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NASA’s James Webb Space Telescope and Hubble Space Telescope have teamed up to capture new views of Saturn, revealing the planet in strikingly different ways. Observing in complementary wavelengths of light, the two space observatories provide scientists with a richer, more layered understanding of the gas giant’s atmosphere.
Both sense sunlight reflected from Saturn’s banded clouds and hazes, but where Hubble reveals subtle color variations across the planet, Webb’s infrared view senses clouds and chemicals at many different depths in the atmosphere, from the deep clouds to the tenuous upper atmosphere.

Together, scientists can effectively ‘slice’ through Saturn’s atmosphere at multiple altitudes, like peeling back the layers of an onion. Each telescope tells a different part of Saturn’s story, and the observations together help researchers understand how Saturn’s atmosphere works as a connected three-dimensional system. Both complement previous observations done by NASA’s Cassini orbiter during its time studying the Saturnian system from 1997 to 2017.
The Hubble image seen here was captured as part of a more than a decade long monitoring program called OPAL (Outer Planet Atmospheres Legacy) in August 2024, while the Webb image was captured a few months later using Director’s Discretionary Time.
The newly released images highlight features from Saturn’s busy atmosphere.
In the Webb image, a long-lived jet stream known as the “ribbon wave” meanders across the northern mid-latitudes, influenced by otherwise undetectable atmospheric waves. Just below that, a small spot represents a lingering remnant from the “Great Springtime Storm” of 2010 to 2012. Several other storms dotting the southern hemisphere of Saturn are visible in Webb’s image, as well.

All these features are shaped by powerful winds and waves beneath the visible cloud deck, making Saturn a natural laboratory for studying fluid dynamics under extreme conditions.
Several of the pointed edges of Saturn’s iconic hexagon-shaped jet stream at its north pole, discovered by NASA’s Voyager spacecraft in 1981, are also faintly visible in both images. It remains one of the solar system’s most intriguing weather patterns. Its persistence over decades highlights the stability of certain large-scale atmospheric processes on giant planets. These are likely the last high-resolution looks we’ll see of the famous hexagon until the 2040’s, as the northern pole enters winter and will shift into darkness for 15 years.
In Webb’s infrared observations, Saturn’s poles appear distinctly grey-green, indicating light emitting at wavelengths around 4.3 microns. This distinct feature could come from a layer of high-altitude aerosols in Saturn’s atmosphere that scatters light differently at those latitudes. Another possible explanation is auroral activity, as charged molecules interacting with the planet’s magnetic field can produce glowing emissions near the poles.
NASA’s Hubble and Webb have already explored Saturn’s auroras, provided insights into Jupiter’s spectacular auroras also seen with Hubble, confirmed the auroras of Uranus glimpsed in 2011 by Hubble, and detected Neptune’s auroras for the first time with Webb.
In Webb’s infrared image, the rings are extremely bright because they are made of highly reflective water ice. In both images, we’re seeing the sunlit face of the rings, a little less so in the Hubble image, hence the shadows visible underneath on the planet.
There are also subtle ring features such as spokes and structure in the B ring (the thick central region of the rings) that appear differently between the two observatories. The F ring, the outermost ring, looks thin and crisp in the Webb image, while it only slightly glows in the Hubble image.
Saturn’s orbit around the Sun, combined with the position of Earth in its annual orbit, determines our changing viewing angle of Saturn’s face and ring.
These 2024 observations, taken 14 weeks apart, show the planet moving from northern summer toward the 2025 equinox. As Saturn transitions into southern spring, and later southern summer in the 2030’s, Hubble and Webb will have progressively better views of that hemisphere.
Hubble’s observations of Saturn for decades have built a record of its evolving atmosphere. Programs like OPAL, with its annual monitoring, are allowing scientists to track storms, banding patterns, and seasonal shifts over time. Webb now adds powerful infrared capabilities to this ongoing record, extending what researchers can measure about Saturn’s atmospheric structure and dynamic processes.
The James Webb Space Telescope is the world’s premier space science observatory. Webb is solving mysteries in our solar system, looking beyond to distant worlds around other stars, and probing the mysterious structures and origins of our universe and our place in it. Webb is an international program led by NASA with its partners, ESA (European Space Agency) and CSA (Canadian Space Agency).
To learn more about Webb, visit:
The Hubble Space Telescope has been operating for over three decades and continues to make ground-breaking discoveries that shape our fundamental understanding of the universe. Hubble is a project of international cooperation between NASA and ESA (European Space Agency). NASA’s Goddard Space Flight Center in Greenbelt, Maryland, manages the telescope and mission operations. Lockheed Martin Space, based in Denver, also supports mission operations at Goddard. The Space Telescope Science Institute in Baltimore, which is operated by the Association of Universities for Research in Astronomy, conducts Hubble science operations for NASA.
To learn more about Hubble, visit:
The following sections contain links to download this article’s images and videos in all available resolutions followed by related information links, media contacts, and if available, research paper and Spanish translation links.
Read more: NASA’s Saturn webpage
Read more: Exploring Our Solar System with Webb
Watch: Exploring Our Solar System with Dr. Amy Simon
Read more: Webb’s Titan Forecast: Partly Cloudy With Occasional Methane Showers
Watch: ViewSpace: Image Tour: Saturn
Laura Betz
NASA’s Goddard Space Flight Center
Greenbelt, Maryland
laura.e.betz@nasa.gov
Hannah Braun
Space Telescope Science Institute
Baltimore, Maryland
Christine Pulliam
Space Telescope Science Institute
Baltimore, Maryland
2026-03-25 16:10
5 min read

For the first time, astronomers have directly measured the speed of superheated gas billowing from a cauldron of stellar activity at the heart of M82, a nearby galaxy undergoing an extraordinary burst of star formation.
The material is moving more than 2 million miles (over 3 million kilometers) per hour and appears to be the primary force driving a cooler, well-studied, galaxy-scale wind.
Researchers made the calculations using data from the Resolve instrument aboard the XRISM (X-ray Imaging and Spectroscopy Mission) spacecraft.
“The classic model of starburst galaxies like M82 suggests that shock waves from star formation and supernovae near the center heat gas, kick-starting a powerful wind,” said Erin Boettcher, an astrophysicist at the University of Maryland, College Park and NASA’s Goddard Space Flight Center in Greenbelt, Maryland. “Prior to XRISM, though, we didn’t have the ability to measure the velocities needed to test that hypothesis. Now we see the gas moving even faster than some models predict, more than enough to drive the wind all the way to the edge of the galaxy.”
A paper about the result, led by Boettcher, published Wednesday, March 25, in Nature. The XRISM mission is led by JAXA (Japan Aerospace Exploration Agency) in collaboration with NASA, along with contributions from ESA (European Space Agency). NASA and JAXA also codeveloped the Resolve instrument.
Sometimes called the Cigar galaxy, M82 is located 12 million light-years away in the northern constellation Ursa Major. Astronomers classify it as a starburst galaxy because it’s forming stars at a much higher rate than typical for its size — about 10 times faster than the Milky Way.
M82 is well known for its extended, cool wind, which stretches out to 40,000 light-years and propels huge quantities of gas and dust. Scientists have studied it with many missions, including NASA’s Chandra, Webb, Hubble, and retired Spitzer space telescopes, trying to connect the dots between the stellar activity and the large-scale outflow.
Researchers particularly want to understand the role of cosmic rays. These high-speed charged particles are found throughout the cosmos and are accelerated by some of the same events scientists think produce winds like in M82. There’s a possibility they are a main source of outward pressure on the gas.
The XRISM Resolve instrument’s high resolution and sensitivity allowed Boettcher and her colleagues to accurately measure the speed of the hot wind by looking at an X-ray signal from superheated iron in the galactic center.
The amount of X-ray light from iron and other elements told them the temperature — right within predictions at 45 million degrees Fahrenheit (25 million degrees Celsius). The heat exerts pressure on the gas and pushes it outward. This rushing from high pressure to low pressure forms the wind — the same reason winds blow through Earth’s atmosphere.

The broadness of iron spectral lines conveyed the hot wind’s speed. This works through Doppler shifting, the same phenomenon that causes the pitch of a sound, like a siren, to rise or fall due to the source’s motion toward or away from you. In the case of M82, the hot material near the center flies quickly in both directions, stretching out the iron’s spectral line. The amount of stretching reveals the iron’s velocity. The researchers found that the wind is a little faster than expected. Combined with the high temperature, it’s powerful enough to produce the cool wind without cosmic rays, although they may still be contributing.
The researchers calculate that the center of M82 expels enough gas every year to form seven stars with the mass of our Sun. This presents another puzzle.
“If the wind blows steadily at the speed we’ve measured, then we think it can power the larger, cooler wind by driving out four solar masses of gas a year. But XRISM tells us much more gas is moving outward,” said co-author Edmund Hodges-Kluck, an astronomer and XRISM team member at NASA Goddard. “Where do the three extra solar masses go? Do they escape out of the galaxy as hot gas some other way? We don’t know.”
The XRISM satellite’s observations of M82 will help improve models of starburst galaxies, which may help scientists answer these types of questions in the future. NASA’s contributions to international projects like XRISM are part of the agency’s efforts to innovate with ambitious science missions that will help us better understand how our cosmos works.
“Some of our early models of starburst galaxies were developed in the 1980s, and we’re finally able to test them in ways that weren’t possible before XRISM,” said co-author Skylar Grayson, a graduate student at Arizona State University in Tempe. “It provides opportunities to figure out why the model might not be capturing everything that’s going on in the real universe.”
By Jeanette Kazmierczak
NASA’s Goddard Space Flight Center, Greenbelt, Md.
Media Contact:
Claire Andreoli
301-286-1940
NASA’s Goddard Space Flight Center, Greenbelt, Md.
2026-03-25 16:00
5 min read
The highly competitive NASA Hubble Fellowship Program (NHFP) recently named 24 new fellows to its 2026 class. The NHFP enables outstanding postdoctoral scientists to pursue independent research in any area of NASA Astrophysics, using theory, observations, simulations, experimentation, or instrument development. Over 650 applicants vied for the 2026 fellowships, representing an oversubscription rate of 27 to 1. Each fellowship provides the awardee up to three years of support at a U.S. institution.
Once selected, fellows are named to one of three sub-categories corresponding to three broad scientific questions that NASA seeks to answer about the universe:
“The 2026 class of the NASA Hubble Fellowship Program is comprised of outstanding astrophysics researchers who will advance NASA’s pursuit of big questions about how the universe works, how it evolved over time, and whether we’re alone in it,” said Shawn Domagal-Goldman, Astrophysics Division director, NASA Headquarters, Washington. “Through their compelling research, and by sharing the products of that work with the broader community, this year’s fellows will once again play an important role in creating our future and in inspiring future generations of students to be a part of that future. These scientists across the country will enhance the impact of U.S. academic institutions and will further American leadership in space-based astrophysics research.”
The list below provides the names of the 2026 awardees, their fellowship host institutions, and their proposed research topics.
The 2026 NHFP Einstein Fellows are:
The 2026 NHFP Hubble Fellows are:
The 2026 NHFP Sagan Fellows are:
An important part of the NHFP is the annual symposium, which allows Fellows the opportunity to present results of their research, and to meet each other and the scientific and administrative staff who manage the program. The 2025 symposium was held at the Space Telescope Science Institute in Baltimore. Topics ranged from understanding the atmospheric chemistry of nearby, rocky planets with NASA’s James Webb Space Telescope to observations of some of the earliest galaxies in the universe, and mapping the expansion of our universe with the latest data releases from the Dark Energy Spectroscopic Instrument.
More information about the 2026 NHFP Fellows is available online.
The Space Telescope Science Institute in Baltimore, Maryland, administers the NHFP on behalf of NASA, in collaboration with the Chandra X-ray Center at the Smithsonian Astrophysical Observatory in Cambridge, Massachusetts, and the NASA Exoplanet Science Institute and the Jet Propulsion Laboratory, in Pasadena, California.
Claire Andreoli
NASA’s Goddard Space Flight Center
Greenbelt, Maryland
claire.andreoli@nasa.gov
Ann Jenkins, Christine Pulliam
Space Telescope Science Institute
Baltimore, Maryland
2026-03-25 15:51
Seattle and Portland, Oregon, are among the cloudiest cities in the United States. But that infamous cloud cover is no match for the U.S.-Indian Earth satellite NISAR (NASA-ISRO Synthetic Aperture Radar), which is designed to peer straight through clouds. Doing so allows scientists to study the Pacific Northwest’s natural landmarks and bustling port cities like never before.
Comparing the highly detailed imagery from the NISAR mission over time can reveal subtle changes in forests, wetlands, urban areas, and infrastructure. Radar images from the satellite — a joint effort between NASA and the Indian Space Research Organisation (ISRO) — can also detect subtle motions associated with volcanic activity, glacier movement, slips along faults, and slow-moving landslides.
“The Pacific Northwest is home to millions of people and supports major industries from tech and aerospace to agriculture and forestry,” said remote sensing technologist Brandi Downs of NASA’s Jet Propulsion Laboratory in Southern California, who helped process the NISAR imagery. “This recent imagery highlights how NISAR data can support resource management, natural-hazard monitoring, and environmental decision-making.”
Built by JPL, NISAR’s L-band radar uses microwaves that can pass uninterrupted through clouds and, thanks to its 39-foot (12-meter) antenna reflector, provides a high level of detail for anyone who wants to understand how a region’s surface and natural resources are changing. These radar signals, sent toward the Earth’s surface, are reflected off the ground and back to the spacecraft, a phenomenon called backscatter. By measuring changes in the reflected signal, scientists can identify properties on the surface like moisture, vegetation, and variations in terrain.
Radar images don’t capture true color the same way photographs do. Instead, the colors seen here represent different combinations and intensities of radar signals or their orientation. The latter is called polarization.
Captured Nov. 10, 2025, the Pacific Northwest imagery shows the waterways around Portland and Seattle, with the roadways and cityscapes built alongside them. Some of these areas are dotted in magenta due to radar signals strongly reflecting off flat surfaces like roads and buildings. The small areas of yellow may be produced by a range of factors, including land cover, soil moisture, and surface geometry.
With radar images like these, scientists can look for changes in backscatter over time to tell where trees and plants have been removed, regrown, or destroyed, and to estimate how much carbon is stored in forests. Monitoring the boundaries of water and wetlands provides insight into flood risks or shifts in river channels.
Yellow-green in the imagery indicates the forests and wetlands covering the region. Those are interrupted by the dark blue peaks of Mount Rainier and Mount Saint Helens, two of the best-known natural landmarks in the Pacific Northwest. Dark blue is representative of relatively smooth surfaces, including both water and exposed mountaintops. Near the foot of each mountain are patches of purple squares cut into the lighter-green vegetation. Their precise right angles indicate that they’re human-made, and most likely the effect of forests being thinned or vegetation growing back after having been thinned in the past.
“A single radar image is a snapshot of the surface conditions,” Downs said. “But scientists typically rely on a time series of images to understand what’s happening. One of NISAR’s strengths is it observes the same areas twice every 12 days, producing a sequence of radar measurements that tells a full story.”
A joint mission developed by NASA and ISRO, NISAR was launched in July 2025 from Satish Dhawan Space Centre on India’s southeastern coast. Managed by Caltech, JPL leads the U.S. component of the project and provided the satellite’s L-band SAR, with a wavelength of 9 inches (24 centimeters), and antenna reflector. The spacecraft bus, the S-band SAR, which operates at a wavelength of 4 inches (10 centimeters), as well as the launch vehicle and launch services were provided by ISRO.
The NISAR satellite is the first to carry two SAR instruments at different wavelengths and monitors Earth’s land and ice surfaces twice every 12 days, collecting data using the spacecraft’s giant drum-shaped reflector, the largest radar antenna reflector NASA has ever sent into space.
To learn more about NISAR, visit:
https://science.nasa.gov/mission/nisar/
Media Contacts
Andrew Good / Andrew Wang
Jet Propulsion Laboratory, Pasadena, Calif.
818-393-2433 / 626-379-6874
andrew.c.good@jpl.nasa.gov / andrew.wang@jpl.nasa.gov
2026-019
2026-03-25 04:01




January 25, 2026 – March 14, 2026
Back-to-back low-pressure systems struck Hawaii in March 2026, delivering some of the worst flooding the state has seen in decades. The subtropical weather systems—called kona lows near Hawaii—siphoned moisture from the tropics, fueling slow-moving thunderstorms with torrential, destructive rains.
The National Weather Service reported rainfall totals of 5 to 10 inches (13 to 26 centimeters) throughout the state between March 11 and 15, with some areas seeing more than 30 inches. Weather stations in Honolulu, Hilo, Līhuʻe, and Kahului all broke daily rainfall records.
The satellite image on the right shows swamped neighborhoods and farmland between Mokuleia and Waialua on the island of O’ahu on March 14, 2026, after the first and more destructive storm system hit the island. Plumes of suspended sediment have discolored waters in and around Kaiaka Bay. Hawaii’s volcanic Hilo soils are known for being red due to the high levels of iron and aluminum oxide that accumulate as they weather. For comparison, the image on the left shows the same area on January 25, 2026, before the deluge.
Preliminary assessments indicate that hundreds of homes in O’ahu sustained damage. Farmers on the island and across the state reported millions of dollars in damage, according to news reports. The storm produced widespread wind gusts between 60 and 75 miles (97 and 121 kilometers) per hour, with gusts in some places reaching 100 miles per hour. As many as 115,000 O’ahu residents faced power outages in the storm’s aftermath.
While the most intense rains had subsided by March 24, forecasters are continuing to monitor unsettled weather and the possibility of more flash floods in the coming days.
NASA’s Disasters Response Coordination System has been activated to support the Hawaii Emergency Management Agency’s response to the storms. The team will be posting maps and data products on its open-access mapping portal as new information becomes available.
NASA Earth Observatory images by Lauren Dauphin, using Landsat data from the U.S. Geological Survey. Story by Adam Voiland.
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