jeudi 31 janvier 2019
Fiery Research Work and CubeSats Deployed Today
ISS - Expedition 58 Mission patch.
January 31, 2019
The Expedition 58 crew set up a variety of combustion research hardware today to look at what happens to high temperatures, fuels and flames in space. The International Space Station also deployed the first set of CubeSats this year.
Image above: The Expedition 58 crew gathers inside the Zvezda service module for a portrait. From left are, NASA astronaut Anne McClain, Roscosmos cosmonaut Oleg Kononenko and Canadian Space Agency astronaut David Saint-Jacques. Image Credit: NASA.
The Two-Phase Flow Experiment, sponsored by the Japan Aerospace Exploration Agency, investigates the heat transfer caused by boiling liquids in space. Flight Engineer Anne McClain set up a specialized microscope to study the phenomena inside Japan’s Kibo lab module today. Results may inform future designs of high-performance thermal management and cooling systems on Earth and in space.
Flight Engineer David Saint-Jacques opened the Combustion Integrated Rack inside the U.S. Destiny lab module again today for more maintenance work. The Canadian astronaut replaced a control unit and a radiometer inside the fuel and flame research device.
The duo also monitored and photographed several CubeSats deployed into Earth orbit outside Kibo’s airlock today. The CubeSats are inexpensive tiny research satellites that will explore Earth’s ionosphere and study space communication techniques.
Image above: Flyingt over Brazil, seen by EarthCam on ISS, speed: 27'614 Km/h, altitude: 405,37 Km, image captured by Roland Berga (on Earth in Switzerland) from International Space Station (ISS) using ISS-HD Live application with EarthCam's from ISS on January 31, 2019 at 18:53 UTC. Image Credits: Orbiter.ch Aerospace/Roland Berga.
Commander Oleg Kononenko, the four-time space station resident from Roscosmos, started Thursday photographing the interior portion of the orbital lab’s Russian segment. The veteran cosmonaut then moved onto life support maintenance and explored ways students and educators can collaborate with space crews.
Related links:
Expedition 58: https://www.nasa.gov/mission_pages/station/expeditions/expedition58/index.html
Two-Phase Flow Experiment: https://www.nasa.gov/mission_pages/station/research/experiments/explorer/Investigation.html?#id=1034
Kibo lab module: https://www.nasa.gov/mission_pages/station/structure/elements/japan-kibo-laboratory
Destiny lab module: https://www.nasa.gov/mission_pages/station/structure/elements/us-destiny-laboratory
CubeSats: https://www.nasa.gov/mission_pages/cubesats/index.html
Russian segment: https://www.nasa.gov/mission_pages/station/structure/elements/space-station-assembly
Collaborate with space crews: https://www.energia.ru/en/iss/researches/popular/07.html
Space Station Research and Technology: https://www.nasa.gov/mission_pages/station/research/index.html
International Space Station (ISS): https://www.nasa.gov/mission_pages/station/main/index.html
Images (mentioned), Text, Credits: NASA/Mark Garcia/Orbiter.ch Aerospace/Roland Berga.
Best regards, Orbiter.ch
Hubble fortuitously discovers a new galaxy in the cosmic neighbourhood
ESA - Hubble Space Telescope logo.
31 January 2019
The accidentally discovered galaxy Bedin I
Astronomers using the NASA/ESA Hubble Space Telescope to study some of the oldest and faintest stars in the globular cluster NGC 6752 have made an unexpected finding. They discovered a dwarf galaxy in our cosmic backyard, only 30 million light-years away. The finding is reported in the journal Monthly Notices of the Royal Astronomical Society: Letters.
Bedin 1 in NGC 6752
An international team of astronomers recently used the NASA/ESA Hubble Space Telescope to study white dwarf stars within the globular cluster NGC 6752. The aim of their observations was to use these stars to measure the age of the globular cluster, but in the process they made an unexpected discovery.
Globular cluster NGC 6752
In the outer fringes of the area observed with Hubble’s Advanced Camera for Surveys a compact collection of stars was visible. After a careful analysis of their brightnesses and temperatures, the astronomers concluded that these stars did not belong to the cluster — which is part of the Milky Way — but rather they are millions of light-years more distant.
Wide-field view of NGC 6752 (ground-based view)
Our newly discovered cosmic neighbour, nicknamed Bedin 1 by the astronomers, is a modestly sized, elongated galaxy. It measures only around 3000 light-years at its greatest extent — a fraction of the size of the Milky Way. Not only is it tiny, but it is also incredibly faint. These properties led astronomers to classify it as a dwarf spheroidal galaxy.
Zooming in on NGC 6752 and Bedin 1
Dwarf spheroidal galaxies are defined by their small size, low-luminosity, lack of dust and old stellar populations [1]. 36 galaxies of this type are already known to exist in the Local Group of Galaxies, 22 of which are satellite galaxies of the Milky Way.
While dwarf spheroidal galaxies are not uncommon, Bedin 1 has some notable features. Not only is it one of just a few dwarf spheroidals that have a well established distance but it is also extremely isolated. It lies about 30 million light-years from the Milky Way and 2 million light-years from the nearest plausible large galaxy host, NGC 6744. This makes it possibly the most isolated small dwarf galaxy discovered to date.
Flight to Bedin 1
From the properties of its stars, astronomers were able to infer that the galaxy is around 13 billion years old — nearly as old as the Universe itself. Because of its isolation — which resulted in hardly any interaction with other galaxies — and its age, Bedin 1 is the astronomical equivalent of a living fossil from the early Universe.
The discovery of Bedin 1 was a truly serendipitous find. Very few Hubble images allow such faint objects to be seen, and they cover only a small area of the sky. Future telescopes with a large field of view, such as the WFIRST telescope, will have cameras covering a much larger area of the sky and may find many more of these galactic neighbours.
Hubble Space Telescope (HST). Animation Credits: NASA/ESA
Notes:
[1] While similar to dwarf elliptical galaxies in appearance and properties, dwarf spheroidal galaxies are in general approximately spherical in shape and have a lower luminosity.
More information:
The Hubble Space Telescope is a project of international cooperation between ESA and NASA.
The results were presented in the letter The HST Large Programme on NGC 6752. I. Serendipitous discovery of a dwarf galaxy in background, published in the journal Monthly Notices of the Royal Astronomical Society: Letters.
The international team of astronomers that carried out this study consists of L. R. Bedin (INAF-Osservatorio Astronomico di Padova, Italy), M. Salaris (Liverpool John Moores University, UK), R. M. Rich (University of California Los Angeles, USA), H. Richer (University of British Columbia), J. Anderson (Space Telescope Science Institute, USA), B. Bettoni (INAF-Osservatorio Astronomico di Padova, Italy), D. Nardiello (Università di Padova, Italy), A. P. Milone (Università di Padova, Italy), A. F. Marino (Università di Padova, Italy), M. Libralato (Space Telescope Science Institute, USA), A. Bellini (Space Telescope Science Institute, USA), A. Dieball (University of Bonn, Germany), P. Bergeron (Université de Montréal, Canada), A. J. Burgasser (University of California San Diego, USA), D. Apai (University of Arizona, USA)
Links:
Images of Hubble: http://www.spacetelescope.org/images/archive/category/spacecraft/
Hubblesite release: http://hubblesite.org/news_release/news/2019-09
Science paper: http://www.spacetelescope.org/static/archives/releases/science_papers/heic1903/heic1903a.pdf
NASA/ESA Hubble Space Telescope: https://www.spacetelescope.org/
Images, Text, Credits: NASA/ESA, Bedin et al./Mathias Jäger/Hubble, NASA, Bedin et al., Digitized Sky Survey 2/Acknowledgement: Davide De Martin/Videos: Credits: Risinger, DSS, Hubble, Damian Peach/Music: Astral Electronic/SA/Hubble, M. Kornmesser.
Greetings, Orbiter.ch
mercredi 30 janvier 2019
Crew Works CubeSats, Life Science and Configures Physics Hardware
ISS - Expedition 58 Mission patch.
January 30, 2019
The International Space Station is set to deploy a new series of CubeSats as the Expedition 58 crew configures research hardware to enable a variety of space experiments.
Japan’s Kibo laboratory module airlock has been set up with a small satellite deployer loaded with several CubeSats. Astronaut Anne McClain finished the installation work Wednesday, depressurized the airlock and maneuvered the deployer outside Kibo.
Image above: Portions of Cuba, The Bahamas and the Turks and Caicos Islands are viewed from the International Space Station as the orbital complex flew 252 miles above the Atlantic Ocean. At left, is the aft end of the Progress 70 resupply ship from Russia attached to the Pirs docking compartment. Image Credit: NASA.
She and fellow astronaut David Saint-Jacques will monitor and photograph the CubeSat deployments planned for Thursday around noon EST. The CubeSats will study Earth’s ionosphere and satellite communication techniques.
McClain next inventoried Rodent Research gear trashing some hardware to make extra space aboard the lab. She later swapped a hard drive on a laptop computer dedicated to meteor observations then attached sensors to her head and chest for the Circadian Rhythms study.
International Space Station (ISS). Animation Credit: NASA
Saint-Jacques installed new electronics on the Kubik incubator upgrading the device that houses biology experiments on seeds, cells and small animals. He later swapped parts in the Combustion Integrated Rack that permits safe research into fuel and flames aboard the orbital lab.
Commander Oleg Kononenko started Wednesday researching microgravity’s effect on heart rate and breathing. He later explored advanced photography tools and techniques to better detect targets of interest on Earth.
Related links:
Expedition 58: https://www.nasa.gov/mission_pages/station/expeditions/expedition58/index.html
Kibo laboratory module: https://www.nasa.gov/mission_pages/station/structure/elements/japan-kibo-laboratory
CubeSats: https://www.nasa.gov/mission_pages/cubesats/index.html
Rodent Research: https://www.nasa.gov/mission_pages/station/research/experiments/explorer/Investigation.html?#id=7735
Meteor: https://www.nasa.gov/mission_pages/station/research/experiments/explorer/Investigation.html?#id=1174
Circadian Rhythms: https://www.nasa.gov/mission_pages/station/research/experiments/explorer/Investigation.html?#id=869
Kubik: https://www.nasa.gov/mission_pages/station/research/experiments/explorer/Facility.html?#id=894
Advanced photography tools and techniques: https://www.nasa.gov/mission_pages/station/research/experiments/explorer/Investigation.html?#id=1469
Space Station Research and Technology: https://www.nasa.gov/mission_pages/station/research/index.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
Huge Cavity in Antarctic Glacier Signals Rapid Decay
NASA - Operation IceBridge Mission patch.
January 30, 2019
A gigantic cavity - two-thirds the area of Manhattan and almost 1,000 feet (300 meters) tall - growing at the bottom of Thwaites Glacier in West Antarctica is one of several disturbing discoveries reported in a new NASA-led study of the disintegrating glacier. The findings highlight the need for detailed observations of Antarctic glaciers' undersides in calculating how fast global sea levels will rise in response to climate change.
Researchers expected to find some gaps between ice and bedrock at Thwaites' bottom where ocean water could flow in and melt the glacier from below. The size and explosive growth rate of the newfound hole, however, surprised them. It's big enough to have contained 14 billion tons of ice, and most of that ice melted over the last three years.
Thwaites Glacier. Image Credit: NASA/OIB/Jeremy Harbeck
"We have suspected for years that Thwaites was not tightly attached to the bedrock beneath it," said Eric Rignot of the University of California, Irvine, and NASA's Jet Propulsion Laboratory in Pasadena, California. Rignot is a co-author of the new study, which was published today in Science Advances. "Thanks to a new generation of satellites, we can finally see the detail," he said.
The cavity was revealed by ice-penetrating radar in NASA's Operation IceBridge, an airborne campaign beginning in 2010 that studies connections between the polar regions and the global climate. The researchers also used data from a constellation of Italian and German spaceborne synthetic aperture radars. These very high-resolution data can be processed by a technique called radar interferometry to reveal how the ground surface below has moved between images.
"[The size of] a cavity under a glacier plays an important role in melting," said the study's lead author, Pietro Milillo of JPL. "As more heat and water get under the glacier, it melts faster."
Numerical models of ice sheets use a fixed shape to represent a cavity under the ice, rather than allowing the cavity to change and grow. The new discovery implies that this limitation most likely causes those models to underestimate how fast Thwaites is losing ice.
About the size of Florida, Thwaites Glacier is currently responsible for approximately 4 percent of global sea level rise. It holds enough ice to raise the world ocean a little over 2 feet (65 centimeters) and backstops neighboring glaciers that would raise sea levels an additional 8 feet (2.4 meters) if all the ice were lost.
Animation above: Changes in surface height at Thwaites Glacier's grounding line, 2011 to 2017, with sinking areas in red and rising areas in blue. The growing cavity (red mass, center) caused the greatest sinking. The mottled area (bottom left) is the site of extensive calving. Contours show bedrock topography. Animation Credits: NASA/JPL-Caltech.
Thwaites is one of the hardest places to reach on Earth, but it is about to become better known than ever before. The U.S. National Science Foundation and British National Environmental Research Council are mounting a five-year field project to answer the most critical questions about its processes and features. The International Thwaites Glacier Collaboration will begin its field experiments in the Southern Hemisphere summer of 2019-20.
How Scientists Measure Ice Loss
There's no way to monitor Antarctic glaciers from ground level over the long term. Instead, scientists use satellite or airborne instrument data to observe features that change as a glacier melts, such as its flow speed and surface height.
Another changing feature is a glacier's grounding line - the place near the edge of the continent where it lifts off its bed and starts to float on seawater. Many Antarctic glaciers extend for miles beyond their grounding lines, floating out over the open ocean.
Just as a grounded boat can float again when the weight of its cargo is removed, a glacier that loses ice weight can float over land where it used to stick. When this happens, the grounding line retreats inland. That exposes more of a glacier's underside to sea water, increasing the likelihood its melt rate will accelerate.
An Irregular Retreat
For Thwaites, "We are discovering different mechanisms of retreat," Millilo said. Different processes at various parts of the 100-mile-long (160-kilometer-long) front of the glacier are putting the rates of grounding-line retreat and of ice loss out of sync.
The huge cavity is under the main trunk of the glacier on its western side - the side farther from the West Antarctic Peninsula. In this region, as the tide rises and falls, the grounding line retreats and advances across a zone of about 2 to 3 miles (3 to 5 kilometers). The glacier has been coming unstuck from a ridge in the bedrock at a steady rate of about 0.4 to 0.5 miles (0.6 to 0.8 kilometers) a year since 1992. Despite this stable rate of grounding-line retreat, the melt rate on this side of the glacier is extremely high.
"On the eastern side of the glacier, the grounding-line retreat proceeds through small channels, maybe a kilometer wide, like fingers reaching beneath the glacier to melt it from below," Milillo said. In that region, the rate of grounding-line retreat doubled from about 0.4 miles (0.6 kilometers) a year from 1992 to 2011 to 0.8 miles (1.2 kilometers) a year from 2011 to 2017. Even with this accelerating retreat, however, melt rates on this side of the glacier are lower than on the western side.
These results highlight that ice-ocean interactions are more complex than previously understood.
Milillo hopes the new results will be useful for the International Thwaites Glacier Collaboration researchers as they prepare for their fieldwork. "Such data is essential for field parties to focus on areas where the action is, because the grounding line is retreating rapidly with complex spatial patterns," he said.
"Understanding the details of how the ocean melts away this glacier is essential to project its impact on sea level rise in the coming decades," Rignot said.
The paper by Milillo and his co-authors in the journal Science Advances is titled "Heterogeneous retreat and ice melt of Thwaites Glacier, West Antarctica." Co-authors were from the University of California, Irvine; the German Aerospace Center in Munich, Germany; and the University Grenoble Alpes in Grenoble, France.
Related links:
Operation IceBridge: https://www.nasa.gov/mission_pages/icebridge/index.html
International Thwaites Glacier Collaboration: https://thwaitesglacier.org/
Image (mentioned), Animation (mentioned), Text, Credits: NASA/JPL/Esprit Smith/University of California/Brian Bell/NASA's Earth Science News Team, written by Carol Rasmussen.
Greetings, Orbiter.ch
NASA’s NICER Mission Maps ‘Light Echoes’ of New Black Hole
NASA - Neutron star Interior Composition Explorer (NICER) patch.
Jan. 30, 2019
Scientists have charted the environment surrounding a stellar-mass black hole that is 10 times the mass of the Sun using NASA’s Neutron star Interior Composition Explorer (NICER) payload aboard the International Space Station. NICER detected X-ray light from the recently discovered black hole, called MAXI J1820+070 (J1820 for short), as it consumed material from a companion star. Waves of X-rays formed “light echoes” that reflected off the swirling gas near the black hole and revealed changes in the environment’s size and shape.
“NICER has allowed us to measure light echoes closer to a stellar-mass black hole than ever before,” said Erin Kara, an astrophysicist at the University of Maryland, College Park and NASA’s Goddard Space Flight Center in Greenbelt, Maryland, who presented the findings at the 233rd American Astronomical Society meeting in Seattle. “Previously, these light echoes off the inner accretion disk were only seen in supermassive black holes, which are millions to billions of solar masses and undergo changes slowly. Stellar black holes like J1820 have much lower masses and evolve much faster, so we can see changes play out on human time scales.”
A paper describing the findings, led by Kara, appeared in the Jan. 10 issue of Nature and is available online: http://dx.doi.org/10.1038/s41586-018-0803-x
NICER Charts the Area Around a New Black Hole
Video above: Watch how X-ray echoes, mapped by NASA’s Neutron star Interior Composition Explorer (NICER) revealed changes to the corona of black hole MAXI J1820+070. Video Credits: NASA’s Goddard Space Flight Center.
J1820 is located about 10,000 light-years away toward the constellation Leo. The companion star in the system was identified in a survey by ESA’s (European Space Agency) Gaia mission, which allowed researchers to estimate its distance. Astronomers were unaware of the black hole’s presence until March 11, 2018, when an outburst was spotted by the Japan Aerospace Exploration Agency’s Monitor of All-sky X-ray Image (MAXI), also aboard the space station. J1820 went from a totally unknown black hole to one of the brightest sources in the X-ray sky over a few days. NICER moved quickly to capture this dramatic transition and continues to follow the fading tail of the eruption.
“NICER was designed to be sensitive enough to study faint, incredibly dense objects called neutron stars,” said Zaven Arzoumanian, the NICER science lead at Goddard and a co-author of the paper. “We’re pleased at how useful it’s also proven in studying these very X-ray-bright stellar-mass black holes.”
A black hole can siphon gas from a nearby companion star into a ring of material called an accretion disk. Gravitational and magnetic forces heat the disk to millions of degrees, making it hot enough to produce X-rays at the inner parts of the disk, near the black hole. Outbursts occur when an instability in the disk causes a flood of gas to move inward, toward the black hole, like an avalanche. The causes of disk instabilities are poorly understood.
Above the disk is the corona, a region of subatomic particles around 1 billion degrees Celsius (1.8 billion degrees Fahrenheit) that glows in higher-energy X-rays. Many mysteries remain about the origin and evolution of the corona. Some theories suggest the structure could represent an early form of the high-speed particle jets these types of systems often emit.
Image above: In this illustration of a newly discovered black hole named MAXI J1820+070, a black hole pulls material off a neighboring star and into an accretion disk. Above the disk is a region of subatomic particles called the corona. Image Credits: Aurore Simonnet and NASA’s Goddard Space Flight Center.
Astrophysicists want to better understand how the inner edge of the accretion disk and the corona above it change in size and shape as a black hole accretes material from its companion star. If they can understand how and why these changes occur in stellar-mass black holes over a period of weeks, scientists could shed light on how supermassive black holes evolve over millions of years and how they affect the galaxies in which they reside.
One method used to chart those changes is called X-ray reverberation mapping, which uses X-ray reflections in much the same way sonar uses sound waves to map undersea terrain. Some X-rays from the corona travel straight toward us, while others light up the disk and reflect back at different energies and angles.
X-ray reverberation mapping of supermassive black holes has shown that the inner edge of the accretion disk is very close to the event horizon, the point of no return. The corona is also compact, lying closer to the black hole rather than over much of the accretion disk. Previous observations of X-ray echoes from stellar black holes, however, suggested the inner edge of the accretion disk could be quite distant, up to hundreds of times the size of the event horizon. The stellar-mass J1820, however, behaved more like its supermassive cousins.
As they examined NICER’s observations of J1820, Kara’s team saw a decrease in the delay, or lag time, between the initial flare of X-rays coming directly from the corona and the flare’s echo off the disk, indicating that the X-rays traveled shorter and shorter distances before they were reflected. From 10,000 light-years away, they estimated that the corona contracted vertically from roughly 100 to 10 miles — that’s like seeing something the size of a blueberry shrink to something the size of a poppy seed at the distance of Pluto
Neutron star Interior Composition Explorer (NICER). Animation Credit: NASA
“This is the first time that we’ve seen this kind of evidence that it’s the corona shrinking during this particular phase of outburst evolution,” said co-author Jack Steiner, an astrophysicist at the Massachusetts Institute of Technology’s Kavli Institute for Astrophysics and Space Research in Cambridge. “The corona is still pretty mysterious, and we still have a loose understanding of what it is. But we now have evidence that the thing that’s evolving in the system is the structure of the corona itself.”
To confirm the decreased lag time was due to a change in the corona and not the disk, the researchers used a signal called the iron K line created when X-rays from the corona collide with iron atoms in the disk, causing them to fluoresce. Time runs slower in stronger gravitational fields and at higher velocities, as stated in Einstein’s theory of relativity. When the iron atoms closest to the black hole are bombarded by light from the core of the corona, the X-ray wavelengths they emit get stretched because time is moving slower for them than for the observer (in this case, NICER).
Kara’s team discovered that J1820’s stretched iron K line remained constant, which means the inner edge of the disk remained close to the black hole — similar to a supermassive black hole. If the decreased lag time was caused by the inner edge of the disk moving even further inward, then the iron K line would have stretched even more.
These observations give scientists new insights into how material funnels in to the black hole and how energy is released in this process.
Image above: The NICER instrument installed on the International Space Station, as captured by a high-definition external camera on Oct. 22, 2018. Image Credit: NASA.
“NICER’s observations of J1820 have taught us something new about stellar-mass black holes and about how we might use them as analogs for studying supermassive black holes and their effects on galaxy formation,” said co-author Philip Uttley, an astrophysicist at the University of Amsterdam. “We’ve seen four similar events in NICER’s first year, and it’s remarkable. It feels like we’re on the edge of a huge breakthrough in X-ray astronomy.”
NICER is an Astrophysics Mission of Opportunity within NASA's Explorer program, which provides frequent flight opportunities for world-class scientific investigations from space utilizing innovative, streamlined and efficient management approaches within the heliophysics and astrophysics science areas. NASA's Space Technology Mission Directorate supports the SEXTANT component of the mission, demonstrating pulsar-based spacecraft navigation.
Related links:
NASA’s Neutron star Interior Composition Explorer (NICER): https://www.nasa.gov/nicer
Monitor of All-sky X-ray Image (MAXI): https://www.nasa.gov/mission_pages/station/research/experiments/603.html
International Space Station (ISS): https://www.nasa.gov/mission_pages/station/main/index.html
Space Station Research and Technology: https://www.nasa.gov/mission_pages/station/research/index.html
NASA’s Goddard Space Flight Center (GSFC): https://www.nasa.gov/goddard
University of Maryland: https://www.umd.edu/
European Space Agency (ESA): https://www.esa.int/ESA
Japan Aerospace Exploration Agency (JAXA): http://global.jaxa.jp/
Images (mentioned), Animation (mentioned), Video (mentioned), Text, Credits: NASA/Rob Garner/Goddard Space Flight Center, by Jeanette Kazmierczak.
Greetings, Orbiter.ch
mardi 29 janvier 2019
Station Crew Helping Future Orion Explorers
ISS - Expedition 58 Mission patch.
January 29, 2019
The International Space Station is providing a research platform today to help future astronauts navigate deep space in the Orion Multi-Purpose Crew Vehicle. The Expedition 58 crew is also testing new lights and setting up the orbital lab for CubeSat deployments.
NASA is planning deep space missions with its new Orion spacecraft that will rely on NASA’s Deep Space Network for communications and navigation. Flight Engineer David Saint-Jacques took photographs of the moon from the cupola today to calibrate Orion’s navigation software. The lunar data will provide additional navigation capability for Orion in the event of a loss of communication with the Deep Space Network.
Image above: The International Space Station photographed by departing Expedition 56 crew members aboard a Soyuz spacecraft after undocking on Oct. 4, 2018. Image Credit: NASA.
Another experiment geared towards future exploration taking place aboard the station is the Sextant study. As its name suggests, astronauts are testing a hand-held sextant to focus on stability and star-sighting opportunities while in microgravity. Results may aid future Orion explorers and provide a backup navigation source for missions far beyond Earth orbit.
Astronaut Anne McClain worked throughout the day inside Japan’s Kibo laboratory module. She is setting up the Kibo airlock with hardware to deploy a set of CubeSats on Thursday. The CubeSats have a variety of educational and technical mission objectives including studying the ionosphere and satellite communications.
Flying over auroras. Animation Credit: NASA
McClain later tested and photographed new lights that scientists are researching for their ability to improve crew sleep and performance. She also continued loading the Northrop Grumman Cygnus cargo craft with disposable gear before it departs from the Unity module Feb. 8.
Both McClain and Saint-Jacques joined Commander Oleg Kononenko early Tuesday for body mass measurements. Kononenko then moved on to life support maintenance, crew culture studies and radiation measurements aboard the orbital lab.
Related links:
Expedition 58: https://www.nasa.gov/mission_pages/station/expeditions/expedition58/index.html
Orion spacecraft: https://www.nasa.gov/exploration/systems/orion/index.html
Deep Space Network: https://deepspace.jpl.nasa.gov/
Cupola: https://www.nasa.gov/mission_pages/station/structure/elements/cupola.html
Sextant: https://www.nasa.gov/mission_pages/station/research/experiments/explorer/Investigation.html?#id=7646
Kibo laboratory module: https://www.nasa.gov/mission_pages/station/structure/elements/japan-kibo-laboratory
CubeSats: https://www.nasa.gov/mission_pages/cubesats/index.html
Unity module: https://www.nasa.gov/mission_pages/station/structure/elements/unity
Space Station Research and Technology: https://www.nasa.gov/mission_pages/station/research/index.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
Warming Seas May Increase Frequency of Extreme Storms
NASA - EOS Aqua Mission logo.
Jan. 29, 2019
A new NASA study shows that warming of the tropical oceans due to climate change could lead to a substantial increase in the frequency of extreme rain storms by the end of the century.
Image above: An "anvil" storm cloud in the Midwestern U.S. Image Credit: UCAR.
The study team, led by Hartmut Aumann of NASA's Jet Propulsion Laboratory in Pasadena, California, combed through 15 years of data acquired by NASA's Atmospheric Infrared Sounder (AIRS) instrument over the tropical oceans to determine the relationship between the average sea surface temperature and the onset of severe storms.
They found that extreme storms — those producing at least 0.12 inches (3 millimeters) of rain per hour over a 16-mile (25-kilometer) area — formed when the sea surface temperature was higher than about 82 degrees Fahrenheit (28 degrees Celsius). They also found that, based on the data, 21 percent more storms form for every 1.8 degrees Fahrenheit (1 degree Celsius) that ocean surface temperatures rise.
"It is somewhat common sense that severe storms will increase in a warmer environment. Thunderstorms typically occur in the warmest season of the year," Aumann explained. "But our data provide the first quantitative estimate of how much they are likely to increase, at least for the tropical oceans."
Image above: A hurricane as seen by NASA's Atmospheric Infrared Sounder (AIRS) instrument. A hurricane is a large collection of extremely severe thunderstorms — seen here in dark blue. Each square pixel represents the measurements from a 10-by-10-mile (16-by-16-kilometer) area. At the time this image was taken, there were 140 of these extreme thunderstorms rotating about the eye of the hurricane. Image Credits: NASA/JPL-Caltech.
Currently accepted climate models project that with a steady increase of carbon dioxide in the atmosphere (1 percent per year), tropical ocean surface temperatures may rise by as much as 4.8 degrees Fahrenheit (2.7 degrees Celsius) by the end of the century. The study team concludes that if this were to happen, we could expect the frequency of extreme storms to increase by as much as 60 percent by that time.
EOS Aqua satellite. Image Credit: NASA
Although climate models aren't perfect, results like these can serve as a guideline for those looking to prepare for the potential effects a changing climate may have.
"Our results quantify and give a more visual meaning to the consequences of the predicted warming of the oceans," Aumann said. "More storms mean more flooding, more structure damage, more crop damage and so on, unless mitigating measures are implemented."
The peer-reviewed study was published in the December 2018 issue of the Geophysical Research Letters journal.
Aqua Satellite: https://www.nasa.gov/mission_pages/aqua/index.html
Climate: https://www.nasa.gov/subject/3127/climate
Images (mentioned), Text, Credits: NASA/Tony Greicius/JPL/Esprit Smith.
Greetings, Orbiter.ch
Inscription à :
Articles (Atom)

























