X-ray: NASA/CXC/SAO/Sejong Univ./Hur et al; JWST: ESA/Webb, NASA & CSA, V. Almendros-Abad, M. Guarcello, K. Monsch, and the EWOCS team. Image Processing: NASA/CXC/SAO/L. Frattare and K. Arcand
This image of Westerlund 2 released on March 19, 2026, features Chandra X-ray Observatory data (pink) and infrared data from NASA’S James Webb Space Telescope (red, orange, green, cyan, and blue). Scores of gleaming stars ringed in neon pink stretch across the frame, highlighting a cluster where stars are between one and three million years old. Brick-orange dust clouds along the bottom edge illustrate the raw materials of this active stellar nursery.
Westerlund 2 resides in a raucous stellar breeding ground known as Gum 29, located 20,000 light-years away from Earth in the constellation Carina.
Image credit: X-ray: NASA/CXC/SAO/Sejong Univ./Hur et al; JWST: ESA/Webb, NASA & CSA, V. Almendros-Abad, M. Guarcello, K. Monsch, and the EWOCS team. Image Processing: NASA/CXC/SAO/L. Frattare and K. Arcand
Atmospheric gravity waves generated by Super Typhoon Sinlaku are visible via mesospheric airglow in this nighttime image acquired with the VIIRS (Visible Infrared Imaging Radiometer Suite) on the NOAA-20 satellite on April 12, 2026, Universal Time (April 13 local time).
NASA Earth Observatory/Michala Garrison
In mid-April 2026, Super Typhoon Sinlaku churned across the North Pacific Ocean and brought heavy rain and flooding to the Mariana Islands. The storm reached “violent typhoon” status—the highest intensity on the scale used by the Japan Meteorological Agency and roughly equivalent to a category 5 storm on the Saffir-Simpson wind scale. Sinlaku was one of only a handful of tropical cyclones of that intensity known to have occurred so early in the year in the region, meteorologists noted.
Sinlaku rapidly intensified over the ocean before its impacts reached land. Around the time of this strengthening, satellites began to detect that the typhoon’s effects also extended upward, into the upper atmosphere.
The nighttime image above, acquired with the VIIRS (Visible Infrared Imaging Radiometer Suite) on the NOAA-20 satellite, shows atmospheric gravity waves radiating from the typhoon. These waves, resembling ripples on a pond, were made visible to the sensor via airglow in the mesosphere. Airglow occurs when atoms and molecules, excited by sunlight during the day, later emit light to release excess energy.
The release of latent heat near the eyewalls of tropical cyclones is known to drive convection and the formation of tall cumulonimbus clouds. These “hot towers” can rise out of the troposphere, the lowest layer of the atmosphere, and generate waves that propagate into the stratosphere and mesosphere above. An analysis of past tropical cyclones revealed that gravity waves often occur around the time that storms are intensifying. Indeed, in the 24 hours prior to the acquisition of the image above, Sinlaku had strengthened from a category 2 to a category 5 storm.
“We’re seeing waves propagating radially and upward, in a cone-like shape,” said Joan Alexander, senior research scientist at NorthWest Research Associates. Alexander was surprised to see well-defined waves in the mesospheric airglow above the storm. Winds in the upper atmosphere can dissipate the waves before they reach such high altitudes, Alexander explained, but relatively light stratospheric winds at the storm’s latitude in April 2026 may have helped preserve them.
A relatively low amount of moonlight was fortuitous, as well. The VIIRS day-night band is sensitive to airglow in the mesosphere but also observes reflected moonlight. The Moon was about 25 percent illuminated on April 12, so some light reflected off clouds in the troposphere was visible, but not enough to overpower the signal from the airglow.
Thermal energy from gravity waves produced by Super Typhoon Sinlaku was detected in the stratosphere by the AIRS (Atmospheric Infrared Sounder) instrument on NASA’s Aqua satellite on April 13, 2026.
NASA Earth Observatory/Michala Garrison
Sinlaku’s gravity waves, in addition to appearing high in the atmosphere via airglow, were observed lower in the atmosphere by the AIRS (Atmospheric Infrared Sounder) instrument on NASA’s Aqua satellite. The image above depicts thermal emissions from gravity waves in the stratosphere on April 13. The rippling pattern appeared in April 14 observations, as well, indicating the storm’s continuing effects on the atmosphere.
Observing atmospheric gravity waves, particularly those caused by tropical cyclones, goes beyond scientific curiosity. Practical implications could include improved monitoring of storm development. “We’d like to use gravity waves to tell us if a storm is intensifying,” Alexander said, “which can be difficult to know, especially over the open ocean.” A geostationary satellite with the proper infrared imager would be able to observe gravity waves and track tropical cyclone evolution, she and colleagues have argued.
Furthermore, it’s critical to account for processes in the stratosphere in weather models, said Laura Holt, also a senior research scientist at NorthWest Research Associates. Stratospheric wind patterns are factors in long-term forecasts of the next Northern Hemisphere winter, for example, and tropical cyclones have a disproportionate influence because their sustained, intense convection drives prolonged gravity wave forcing of the stratosphere.
The effect of gravity waves even reaches into the realm of space weather. “For a while, people have seen signatures of hurricanes in ionospheric weather,” Holt said. Gravity waves can lead to traveling ionospheric disturbances—large-scale ripples in plasma density—and in some cases plasma bubbles, both of which can disrupt satellite signals and radio communications. “With space weather in particular,” Holt added, “a single event such as a tropical cyclone can be very important.”
NASA has selected seven companies to provide construction, revitalization, and infrastructure improvements at the agency’s Johnson Space Center in Houston.
The Johnson Space Center Multiple Award Construction Contract supports up to $300 million in upgrades to mission‑support facilities, utilities, and equipment across the NASA Johnson campus. All funds must be obligated by Sept. 30, 2026.
The indefinite-delivery/indefinite-quantity award enables rapid execution of facility projects essential to sustaining astronaut crew training, engineering development, and mission readiness. Task orders will be competed among awardees to ensure fair opportunity and best value to the government.
Contract awardees are:
Coho Construction Management, LLC
Conti Federal Services, LLC
Healtheon, Inc.
HITT Contracting, Inc.
Ross Group Construction Corporation, LLC
Energy EPC Solutions, LLC, doing business as S&B Services
Sauer Construction, LLC
For more information about NASA and its missions, visit:
NASA’s SpaceX Crew-11 astronauts gather together for a crew portrait wearing their Dragon pressure suits during a suit verification check inside the International Space Station’s Kibo laboratory module. Clockwise from bottom left are, NASA astronaut Mike Fincke, Roscosmos cosmonaut Oleg Platonov, NASA astronaut Zena Cardman, and JAXA (Japan Aerospace Exploration Agency) astronaut Kimiya Yui.
Credit: NASA
NASA will host a public event featuring three crew members from the agency’s SpaceX Crew-11 mission at 11 a.m. EDT Monday, June 1. The event, which takes place during the crew’s standard postflight visit, will be held in the Webb Auditorium at NASA Headquarters in the Mary W. Jackson building, 300 E. Street SW in Washington.
The crew members, including NASA astronauts Zena Cardman and Mike Fincke and JAXA (Japan Aerospace Exploration Agency) astronaut Kimiya Yui, will discuss their recent 167-day mission aboard the International Space Station, where they conducted a wide range of science experiments to benefit life on Earth and advance human space exploration as part of International Space Station Expedition 73/74.
The Crew-11 mission lifted off on Aug.1, 2025, from Launch Complex 39A at NASA’s Kennedy Space Center in Florida. The crew’s SpaceX Dragon spacecraft docked to the orbital outpost on Aug. 2.
During their mission, the three astronauts, along with crewmate Roscosmos cosmonaut Oleg Platonov, traveled nearly 71 million miles and completed more than 2,670 orbits around Earth. The Crew-11 mission was Fincke’s fourth spaceflight, Yui’s second, and the first for Cardman and Platonov. Fincke has logged 549 days in space, ranking him fourth among all NASA astronauts for cumulative days in space. The crew members returned to Earth on Jan. 15, splashing down off the coast of San Diego.
Along the way, Crew-11 logged hundreds of hours of research, maintenance, and technology demonstrations. The crew members also celebrated the 25th anniversary of continuous human presence aboard the orbiting laboratory on Nov. 2, 2025. Research conducted aboard the space station advances scientific knowledge and demonstrates new technologies that enable us to prepare for human exploration of the Moon and Mars.
Media interested in attending the event must RSVP by 8 a.m., June 1, by emailing the NASA Headquarters newsroom at hq-media@mail.nasa.gov. NASA’s media accreditation policy is online. Based on the crew’s schedule, NASA will not be able to accommodate interviews.
This opportunity also is part of NASA’s Frontiers Forum: Voices Shaping the Future of Space speaking series designed to convene bold thinkers and senior leaders at the forefront of exploration and innovation. The series will spotlight mission-critical priorities from advancing the Artemis campaign and strengthening commercial partnerships to shaping the future workforce and accelerating breakthrough technologies. The agency will share more details soon.
To learn more about the International Space Station and its research and crews, visit:
The 2026-2030 Landsat Science Team met for their first in-person meeting May 5-7, 2026 at the USGS EROS Center. Front Row: Raquel De Los Reyes, Courtney Bright, Forrest Melton, Michael Campbell , Hankui Zhang Standing: Greg Vaughan, Lin Yan, Mike Wulder, David Frantz, Kyle Knipper, Nimrod Carmon, Dean Hively, Yun Yang, Peter Strobl, David Roy, Morgan Crowley, Ned Bair, Phillip Dennison, Ryan O’Shea, Feng Gao, Medhavy Thankappan, Zhuosen Wang. Not pictured: Martha Anderson, Kimberlee Baldry, Eric Vermote.
USGS
From May 5 to 7, the 2026–2030 Landsat Science Team met for their first in-person meeting at the Earth Resources Observation and Science (EROS) Center in Sioux Falls, SD. The three-day event, co-moderated by Landsat 8, 9, and 10 Project Scientist Chris Neigh, allowed leaders from USGS and NASA to begin work on a vision for the upcoming five-year period.
Attendees shared their current work and a vision for the future of the Landsat program. Participants received comprehensive status updates on the upcoming Landsat 10 project, the ongoing interagency and international collaboration on the Harmonized Landsat and Sentinel-2 (HLS) data products, and detailed plans for Collection 3 (C3).
Throughout the event, team members representing funded, international, and federal programs showcased the far-reaching impact of Landsat data across various Earth science disciplines, spanning snow cover mapping, atmospheric correction, water quality monitoring, evapotranspiration, agricultural applications, volcanic monitoring, and more.
The meeting culminated in focused breakout sessions, where experts drafted vital recommendations across four key technical areas to guide future mission data processing:
Surface Reflectance
The surface reflectance working group identified several priorities, including topography and adjacency corrections, Bidirectional Reflectance Distribution Function (BRDF) correction, and enhanced cloud masking with consistent approaches for HLS data products. Key recommendations included incorporating CMIX2 cloud masking results into future collections and mapping out C3 toolkit dependencies for user-applied corrections.
Temperature and Emissivity
Discussions on land surface temperature and emissivity centered heavily on maintaining archive consistency. The team recommended either maintaining native resolution or standardizing to 60 meters, with additional testing specifically for volcano studies. They endorsed using ASTER GED/CAMEL emissivity datasets and preparing for Landsat 10’s five thermal bands through ECOSTRESS comparison. They also called for better quantification of how atmospheric inputs impact harmonization efforts through collaboration between NASA’s Jet Propulsion Laboratory (JPL), RIT, and EROS.
Aquatic Reflectance
Aquatic reflectance experts raised critical concerns regarding Landsat 10’s planned 18-day repeat cycle, noting that it severely limits the monitoring of highly dynamic processes such as harmful algal blooms. The group called for increased investment in validation infrastructure for inland waters coordinated with international CEOS efforts. They also strongly advised against pixelwise algorithm switching to prevent data discontinuities and emphasized the need for strict compliance with CEOS Aquatic Reflectance V2.0 standards.
Projections, Tiling, and the Pixel
Finally, the group reviewing projection and tiling endorsed the USGS pixel grid nesting plan (which spans 10, 15, 20, 30, 60, and 120 meters). However, they recommended further trade analysis to optimize pixel replication errors, manage storage costs, and ensure proper coordination with Sentinel-2 Next Generation. The working group strongly recommended that if these complex grid issues remain unresolved, the program should maintain the Collection 2 approach (UTM and polar stereographic) while continuing to refine Analysis Ready Data (ARD) products for CONUS, Hawaii, and Alaska.
The recommendations generated during these breakout sessions created a roadmap for the new Landsat Science Team, ensuring that the global scientific community continues to receive high-quality, actionable Earth observation data through the end of the decade.
Curiosity Blog, Sols 4900-4907: Pasadena, We Have a Drill Sample!
NASA’s Mars rover Curiosity acquired this image, the first color look of the “Campo Marte” drill hole, on May 16, 2026. The rover captured the image using its right Mast Camera (Mastcam) — one of a pair of cameras mounted on the head atop the rover’s mast — on Sol 4897, or Martian day 4,897 of the Mars Science Laboratory mission, at 18:05:49 UTC.
NASA/JPL-Caltech/MSSS
Written by Abigail Fraeman, Deputy Project Scientist at Jet Propulsion Laboratory, California Institute of Technology
Earth planning date: Friday, May 22, 2026
I spent this past weekend eagerly awaiting the downlink from Mars that would show us the results of Curiosity’s drill attempt at “Campo Marte.” A few weeks ago, when Curiosity drilled the “Atacama” block, it had been quite the surprise to see the post-drill images arrive on Earth that showed the rover picking up the entire Atacama block along with the drill. After freeing ourselves from this pesky passenger, the team carefully assessed all the telemetry and imaging data we had collected to understand why the entanglement happened and to mitigate the chance of it happening again. We concluded it would be ok to try another drill in this general area, and nearby Campo Marte looked like a great target because it had all the right geologic features and was significantly bigger than Atacama. What a delight it was to see images, like the Mastcam shown above, streaming down on Saturday that showed Curiosity had successfully retracted its drill from the rock and collected some sample to analyze this time around!
On Monday, the team looked at the pinches of drilled rock powder, or portions, that we had dropped as a test onto part of Curiosity, an element of our standard post-drilling activities. You can also take a look at what we saw — here’s a picture of the rover before we did anything, and here’s what we saw after we delivered the first portion, and then the second portion. Can you make out the little bit of powder that appears between the sample deliveries? This test is important to make sure we’ll provide good samples to the analytical instruments inside our chassis, CheMin and SAM. Beyond their science operations value, I also love seeing these images because they remind me how powerful our laboratory instruments are. With just a little pinch of powder, no more than tens of milligrams, these laboratories can reveal incredibly detailed information about the composition of Martian rocks and give us huge new insights into the planet’s past climate and habitability.
We concluded the portions from Campo Marte looked similar to the drilled samples we’ve previously analyzed, so we went ahead and delivered one portion to CheMin in Monday’s plan. We use the results from CheMin to tailor our analysis of the samples with SAM, so after we saw the first CheMin results in the middle of the week, we made decisions about how to run SAM and then planned to analyze four portions with that instrument in today’s plan. We think we’ll be nearly out of sample after that, but it’s hard to know for sure (we only drilled to a depth of 28 millimeters here, about 1.1 inches, rather than our usual 35 millimeters, or 1.38 inches). To learn more, in this upcoming weekend’s plan, we’ll also repeat the sample drop-off test we did right after drilling, which will show us how many portions were left. We do a ton of testing with Curiosity’s twin drill here on Earth, but it’s always insightful to see how our hardware performs on Mars under the unique geologic and environmental conditions of that entirely different world.
