Thursday, November 8, 2018

Multimessenger links to NASA's Fermi Mission show how luck favors the prepared

In 2017, NASA's Fermi Gamma-ray Space Telescope played a pivotal role in two important breakthroughs occurring just five weeks apart. But what might seem like extraordinary good luck is really the product of research, analysis, preparation and development extending back more than a century. On Aug. 17, 2017, Fermi detected the first light ever seen from a source of gravitational waves - ripples in space-time produced, in this event, by the merger of two superdense neutron stars. Just five weeks later, a single high-energy particle discovered by the National Science Foundation's (NSF) IceCube Neutrino Observatory was traced to a distant galaxy powered by a supermassive black hole thanks to a gamma-ray flare observed by Fermi. "For millennia, light was our only source of information about the universe," said Julie McEnery, the Fermi project scientist at NASA's Goddard Space Flight Center in Greenbelt, Maryland. "The recent discoveries connect light, our best-known cosmic courier, to gravitational waves and particles like neutrinos - new messengers delivering different kinds of information that we're just beginning to explore." The origins of these discoveries stretch back to cutting-edge research as long ago as 1887. That's when physicists Albert Michelson and Edward Morley conducted an experiment to detect a substance, called the aether, which was postulated as a medium that permitted light waves to travel through space.


As their experiment showed and many since have confirmed, the aether doesn't exist. But the negative result proved to be one of the inspirations for Albert Einstein's 1905 special theory of relativity. He generalized this into a full-fledged theory of gravity in 1915, one that predicted the existence of gravitational waves.

A century later, on Sept. 14, 2015, the NSF's Laser Interferometer Gravitational-Wave Observatory (LIGO) detected these space-time vibrations for the first time as waves from the merger of two black holes reached Earth. In between came a steady stream of advances, including lasers, improved instrumentation and increasingly more powerful computers and software.

"Just as inventing the detector technologies has taken decades, so too has the theoretical and computational framework for analyzing and interpreting multimessenger observations," said Tyson Littenberg, the principal investigator of the LIGO research group at NASA's Marshall Space Flight Center in Huntsville, Alabama.

"We went through countless simulations to test new ideas and improve on existing algorithms so that we were prepared to make the most out of the first observations, and that basic research and development work continues."

Until 2005, it wasn't even possible to simulate in detail what happens when a pair of orbiting black holes coalesce. The breakthrough came when separate teams at Goddard and the University of Texas at Brownsville independently developed new computational methods that overcame all previous hurdles. An accurate understanding of gravitational-wave signals was one important step in evolving techniques designed to rapidly detect and characterize them.

"Another fundamental development was the highly optimized analysis pipelines and information technology infrastructure that can compare the theoretical model with the data, recognize the presence of a signal, calculate the location of the source on the sky and format the information in a way that the rest of the astronomical community could use," explained Tito Dal Canton, a NASA Postdoctoral Program Fellow and a member of a LIGO research group at Goddard led by Jordan Camp.

Astronomers need to know about short-lived events as soon as possible so they can bring to bear a wide array of telescopes in space and on the ground. Back in 1993, scientists at Goddard and Marshall began developing an automated system for distributing the locations of gamma-ray bursts (GRBs) - distant, powerful explosions that typically last a minute or less - to astronomers around the world in real time.

Located at Goddard and led by Principal Investigator Scott Barthelmy, the Gamma-ray Coordinates Network/Transient Astronomy Network now distributes alerts from many space missions as well as ground-based instruments like LIGO and IceCube.

Ghost particles

The historical thread for neutrinos began with French physicist Henri Becquerel and his 1895 discovery of radioactivity. In 1930, after studying a radioactive process called beta decay, Wolfang Pauli suggested it likely involved a new subatomic particle, later dubbed the neutrino. We now know neutrinos possess little mass, travel almost as fast as light, come in three varieties and are among the most abundant particles in the universe. But because they don't readily interact with other matter, neutrinos weren't discovered until 1956.

In 1912, Victor Hess discovered that charged particles, now called cosmic rays, continually enter Earth's atmosphere from every direction, which means space is filled with them. When cosmic rays strike air molecules, the collision produces a shower of particles - including neutrinos - that rains down through the atmosphere. Searching for astronomical neutrino sources meant placing experiments underground to reduce interference from cosmic rays and building very large detectors to tease out the weak signals of publicity-shy neutrinos.

Neutrinos produced by nuclear reactions inside the Sun's core were first detected in 1968 thanks to an experiment using 100,000 gallons of dry-cleaning fluid located deep in a South Dakota gold mine. Discovering the next astronomical neutrino source would take another 19 years.

Supernova 1987A, a stellar explosion in a nearby galaxy, remains the brightest and closest supernova seen in over 400 years and is the first for which the original star could be identified on pre-explosion images.

Theorists anticipated that neutrinos, which escape a collapsing star more readily than light, would be the first signal from a new supernova. And hours before 1987A's visible light arrived at Earth, experiments in Japan, the U.S. and Russia detected a brief burst of neutrinos, making the supernova the first source of neutrinos identified beyond the solar system.

"If none of these experiments was operating at the time, the neutrino signal would have passed by unnoticed," said Francis Halzen, the principal investigator of IceCube, which is essentially a neutrino telescope build into a cubic kilometer of ice at the South Pole.

"It isn't enough to develop the technology, refine theories or even construct a detector. We need to be making observations as often as we can for the best chance of catching brief, rare and scientifically interesting events. Both Fermi and IceCube are operating continuously, making uninterrupted observations of the sky."

Light fantastic

The third historical thread belongs to gamma rays, the highest-energy form of light, discovered in 1900 by the French physicist Paul Villard. When a gamma ray of sufficient energy interacts with matter, it provides a perfect demonstration of Einstein's most famous equation, E=mc2, by instantly transforming into particles - an electron and its antimatter counterpart, a positron. Conversely, crash an electron and a positron together and a gamma ray results.

NASA's Explorer 11 satellite, launched in 1961, detected the first gamma rays in space. In 1963, the U.S. Air Force began launching a series of satellites as part of Project Vela. These increasingly sophisticated satellites were designed to verify compliance with an international treaty that banned nuclear weapons tests in space or in the atmosphere. But starting in July 1967, scientists became aware the Vela satellites were seeing brief gamma-ray events that were clearly unrelated to weapons tests.

These explosions were GRBs, an entirely new phenomenon now known to mark the death of certain types of massive stars or the merger of orbiting neutron stars. NASA further explored the gamma-ray sky with the Compton Gamma Ray Observatory, which operated from 1991 to 2000 and recorded thousands of GRBs.

Starting in 1997, critical observations by the Italian-Dutch BeppoSAX satellite proved that GRBs were located far beyond our galaxy. Compton was succeeded by NASA's Neil Gehrels Swift Observatory in 2004 and Fermi in 2008, missions that continue exploring the high-energy sky and that follow up on LIGO and IceCube alerts.

"In the fields of observation, chance favors only the prepared mind," noted Louis Pasteur, the French chemist and microbiologist, in an 1854 lecture. Supported by decades of scientific discoveries and technological innovation, the burgeoning field of multimessenger astronomy is increasingly prepared for its next stroke of luck.

NASA's Fermi Gamma-ray Space Telescope is an astrophysics and particle physics partnership, developed in collaboration with the U.S. Department of Energy and with important contributions from academic institutions and partners in France, Germany, Italy, Japan, Sweden and the United States.

Russia's Roscosmos confirms computer glitch on board ISS

According to Roscosmos, the reported glitch will not hamper operations on board the ISS, and the affected computer will be rebooted on Thursday. Russia's State Space Corporation Roscosmos confirmed on Tuesday that one of the three computers on the Russian segment of the International Space Station (ISS) had been out of service due to a software glitch. "It will not affect the operations on board the orbital outpost as the standard cyclogram allows us to work with only two computers and still be able to fly for an indeterminately long time," Roscosmos said in a statement. The agency also stressed that there was no need to replace the computer, however it will be rebooted ahead of the arrival of Progress space freighted to the ISS. "In order to ensure the safety of the November docking with the Progress spacecraft, we will perform the reboot on November 8, 2018," the statement said. Last month, an accident occurred during the launch of a Soyuz-FG launch vehicle carrying the Soyuz MS-10 spacecraft with two new ISS crew members on board. Russian cosmonaut Alexey Ovchinin NASA astronaut Nick Hague safely returned to Earth in a jettisoned escape capsule.


The incident became the first failure of a manned space launch in modern Russian history. The crash is being investigated by a special commission of Russia's space agency Roscosmos. All manned launches from Baikonur Cosmodrome have been suspended until the commission finds out the causes of the failure.

Wednesday, November 7, 2018

NASA's ICON to explore boundary between Earth and Space

Early in the morning of Nov. 7, 2018, NASA launches the Ionospheric Connection Explorer, or ICON, a spacecraft that will explore the dynamic region where Earth meets space: the ionosphere. Overlapping the farthest reaches of Earth's atmosphere and the very beginning of space, the ionosphere stretches roughly 50 to 400 miles above the surface. Solar radiation cooks tenuous gases there until they lose an electron (or two or three), creating a sea of electrically charged ions and electrons. Neither fully Earth nor space, the ionosphere reacts both to winds and weather from the lower atmosphere below and solar energy streaming in from above, changing constantly to form conditions we call space weather. "After years of work, I'm excited to get into orbit and turn on the spacecraft, open the doors on all our instruments," said Thomas Immel, ICON principal investigator at the University of California, Berkeley. "ICON carries incredible capacity for science. I'm looking forward to surprising results and finally seeing the world through its eyes." As far as space goes, the ionosphere is as close to home as it gets. Its constant changes can affect astronauts, satellites and much of the communications signals modern society relies upon. Scientists want to understand these changes, so they can eventually better predict them and protect our interests in space. Space may look empty, but the ionosphere brims with electrically charged gases, solar radiation, and electric and magnetic fields. Turbulence in this sea of charged particles can manifest as disruptions that interfere with orbiting satellites or communication and navigation signals used, for example, to guide airplanes, ships and self-driving cars.



Depending on the energy it absorbs from the Sun, the ionosphere grows and shrinks. For that reason, scientists long thought this part of space was only affected by what happens in the space above it.

But over the past decade, a growing body of evidence has indicated the region is much more variable than we can explain with solar activity alone. The ionosphere's contents are not evenly distributed: Dense patches of its charged gases, called plasma, are scattered throughout. Eventually, researchers linked these patches to global weather patterns - large-scale events such as several hurricanes rushing across the ocean at once, or changes in cloud formation over tropical rainforests.

Though the Sun provides the energy that drives weather we experience on Earth, day-to-day weather is driven by something very different: differences in temperature and moisture, interactions between oceans and land, and regions of high and low atmospheric pressure. Still, scientists were surprised to discover that terrestrial weather and the Sun manage to meet in the middle - at the ionosphere - in a tug-of-war for control.

Vast winds high above Earth's surface carry energy around the globe and can modify the ionosphere indirectly by pushing around charged particles in the upper atmosphere. That motion creates an electric field, which guides the behavior of particles throughout the electrically charged ionosphere.

Part of the reason the ionosphere has remained so mysterious until now is the region is difficult to observe. Too high for scientific balloons and too low for satellites, the lower ionosphere especially - where Earth and space are most strongly connected - has eluded much of the technology researchers have used to study near-Earth space. But ICON is uniquely equipped to investigate the region.

"We've had the smoking gun - that indicated terrestrial and space weather are linked - but we've been missing actual observations in the region where these changes are taking place," said Scott England, ICON project scientist at Virginia Tech in Blacksburg, Virginia. "ICON has all the tools to see the drivers and their effects in the system."

From low-Earth orbit, ICON will explore these connections by tracking airglow, a quirk of our planet's upper atmosphere. It refers to the light that shines from the ionosphere, enveloping Earth in a tenuous bubble of red, green and yellow. Airglow is created by a similar process that sparks the aurora: Gas is excited and emits light. Though auroras are typically confined to extreme northern and southern latitudes, airglow shines constantly across the globe, and is much fainter.

"It's amazing that our atmosphere glows like this, but what's more - it gives us a direct ability to make observations of the key parameters we need in order to investigate the connection between the neutral atmosphere and the ionosphere," Immel said.

Different atmospheric gases glow in certain colors and at specific altitudes, so scientists can use airglow to probe the different layers of the atmosphere, gleaning information like density, temperature and composition. In addition, Earth's natural glow helps scientists track motions within the ionosphere itself: As high-altitude winds sweep through the region, pushing its contents around, airglow's dim light morphs in turn, tracing out global patterns.

"I can't wait to see what airglow looks like from ICON's point of view," Immel said.

ICON's 90-minute launch window opens at 3:00 a.m. EST on Nov. 7, 2018. ICON launches on a Northrop Grumman Pegasus XL rocket, which is carried aloft by the Stargazer L-1011 aircraft that takes off from Cape Canaveral Air Force Station in Florida. The L-1011 carries the rocket to approximately 40,000 feet over the open ocean, where it is released and free-falls five seconds before igniting its first-stage rocket motor. Release from the Stargazer is anticipated for 3:05 a.m. EST. The spacecraft deploys approximately 11 minutes after the Pegasus drop.

ICON will join another ionospheric mission, GOLD, short for Global-scale Observations of the Limb and Disk, which launched in January 2018. While ICON flies just 357 miles above Earth and will capture close-up images of the region, GOLD flies in geostationary orbit 22,000 miles above the Western Hemisphere, where it specializes in global-scale images of the ionosphere and upper atmosphere. Where ICON takes close-ups, GOLD captures landscapes.

Together, these missions will provide the most comprehensive ionosphere observations we've ever had - data that's hard to get from Earth, where we can only measure small fractions of the region at a time - enabling a deeper understanding of how our planet interacts with space.

"It's a truly wonderful time to be studying heliophysics," said Nicola Fox, director of NASA's Heliophysics Division in Washington. "We just launched Parker Solar Probe earlier this year, which will give us the first close-up view of what drives the solar wind. Now, with ICON joining our heliophysics system fleet, we will have the incredibly detailed measurements of the ionosphere's response to the solar drivers. This is an amazing opportunity to study the whole system response."

NASA heliophysics missions study a vast interconnected system from the Sun to the space surrounding Earth and other planets, and to the farthest limits of the Sun's constantly flowing stream of solar wind. ICON's observations will provide key information about how Earth's atmosphere is connected to this complex, dynamic system.

ICON is an Explorer-class mission. NASA Goddard manages the Explorers Program for NASA's Heliophysics Division within the Science Mission Directorate in Washington. UC Berkeley's Space Sciences Laboratory developed and operates the ICON mission and built the EUV and FUV imagers. The Naval Research Laboratory in Washington, D.C., developed the MIGHTI instrument, the University of Texas in Dallas developed IVM, and the ICON spacecraft and Pegasus launch vehicle were built by Northrop Grumman in Dulles, Virginia.

Tuesday, November 6, 2018

'Dust up' on International Space Station hints at sources of structure

Imagine looking under your couch and instead of finding fluffy dust bunnies, you see the dust is arranged in straight lines - you might wonder what caused this order. Scientists are experiencing that same feeling, not with dust under a couch, but with electrically charged dust in the microgravity of space. The dust the scientists are studying is made up of tiny spheres 10 times smaller than the width of a human hair. This dust becomes electrically charged when it collects electrons from an energetic gas called a plasma. In a lab on Earth, electrically charged dust generally lines up either along the downward pull of gravity or across it. Scientists at the Center for Astrophysics, Space Physics, and Engineering Research (CASPER), at Baylor University, got a surprise when examining data from a similar experiment on the International Space Station orbiting 248 miles above Earth where gravity is much weaker. Rather than the dust bouncing around randomly, the dust often wiggled around in straight lines, even without gravity. "Gravity on Earth is at least as strong as the electric forces between the dust grains. In microgravity we expected the dust particles to spread out," said Truell Hyde, director of CASPER, who leads the study. "Instead, we found that the small forces between the dust particles and the atoms in the plasma impose order on the system." Dr. Hyde and his research group are presenting their findings at the American Physical Society Division of Plasma Physics meeting in Portland, Ore.


The study was carried out on the PK-4 experiment, short for Plasma Kristall-4, which was built through a partnership between the European Space Agency (ESA) and the Russian Federal Space Agency (Roscosmos). The research is the first project of this kind on the space station with direct involvement of U.S. research groups and is funded by the National Science Foundation and NASA.

Learning that dust grains line up in microgravity is potentially important for understanding how groups of things attain structure. At small sizes, forces between atoms provide structure for molecules and proteins, while at very large sizes gravity provides the structure for stars and galaxies. Hyde said, "This experiment may help explain how structures form when they are between very small and very large sizes."

MetOp-C ready for big day

With liftoff set for 7 November, the latest MetOp weather satellite has been rolled out to the launch pad and positioned on the Soyuz rocket for its ride into space from French Guiana. MetOp-C is the last in the current series of MetOp satellites, following on from MetOp-A and MetOp-B, which were launched in 2006 and 2012, respectively. Launching the satellites sequentially ensures continuous observations of a host of atmospheric variables such as temperature, humidity, trace gases, ozone, and wind speed over the ocean. These data are used mainly for numerical weather prediction - the basis for weather forecasting. Recent studies show that MetOp-A and MetOp-B have already reduced errors in one-day forecasts by as much as 27%. The satellites have all been developed by ESA under a cooperation agreement with EUMETSAT for the space segment of the EUMETSAT Polar System. This is also Europe's contribution to a multi-satellite system shared with the US NOAA agency. While it was envisaged that each successive satellite would take over from its predecessor, their extraordinary quality means that MetOp-A and MetOp-B are still going strong. Once MetOp-C has been launched and commissioned for service, EUMETSAT will have three satellites in the same orbit, equally spaced by 120 . This will benefit weather forecasting even more. MetOp-C has been at Europe's Spaceport in Kourou for a few months being carefully prepared for liftoff and its life in space.


ESA's MetOp-C Project Manager, Stefane Carlier, said, "MetOp is a large satellite carrying an array of instruments. Teams from ESA, EUMETSAT, Airbus Defence and Space and instruments suppliers have been working hard to get to this point.

"We had to say good-bye when the satellite was sealed in the Soyuz fairing and rolled out to the launch pad.

"While it is mainly in the hands of Arianespace for launch, ESA will still be playing a role in its big day, particularly through our teams here in Kourou for the countdown and teams at our operations centre in Germany who are responsible for the mission's first critical days in orbit.

"Ownership of MetOp-C will be transferred to EUMETSAT after liftoff."

MetOp-C will liftoff on 7 November at 00:47 GMT (01:47 CET), 6 November 21:47 local time.