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By NASA
5 min read
NASA, ESA Missions Help Scientists Uncover How Solar Wind Gets Energy
Since the 1960s, astronomers have wondered how the Sun’s supersonic “solar wind,” a stream of energetic particles that flows out into the solar system, continues to receive energy once it leaves the Sun. Now, thanks to a lucky lineup of a NASA and an ESA (European Space Agency)/NASA spacecraft both currently studying the Sun, they may have discovered the answer — knowledge that is a crucial piece of the puzzle to help scientists better forecast solar activity between the Sun and Earth.
A paper published in the Aug. 30, 2024, issue of the journal Science provides persuasive evidence that the fastest solar winds are powered by magnetic “switchbacks,” or large kinks in the magnetic field, near the Sun.
“Our study addresses a huge open question about how the solar wind is energized and helps us understand how the Sun affects its environment and, ultimately, the Earth,” said Yeimy Rivera, co-leader of the study and a postdoctoral fellow at the Smithsonian Astrophysical Observatory, part of Center for Astrophysics | Harvard & Smithsonian. “If this process happens in our local star, it’s highly likely that this powers winds from other stars across the Milky Way galaxy and beyond and could have implications for the habitability of exoplanets.”
This artist’s concept shows switchbacks, or large kinks in the Sun’s magnetic field. NASA’s Goddard Space Flight Center/Conceptual Image Lab/Adriana Manrique Gutierrez Previously, NASA’s Parker Solar Probe found that these switchbacks were common throughout the solar wind. Parker, which became the first craft to enter the Sun’s magnetic atmosphere in 2021, allowed scientists to determine that switchbacks become more distinct and more powerful close to the Sun. Up to now, however, scientists lacked experimental evidence that this interesting phenomenon actually deposits enough energy to be important in the solar wind.
“About three years ago, I was giving a talk about how fascinating these waves are,” said co-author Mike Stevens, astrophysicist at the Center for Astrophysics. “At the end, an astronomy professor stood up and said, ‘that’s neat, but do they actually matter?’”
To answer this, the team of scientists had to use two different spacecraft. Parker is built to fly through the Sun’s atmosphere, or “corona.” ESA’s and NASA’s Solar Orbiter mission is also on an orbit that takes it relatively close to the Sun, and it measures solar wind at larger distances.
The discovery was made possible because of a coincidental alignment in February 2022 that allowed both Parker Solar Probe and Solar Orbiter to measure the same solar wind stream within two days of each other. Solar Orbiter was almost halfway to the Sun while Parker was skirting the edge of the Sun’s magnetic atmosphere.
This conceptual image shows Parker Solar Probe about to enter the solar corona. NASA/Johns Hopkins APL/Ben Smith An artist’s concept shows Solar Orbiter near the Sun. NASA’s Goddard Space Flight Center Conceptual Image Lab
“We didn’t initially realize that Parker and Solar Orbiter were measuring the same thing at all. Parker saw this slower plasma near the Sun that was full of switchback waves, and then Solar Orbiter recorded a fast stream which had received heat and with very little wave activity,” said Samuel Badman, astrophysicist at the Center for Astrophysics and the other co-lead of the study. “When we connected the two, that was a real eureka moment.”
Scientists have long known that energy is moved throughout the Sun‘s corona and the solar wind, at least in part, through what are known as “Alfvén waves.” These waves transport energy through a plasma, the superheated state of matter that makes up the solar wind.
However, how much the Alfvén waves evolve and interact with the solar wind between the Sun and Earth couldn’t be measured — until these two missions were sent closer to the Sun than ever before, at the same time. Now, scientists can directly determine how much energy is stored in the magnetic and velocity fluctuations of these waves near the corona, and how much less energy is carried by the waves farther from the Sun.
The new research shows that the Alfvén waves in the form of switchbacks provide enough energy to account for the heating and acceleration documented in the faster stream of the solar wind as it flows away from the Sun.
“It took over half a century to confirm that Alfvenic wave acceleration and heating are important processes, and they happen in approximately the way we think they do,” said John Belcher, emeritus professor from the Massachusetts Institute of Technology who co-discovered Alfvén waves in the solar wind but was not involved in this study.
In addition to helping scientists better forecast solar activity and space weather, such information helps us understand mysteries of the universe elsewhere and how Sun-like stars and stellar winds operate everywhere.
“This discovery is one of the key puzzle pieces to answer the 50-year-old question of how the solar wind is accelerated and heated in the innermost portions of the heliosphere, bringing us closer to closure to one of the main science objectives of the Parker Solar Probe mission,” said Adam Szabo, Parker Solar Probe mission science lead at NASA.
By Megan Watzke
Center for Astrophysics | Harvard & Smithsonian
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Last Updated Aug 30, 2024 Related Terms
Goddard Space Flight Center Heliophysics Heliophysics Division Parker Solar Probe (PSP) Science & Research Science Mission Directorate Solar Flares Solar Orbiter Solar Science Solar Wind Space Weather The Sun The Sun & Solar Physics Explore More
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By NASA
Research astrophysicist Regina Caputo puzzles out how the universe works by studying the most extreme events in the cosmos.
Name: Regina Caputo
Title: Research Astrophysicist
Organization: Astroparticle Physics Laboratory (Code 661)
Regina Caputo is a research astrophysicist at NASA’s Goddard Space Flight Center in Greenbelt, Md. She focuses on technology development and support for gamma-ray telescopes.Photo credit: NASA/David Friedlander What do you do and what is most interesting about your role here at Goddard?
I’m a research astrophysicist in the particle astrophysics lab at Goddard. I’m really interested in the most extreme events that happen in the universe, so I work on current gamma-ray missions and develop technology for future gamma-ray telescopes.
The most exciting part of my work is trying to figure out how the universe works and how it got the way it is today.
What is your educational background?
In 2006, I got my bachelor’s degree in engineering physics from the Colorado School of Mines. Then, in 2011 I got my Ph.D. in particle physics from Stony Brook University.
I’ve always been inclined to bridge the gap between science and engineering, so my undergraduate education was where I learned to build things, develop instruments, and analyze data. Then, through my Ph.D. program, I started trying to understand the fundamental building blocks of matter. Eventually, I found my way to astro-particle physics. Particles on the ground are cool, but particles in space are even cooler!
What brought you to Goddard?
I arrived at Goddard in 2017, and I think it was a natural confluence of building telescopes, doing high energy astrophysics, and working in a collaborative environment.
What were the most exciting moments of your career?
I am very fortunate because there have been a couple exciting moments. I was a student working on CERN’s Large Hadron Collider when the Higgs Boson was discovered, so that was really exciting.
Then, after I had gotten into particle astrophysics, we discovered in 2017 that merging neutron stars created gravitational waves and gamma-ray bursts. Around the same time, we discovered an active galaxy that produced neutrinos with ultra-high-energy gamma-ray flares. This was like the birth of multi-messenger astrophysics, so it felt like a whole new era of discovery. I really felt like the universe was telling me something.
How does your work involve different teams?
I’m on a few different teams on different scales. On the science side, I’m a part of the Fermi Large Area Telescope (LAT) collaboration — an international group of scientists supporting Fermi, analyzing data, and doing science.
I’m also a Swift Observatory project scientist. I support the mission by making sure it’s fulfilling its obligations to the public and various stakeholders.
The technology development teams are the ones that I’m leading in preparation for a next-generation gamma-ray telescope. I have a group of postdocs, students, and other scientists — 10 or 15 people around the world. We are developing and characterizing silicon CMOS detectors, called AstroPix, to make sure that they meet our requirements, and think about the next steps to implement them in different experiments.
The other team, called Compton-Pair Telescope (ComPair), built a prototype gamma-ray telescope that was launched as a balloon payload last summer. Right now, we’re working on the next generation of it.
Regina Caputo at the August 2023 ComPair balloon launch in Fort Sumter, New Mexico. ComPair is a prototype gamma-ray telescope that can measure and detect gamma-rays.Photo courtesy of Regina Caputo What is challenging about your position?
I think one of the most challenging things is communicating effectively with an international group of people. You have to be like an events coordinator to make sure people have the resources they need.
What role do you serve for early career scientists?
I think it’s really important that scientists think about the next generation of scientists and technically minded people. It’s really important to me to make sure that we are giving junior folks the field opportunities they need to achieve their goals.
What science outreach do you do?
I really enjoy science outreach, so I like to jump in whenever there’s an opportunity — like Black Hole Week, career days, or public talks. I like to be able to say, “Hey, you’re paying us to explore the universe — here’s what we found!”
What goals do you have for the future?
It would be so cool to see the detectors we develop to be in a next-generation gamma-ray telescope that flies and takes data. It’s a hard goal, but hey, I shoot for the stars.
By Laine Havens
NASA’s Goddard Space Flight Center in Greenbelt, Md.
Conversations With Goddard is a collection of Q&A profiles highlighting the breadth and depth of NASA’s Goddard Space Flight Center’s talented and diverse workforce. The Conversations have been published twice a month on average since May 2011. Read past editions on Goddard’s “Our People” webpage.
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Last Updated Aug 09, 2024 EditorMadison OlsonContactRob Garnerrob.garner@nasa.govLocationGoddard Space Flight Center Related Terms
People of Goddard Astrophysics Goddard Space Flight Center People of NASA The Universe Explore More
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By NASA
6 min read
Quantum Scale Sensors used to Measure Planetary Scale Magnetic Fields
Magnetic fields are everywhere in our solar system. They originate from the Sun, planets, and moons, and are carried throughout interplanetary space by solar wind. This is precisely why magnetometers—devices used to measure magnetic fields—are flown on almost all missions in space to benefit the Earth, Planetary, and Heliophysics science communities, and ultimately enrich knowledge for all humankind. These instruments can remotely probe the interior of a planetary body to provide insight into its internal composition, structure, dynamics, and even evolution based on the magnetic history frozen into the body’s crustal rock layers. Magnetometers can even discover hidden oceans within our solar system and help determine their salinity, thereby providing insight into the potential habitability of these icy worlds.
Left: The magnetic field of Jupiter provides insight into its interior composition, structure, dynamics, and even its evolutionary history. Right: Image of the first prototype 4H-SiC solid-state magnetometer sensor die (2mm by 2mm) developed by NASA-GRC. Each gold rectangle or square on the surface represents an individual sensor, the smallest being 10 microns by 10 microns. Fluxgates are the most widely used magnetometers for missions in space due to their proven performance and simplicity. However, the conventional size, weight, and power (SWaP) of fluxgate instruments can restrict them from being used on small platforms like CubeSats and sometimes limit the number of sensors that can be used on a spacecraft for inter-sensor calibration, redundancy, and spacecraft magnetic field removal. Traditionally, a long boom is used to distance the fluxgate magnetometers from the contaminate magnetic field generated by the spacecraft, itself, and at least two sensors are used to characterize the falloff of this field contribution so it can be removed from the measurements. Fluxgates also do not provide an absolute measurement, meaning that they need to be routinely calibrated in space through spacecraft rolls, which can be time and resource intensive.
An SMD-funded team at NASA’s Jet Propulsion Laboratory in Southern California has partnered with NASA’s Glenn Research Center in Cleveland, Ohio to prototype a new magnetometer called the silicon carbide (SiC) magnetometer, or SiCMag, that could change the way magnetic fields are measured in space. SiCMag uses a solid-state sensor made of a silicon carbide (SiC) semiconductor. Inside the SiC sensor are quantum centers—intentionally introduced defects or irregularities at an atomic scale—that give rise to a magnetoresistance signal that can be detected by monitoring changes in the sensor’s electrical current, which indicate changes in the strength and direction of the external magnetic field. This new technology has the potential to be incredibly sensitive, and due to its large bandgap (i.e., the energy required to free an electron from its bound state so it can participate in electrical conduction), is capable of operating in the wide range of temperature extremes and harsh radiation environments commonly encountered in space.
Team member David Spry of NASA Glenn indicates, “Not only is the SiC material great for magnetic field sensing, but here at NASA Glenn we’re further developing robust SiC electronics that operate in hot environments far beyond the upper temperature limitations of silicon electronics. These SiC-based technologies will someday enable long-duration robotic scientific exploration of the 460 °C Venus surface.”
SiCMag is also very small— the sensor area is only 0.1 x 0.1 mm and the compensation coils are smaller than a penny. Consequently, dozens of SiCMag sensors can easily be incorporated on a spacecraft to better remove the complex contaminate magnetic field generated by the spacecraft, reducing the need for a long boom to distance the sensors from the spacecraft, like implemented on most spacecraft, including Psyche (see figure below).
The magnetic field lines associated with the Psyche spacecraft, modeled from over 200 individual magnetic sources. Removing this magnetic field contribution from the measurements conventionally requires the use of two fluxgate sensors on a long boom. Incorporating 4 or more SiCMag sensors in such a scenario would significantly reduce the size of the boom required, or even remove the need for a boom completely. Image Credit: This image was adopted from https://science.nasa.gov/resource/magnetic-field-of-the-psyche-spacecraft/ SiCMag has several advantages when compared to fluxgates and other types of heritage magnetometers including those based on optically pumped atomic vapor. SiCMag is a simple instrument that doesn’t rely on optics or high-frequency components, which are sensitive to temperature variations. SiCMag’s low SWaP also allows for accommodation on small platforms such as CubeSats, enabling simultaneous spatial and temporal magnetic field measurements not possible with single large-scale spacecraft. This capability will enable planetary magnetic field mapping and space weather monitoring by constellations of CubeSats. Multiplatform measurements would also be very valuable on the surface of the Moon and Mars for crustal magnetic field mapping, composition identification, and magnetic history investigation of these bodies.
SiCMag has a true zero-field magnetic sensing ability (i.e., SiCMag can measure extremely weak magnetic fields), which is unattainable with most conventional atomic vapor magnetometers due to the requisite minimum magnetic field needed for the sensor to operate. And because the spin-carrying electrons in SiCMag are tied up in the quantum centers, they won’t escape the sensor, meaning they are well-suited for decades-long journeys to the ice-giants or to the edges of the heliosphere. This capability is also an advantage of SiCMag’s optical equivalent sibling, OPuS-MAGNM, an optically pumped solid state quantum magnetometer developed by Hannes Kraus and matured by Andreas Gottscholl of the JPL solid-state magnetometry group. SiCMag has the advantage of being extremely simple, while OPuS-MAGNM promises to have lower noise characteristics, but uses complex optical components.
According to Dr. Andreas Gottscholl, “SiCMag and OPuS-MAGNM are very similar, actually. Progress in one sensor system translates directly into benefits for the other. Therefore, enhancements in design and electronics advance both projects, effectively doubling the impact of our efforts while we are still flexible for different applications.”
SiCMag has the ability to self-calibrate due to its absolute sensing capability, which is a significant advantage in the remote space environment. SiCMag uses a spectroscopic calibration technique that atomic vapor magnetometers also leverage called magnetic resonance (in the case of SiCMag, the magnetic resonance is electrically detected) to measure the precession frequency of electrons associated with the quantum centers, which is directly related to the magnetic field in which the sensor is immersed. This relationship is a fundamental physical constant in nature that doesn’t change as a function of time or temperature, making the response ideal for calibration of the sensor’s measurements. “If we are successful in achieving the sought-out sensitivity improvement we anticipate using isotopically purer materials, SiC could change the way magnetometry is typically performed in space due to the instrument’s attractive SWaP, robustness, and self-calibration ability,” says JPL’s Dr. Corey Cochrane, principal investigator of the SiCMag technology.
The 3-axis 3D printed electromagnet – no larger than the size of a US penny – is used to modulate and maintain a region of zero magnetic field around our 0.1 mm x 0.1 mm 4H-SiC solid-state sensor. NASA has been funding this team’s solid-state quantum magnetometer sensor research through its PICASSO (Planetary Instrument Concepts for the Advancement of Solar System Observations) program since 2016. A variety of domestic partners from industry and academia also support this research, including NASA’s Glenn Research Center in Cleveland, Penn State University, University of Iowa, QuantCAD LLC, as well as international partners such as Japan’s Quantum Materials and Applications Research Center (QUARC) and Infineon Technologies.
The SiC magnetometer team leads from JPL and GRC (left: Dr. Hannes Kraus, middle: Dr. Phillip Neudeck, right: Dr. Corey Cochrane) at the last International Conference on Silicon Carbide and Related Materials (ICSCRM) where their research is presented annually. Acknowledgment: The research was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration (80NM0018D0004) and the NASA Glenn Research Center.
Project Lead(s):
Dr. Corey Cochrane, Dr. Hannes Kraus, Jet Propulsion Laboratory/California Institute of Technology
Dr. Phil Neudeck, David Spry, NASA Glenn Research Center
Sponsoring Organization(s):
Science Mission Directorate PICASSO, JPL R&D fund
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Last Updated Aug 06, 2024 Related Terms
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By NASA
5 Min Read ‘Current’ Events: NASA and USGS Find a New Way to Measure River Flows
The River Observing System (RiOS) tracking the motion of water surface features from above a section of the Sacramento River in Northern California in 2023. Credits: NASA/USGS/Joe Adams and Chris Gazoorian A team of scientists and engineers at NASA and the U.S. Geological Survey (USGS) collaborated to see if a small piloted drone, equipped with a specialized payload, could help create detailed maps of how fast water is flowing. Rivers supply fresh water to our communities and farms, provide homes for a variety of creatures, transport people and goods, and generate electricity. But river flows can also carry pollutants downstream or suddenly surge, posing dangers to people, wildlife, and property. As NASA continues its ongoing commitment to better understand our home planet, researchers are working to answer the question of how do we stay in-the-know about where and how quickly river flows change?
NASA and USGS scientists have teamed up to create an instrument package – about the size of a gallon of milk – called the River Observing System (RiOS). It features thermal and visible cameras for tracking the motion of water surface features, a laser to measure altitude, navigation sensors, an onboard computer, and a wireless communications system. In 2023, researchers took RiOS into the field for testing along a section of the Sacramento River in Northern California, and plan to return for a third and final field test in the fall of 2024.
The River Observing System (RiOS) tracking the motion of water surface features from above a section of the Sacramento River in Northern California in 2023. “Deploying RiOS above a river to evaluate the system’s performance in a real-world setting is incredibly important,” said Carl Legleiter, USGS principal investigator of the joint NASA-USGS StreamFlow project. “During these test flights we demonstrated that the onboard payload can be used to make calculations – do the analysis – in nearly real-time, while the drone is flying above the river. This was one of our top-tier goals: to enable minimal latency between the time we acquire images and when we have detailed information on current speeds and flow patterns within the river.”
To realize this vision for onboard computing, the team uses open-source software, combined with their own code, to produce maps of water surface velocities, or flow field, from a series of images taken over time.
“You might think that we need to be able to see discrete, physical objects – like sticks or silt or other debris as they move downstream – to estimate the flow velocity, but that’s not always the case, nor is it always possible,” said Legleiter. “Using a highly-sensitive infrared camera, we instead detect the movement of subtle differences in the temperature of water carried downstream.”
Those same tiny temperature differences also appear wherever there are undulations – like at the boundary between the air and the water or ice below. Knowing this, NASA members of the StreamFlow team used this phenomenon to their advantage when developing methods for possible future landed planetary missions to navigate at distant and hard-to-see environments, including Europa, the icy moon orbiting Jupiter.
Our technology can precisely track the static surface of icy terrain while flying over it, or a moving surface, like water, while hovering above it to keep the spacecraft safe while gathering valuable data
uland wong
Co-investigator and NASA lead of the StreamFlow Project
“Icy surfaces present challenging visual conditions such as lack of contrast,” said Uland Wong, co-investigator and NASA lead of the StreamFlow project at NASA’s Ames Research Center in California’s Silicon Valley. “Our technology can precisely track the static surface of icy terrain while flying over it, or a moving surface, like water, while hovering above it to keep the spacecraft safe while gathering valuable data.”
To prepare for the Sacramento River field tests, the NASA team built a robotics simulator to run thousands of virtual drone flights over the Sacramento River test site using flow fields modeled by USGS. These simulations are helping the team create intelligent software capable of selecting the best routes for the drone to fly and ensuring efficient use of limited battery power.
The next step in the partnership is for NASA to develop techniques for making the system more autonomous. The researchers want to use calculations of river flows – performed onboard in real time – to guide where the drone should fly next.
“Does the drone drop down to get better resolution data about a particular location or stay high and capture a wide-angle view,” posed Wong. “If it identifies areas that are flowing particularly fast or slow, could the drone more quickly detect areas of flooding?”
The USGS currently operates an extensive network of thousands of automated stream gauges and fixed cameras installed on bridges and riverbanks to monitor river flows in real-time across the country.
“Drones could enable us to make measurements in so many more areas, potentially allowing our network to be larger, more robust, and safer for our technicians to monitor and maintain,” said Paul Kinzel, StreamFlow co-investigator at USGS. “Drones could help keep our people and equipment out of harm’s way in addition to telling us how the environment is changing over time in as many locations as possible.”
A drone with the StreamFlow thermal mapping payload flying above the Sacramento River in Northern California.NASA/Massimo Vespignani For more information about how NASA improves life on Earth through climate and technological innovations, visit:
http://www.nasa.gov/earth
The StreamFlow project is a collaboration between researchers with the USGS’s Hydrologic Remote Sensing Branch, Unmanned Aircraft Systems engineers with the USGS National Innovation Center, and scientists in the Intelligent Robotics Group at NASA Ames. The Streamflow payload concept was demonstrated through research initially seeded by a grant from the USGS National Innovation Center and is now supported by NASA’s Advanced Information Systems Technology program, which is managed by the agency’s Earth Science Technology Office. The field tests were conducted in collaboration with the National Oceanographic and Atmospheric Administration (NOAA) Southwest Fisheries Science Center, which helped collect direct field measurements of the river’s flow velocity and granted access to the field site, which is owned by the Nature Conservancy.
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Last Updated Aug 05, 2024 Related Terms
Earth Science Division Ames Research Center Applied Sciences Program Drones & You General USGS (United States Geological Survey) Keep Exploring Discover More Topics From NASA
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