be hard to distinguish from asteroids like Phaethon which shine temporarily. However, the sodium identified in this study has opened the possibility that perhaps the so-called comets discovered by SOHO are more like rocky asteroids similar to Phaethon.

This study shines more light on the events which could have formed the Geminid meteoroids, which range in size from sand-grains to pea-sized. Sodium activity on the surface is not enough to lift these particles and contribute to the stream. Instead, an unobserved and unknown disruption of Phaethon, perhaps over two thousand years ago, is assumed to have created the shower.   

The fresh layers of volatile sodium which contribute to the brightening observed today suggest that another mass-loss event may have resurfaced Phaethon more recently, perhaps less than 1000 years ago. Therefore, the exact origin of the Geminids meteoroids may be better understood by studying Phaethon.

SOHO’s comet encounters

There is great interest in Phaethon due to its distinctive activity and mysterious history, which make it an essential and intriguing source of up-close future study. Hence, JAXA is preparing to send a flyby mission called DESTINY+ to image the surface of Phaethon in 2028 and uncover more about its history.  
In addition to future missions, citizen scientists can play their part in revealing new discoveries using SOHO. Over 4500 Sun-skirting objects have been identified in SOHO images, the majority with the help of the Sungrazer Project. Citizen scientist ‘comet hunters’ can sift through SOHO and STEREO data to identify new objects.

Karl Battams, principal investigator of both LASCO and the Sungrazer project, explains, “SOHO is the most prominent comet hunter in history, with a huge catalogue of discoveries still awaiting detailed analysis. Both SOHO and STEREO are uniquely placed to be able to routinely observe objects extremely close to the Sun. The future of asteroid and comet studies is bright thanks to these and future encounter missions that will help us uncover more about these dynamic objects.”

“Since its launch in 1995, SOHO and its instruments continue to deliver exciting science, using the mission in different ways to study asteroids and comets in addition to its primary target, the Sun,” adds Bernhard Fleck, ESA’s SOHO project scientist.

Notes for editors

‘Sodium Brightening of (3200) Phaethon Near Perihelion’ by Q. Zhang et al. is published in The Planetary Science Journal here: https://iopscience.iop.org/article/10.3847/PSJ/acc866

Related links:

SOHO: https://www.esa.int/Science_Exploration/Space_Science/SOHO_overview2

STEREO: https://stereo.gsfc.nasa.gov/

Animations, Images, Text, Credits: ESA/NASA/Q. Zhang/ESA/NASA/USNRL/K. Battams/ESA/NASA/R. Pickard.

Greetings, Orbiter.ch

lundi 24 avril 2023

Astronauts Gearing Up for Friday Spacewalk

 







ISS - Expedition 69 Mission patch.


April 24, 2023

Two astronauts on the Expedition 69 crew are gearing up for a spacewalk at the end of the week. Meanwhile, two cosmonauts are standing down after their spacewalk planned for Tuesday was postponed.

Flight Engineers Stephen Bowen of NASA and Sultan Alneyadi of UAE (United Arab Emirates) are preparing for a spacewalk scheduled for 9:15 a.m. EDT on Friday. The duo in their Extravehicular Mobility Units, or spacesuits, will spend about six-and-a-half hours in the vacuum of space continuing to upgrade the orbital outpost’s power generation system. International Space Station managers will appear on NASA TV, on the agency’s app and website, at 2 p.m. today to discuss Friday’s spacewalk.

Image above: Astronaut Stephen Bowen is pictured waving during the seventh spacewalk of his career on March 2, 2011. Image Credit: NASA.

The two astronauts spent the day checking their spacesuits for leaks and proper fit verification with assistance from NASA Flight Engineer Woody Hoburg. Hoburg, along with NASA Flight Engineer Frank Rubio, will assist the astronauts in and out of their spacesuits and monitor their spacewalk. Alneyadi also wore a set of virtual reality goggles and trained for a variety of unlikely spacewalking rescue scenarios.

International Space Station (ISS). Animation Credit: ESA

Meanwhile, another spacewalk that was planned for Tuesday has been postponed until early May. Commander Sergey Prokopyev and Flight Engineer Dmitri Petelin , with assistance from European robotic arm operator and Flight Engineer Andrey Fedyaev, were due to move an experiment airlock from the Rassvet module to the Nauka science module. That work has been pushed back several days while ground controllers study the procedures planned for the spacewalk.

Related article (NASA):

NASA Sets Coverage of Spacewalk, News Conference for Station Upgrades
https://www.nasa.gov/press-release/nasa-sets-coverage-of-spacewalk-news-conference-for-station-upgrades

Related links:

NASA TV: https://www.nasa.gov/nasalive

Expedition 69: https://www.nasa.gov/mission_pages/station/expeditions/expedition69/index.html

Rassvet module: https://www.nasa.gov/mission_pages/station/structure/elements/rassvet

Nauka multipurpose laboratory module: https://www.roscosmos.ru/tag/nauka/

Space Station Research and Technology: https://www.nasa.gov/mission_pages/station/research/overview.html

International Space Station (ISS): https://www.nasa.gov/mission_pages/station/main/index.html

Image (mentioned), Animation (mentioned), Text, Credits: NASA/Mark Garcia.

Best regards, Orbiter.ch