NASA’s Hubble Reveals Largest Found Chaotic Birthplace of Planets

NASA’s Hubble Reveals Largest Found Chaotic Birthplace of Planets

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NASA’s Hubble Reveals Largest Found Chaotic Birthplace of Planets

Near the center is an object that resembles an edge-on view of a hamburger. There is a diagonal dark strip (the meat patty) of dust, running from 1 o'clock to 7 o'clock, that obscures a central star. Curving away from either side of the dark strip are glowing white clouds (the buns) where dust is reflecting starlight. Bright blue finger-like wisps of material extend far above and below the dark center plane. A few dozen stars, some with four diffraction spikes, are scattered on the black background of space.

Astronomers using NASA’s Hubble Space Telescope have imaged the largest protoplanetary disk ever observed circling a young star. For the first time in visible light, Hubble has revealed the disk is unexpectedly chaotic and turbulent, with wisps of material stretching much farther above and below the disk than astronomers have seen in any similar system. Strangely, more extended filaments are only visible on one side of the disk. The findings, which published Tuesday in The Astrophysical Journal, mark a new milestone for Hubble and shed light on how planets may form in extreme environments, as NASA’s missions lead humanity’s exploration of the universe and our place in it.

Located roughly 1,000 light-years from Earth, IRAS 23077+6707, nicknamed “Dracula’s Chivito,” spans nearly 400 billion miles — 40 times the diameter of our solar system to the outer edge of the Kuiper Belt of cometary bodies. The disk obscures the young star within it, which scientists believe may be either a hot, massive star, or a pair of stars. And the enormous disk is not only the largest known planet-forming disk; it’s also shaping up to be one of the most unusual.

“The level of detail we’re seeing is rare in protoplanetary disk imaging, and these new Hubble images show that planet nurseries can be much more active and chaotic than we expected,” said lead author Kristina Monsch of the Center for Astrophysics | Harvard & Smithsonian (CfA). “We’re seeing this disk nearly edge-on and its wispy upper layers and asymmetric features are especially striking. Both Hubble and NASA’s James Webb Space Telescope have glimpsed similar structures in other disks, but IRAS 23077+6707 provides us with an exceptional perspective — allowing us to trace its substructures in visible light at an unprecedented level of detail. This makes the system a unique, new laboratory for studying planet formation and the environments where it happens.”

The nickname “Dracula’s Chivito” playfully reflects the heritage of its researchers—one from Transylvania and another from Uruguay, where the national dish is a sandwich called a chivito. The edge-on disk resembles a hamburger, with a dark central lane flanked by glowing top and bottom layers of dust and gas.

Near the center is an object that resembles an edge-on view of a hamburger. There is a diagonal dark strip (the meat patty) of dust, running from 1 o'clock to 7 o'clock, that obscures a central star. Curving away from either side of the dark strip are glowing white clouds (the buns) where dust is reflecting starlight. Bright blue finger-like wisps of material extend far above and below the dark center plane. A few dozen stars, some with four diffraction spikes, are scattered on the black background of space.
This Hubble Space Telescope image shows the largest planet-forming disk ever observed around a young star. It spans nearly 400 billion miles — 40 times the diameter of our solar system.
Image: NASA, ESA, STScI, Kristina Monsch (CfA); Image Processing: Joseph DePasquale (STScI)

Puzzling asymmetry

The impressive height of these features wasn’t the only thing that captured the attention of scientists. The new images revealed that vertically imposing filament-like features appear on just one side of the disk, while the other side appears to have a sharp edge and no visible filaments. This peculiar, lopsided structure suggests that dynamic processes, like the recent infall of dust and gas, or interactions with its surroundings, are shaping the disk.

“We were stunned to see how asymmetric this disk is,” said co-investigator Joshua Bennett Lovell, also an astronomer at the CfA. “Hubble has given us a front row seat to the chaotic processes that are shaping disks as they build new planets — processes that we don’t yet fully understand but can now study in a whole new way.”

All planetary systems form from disks of gas and dust encircling young stars. Over time, the gas accretes onto the star, and planets emerge from the remaining material. IRAS 23077+6707 may represent a scaled-up version of our early solar system, with a disk mass estimated at 10 to 30 times that of Jupiter — ample material for forming multiple gas giants. This, plus the new findings, makes it an exceptional case for studying the birth of planetary systems.

“In theory, IRAS 23077+6707 could host a vast planetary system,” said Monsch. “While planet formation may differ in such massive environments, the underlying processes are likely similar. Right now, we have more questions than answers, but these new images are a starting point for understanding how planets form over time and in different environments.”

Credit: NASA’s Goddard Space Flight Center; Lead Producer: Paul Morris

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.

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Last Updated
Dec 23, 2025
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Andrea Gianopoulos
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Media

Claire Andreoli
NASA’s Goddard Space Flight Center
Greenbelt, Maryland
claire.andreoli@nasa.gov

Christine Pulliam
Space Telescope Science Institute
Baltimore, Maryland

Amy Oliver
Center for Astrophysics | Harvard & Smithsonian
Cambridge, Massachusetts

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I Am Artemis: Grace Lauderdale

I Am Artemis: Grace Lauderdale

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I Am Artemis: Grace Lauderdale

Grace Lauderdale, exploration project manager for the Training Systems Office at NASA’s Johnson Space Center in Houston, sits inside the Orion Mission Simulator used for training the Artemis II crew and flight control team.

Credits:
NASA/Rad Sinyak

Listen to this audio excerpt from Grace Lauderdale, exploration project manager for the Training Systems Office at NASA Johnson:

0:00 / 0:00

In preparation for their mission around the Moon inside NASA’s Orion spacecraft, the Artemis II crew will spend countless hours training inside the Orion Mission Simulator. The simulator replicates what the crew will experience inside the spacecraft and allows the astronauts and flight controllers to rehearse every phase of the mission.

As the exploration project manager for the Training Systems Office at Johnson, Grace Lauderdale leads the team that develops and operates the Orion Mission Simulator at NASA’s Johnson Space Center in Houston, playing a key role in making sure astronauts and flight control teams are ready for the first crewed mission of the Artemis campaign.

«This simulator trains the flight control team and the crew all the way from launch to splashdown. Every button, every display, every view out the window is as lifelike as possible.”

Grace Lauderdale

Grace Lauderdale

Exploration Project Manager for the Training Systems Office at NASA Johnson

The simulator is more than a mock-up. It connects directly to Johnson’s Mission Control Center, sending real-time data, audio, and video — just like the spacecraft will during flight. That means the flight control team trains in parallel, seeing and hearing exactly what they would throughout the mission.

“One of our major goals is to make the data they see on their displays look like the real vehicle,” Lauderdale said. “We also simulate the near space and deep space networks, including all the communication delays. It’s all about realism.”

That realism is powered by a complex software system developed in collaboration with partners like Lockheed Martin. Lauderdale’s team works behind the scenes to ensure the simulator runs smoothly — writing code, troubleshooting issues, and even creating custom malfunctions to challenge the crew during training.

Grace Lauderdale, exploration project manager for the Training Systems Office at NASA’s Johnson Space Center in Houston, sits inside the Orion Mission Simulator used for training the Artemis II crew and flight control team.
Credits: NASA/Rad Sinyak

To prepare astronauts for the unexpected, instructors work with Lauderdale’s team to simulate problems that could occur during the mission, some of which require creative solutions.

“There are times when the instructors will ask for malfunctions or capabilities that the sim doesn’t automatically do,” she said. “Part of our role is to come up with ways to make that happen.”

Her team plans, develops, and executes training scenarios in the Orion Mission Simulator across multiple Artemis missions, often simultaneously. “Currently, we’re planning for future crewed missions, developing Artemis III, and executing Artemis II,” she said.

The work is demanding, but deeply personal, according to Lauderdale.

“I’ve known I wanted to work at NASA since the seventh grade. Every class I took, the degree I earned — it was all to get here.”

Grace Lauderdale

Grace Lauderdale

Exploration Project Manager for the Training Systems Office at NASA Johnson

That passion shows in her leadership. Her team often works nights, weekends, and holidays to ensure the simulator is ready. During a recent 30-hour simulation, they spent days preparing, fixing memory issues, and ensuring the system wouldn’t crash. It didn’t.

“I’m very proud of my team,” she said. “They’ve put in countless hours of work to make sure this simulator reacts exactly as it would in the real mission.”

For Lauderdale, helping send astronauts around the Moon isn’t just a job—it’s a dream realized.

“Being part of getting us back to the Moon is very personal to me,” she said. “And I’m proud to be part of the team that will help get our astronauts there.”

Reid Wiseman and Victor Glover train for the Artemis II mission inside the Orion Mission Simulator at NASA’s Johnson Space Center in Houston.
NASA/Bill Stafford

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Erika Peters

Erika Peters

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Dec 22, 2025

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Curiosity Blog, Sols 4750-4762: See You on the Other Side of the Sun

Curiosity Blog, Sols 4750-4762: See You on the Other Side of the Sun

3 min read

Curiosity Blog, Sols 4750-4762: See You on the Other Side of the Sun

A grayscale photo of Martian landscape shows a wide expanse in the foreground, with dark gray, uneven terrain that slopes slightly from the middle right of the frame down toward the lower left corner. Beyond that in the far distance is a horizon line that follows the same descent; it’s hazy, pale gray, and looks like a long edge with walls sloping downward. The empty sky above appears as a whitish pale gray.
NASA’s Mars rover Curiosity acquired this image, with the boxwork terrain in the foreground and Gale crater rim in the far background, using its Right Navigation Camera. Curiosity captured the image on Dec. 21, 2025 — Sol 4755, or Martian day 4,755 of the Mars Science Laboratory mission — at 15:57:21 UTC.
NASA/JPL-Caltech

Written by Lucy Thompson, Planetary Scientist and APXS team member, University of New Brunswick, Canada

Earth planning date: Monday, Dec. 22, 2025

As we all prepare for the holiday season here on Earth, we have been planning a few last activities before Curiosity and the team of scientists and engineers take a well-deserved, extended break. This holiday season coincides with conjunction — every two years, because of their different orbits, Earth and Mars are obstructed from one another by the Sun; this one will last from Dec. 27 to Jan. 20. We do not like to send commands through the Sun in case they get scrambled, so we have been finishing up a few last scientific observations before preparing Curiosity for its quiet conjunction break.

As part of a pre-planned transect between our two recent drill holes, “Valle de la Luna” (hollow) and “Nevado Sajama” (ridge), we successfully completed chemical analyses and imaging of a ridge wall. These observations were acquired to document changes in texture, structure, and composition between the two drill holes and to elucidate why we see such contrasting physical features of resistant ridges and eroded hollows in this region. Mastcam and ChemCam also imaged a little further afield. ChemCam continued observations of the “Mishe Mokwa” butte and captured textures in the north facing wall of the next, adjacent hollow. Mastcam imaged the central fracture along the “Altiplano” ridge above the wall we were parked at, as well as polygonal features in our previous workspace.

The rover engineers then successfully orchestrated Curiosity’s drive back up onto the nearby ridge to ensure a safe parking spot over conjunction. We documented the drive with a MARDI sidewalk video, tracking how the terrain beneath the rover changes as we drive. Although we could not use APXS and MAHLI on the robotic arm from Friday on, owing to constraints that need to be in place prior to conjunction, we were able to use the rover’s Mastcam to image areas of interest in the near field, which will help us with our planned activities when we return from conjunction. These will hopefully include getting chemistry (with APXS and ChemCam) and imaging (with MAHLI) of some freshly broken rock surfaces that we drove over.

The environmental scientists were also very busy. Navcam observations included: Navcam suprahorizon and zenith movies to monitor clouds; Navcam line-of-sight observations; and Navcam dust-devil movies and surveys as we enter the dust storm season on Mars. Mastcam tau observations were acquired to monitor the optical depth of the atmosphere, and APXS analyses of the atmosphere were also planned to monitor seasonal variations in argon.

Today we are uplinking the last plan before Mars disappears behind the Sun and we all take a break (the actual conjunction plan to take us through sols 4763-4787 was uplinked a couple of weeks ago). Because of constraints put in place to make sure Curiosity stays safe and healthy, we were limited to very few activities in today’s plan. These include more APXS atmospheric argon measurements and Hazcam and Navcam imaging including monitoring for dust-devil activity.

As usual, our plans also included background DAN, RAD, and REMS observations, which continue through conjunction.

It has been a pleasure to be a part of this amazing team for another year. We are all looking forward to coming back in January, when Mars reappears from behind the Sun, to another exciting year of roving in Gale crater.

A rover sits on the hilly, orange Martian surface beneath a flat grey sky, surrounded by chunks of rock.
NASA’s Mars rover Curiosity at the base of Mount Sharp
NASA/JPL-Caltech/MSSS

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Dec 22, 2025

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Holidays in Space: 25 Years of Space Station Celebrations

Holidays in Space: 25 Years of Space Station Celebrations

In the quarter century that humans have lived and worked aboard the International Space Station, astronauts and visitors from around the world have celebrated countless holidays more than 250 miles above Earth while traveling 17,500 miles per hour. Crews have marked Thanksgiving, Christmas and Hanukkah, New Year’s, birthdays, and national holidays as they circle the planet every 90 minutes.  

Holiday traditions in space often look familiar, just adapted for microgravity. NASA astronauts share special meals packed by the Space Food Systems Laboratory at the agency’s Johnson Space Center in Houston, where crews select their menus with help from nutritionists and food scientists before launch. Cargo launches arriving before special occasions often deliver Holiday Bulk Overwrapped Bags filled with foods like clams, oysters, turkey, green beans, and smoked salmon, along with shelf-stable treats such as candies, icing, almond butter, and hummus. 

Crew members exchange small gifts that float through the modules, add festive decorations around the station, and connect with loved ones through video calls. Astronauts also send holiday greetings to Earth, a reminder that even in space, home is never far away. 

The Expedition 73 crew share a holiday message aboard the International Space Station in Dec. 2025.

Enjoy 25 years of celebrations below. 

The space station remains a vital scientific platform, providing the foundation needed to survive and thrive as humanity ventures into the unexplored territories of our universe.

Learn more about the space station’s 25 years of continuous human presence and explore stories, images, and research at:

https://www.nasa.gov/international-space-station/iss25

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Sumer Loggins

Keeping Up with PACE: Summary of the 2025 PAC3 Meeting

Keeping Up with PACE: Summary of the 2025 PAC3 Meeting

12 min read

Keeping Up with PACE: Summary of the 2025 PAC3 Meeting

Introduction

Launched in Feb. 2024, NASA’s Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) mission is a cornerstone of Earth system science designed to deepen our understanding of how these environmental and biological components come together to influence our climate, carbon cycle, and ecosystems. PACE has funded three supporting components: the PACE Postlaunch Airborne eXperiment (PACE–PAX), the third PACE Science and Applications Team (SAT3), and the PACE Validation Science Team (PVST). Each group serves distinct but interdependent roles in advancing the scientific objectives of the mission through product development and rigorous assessment of data quality.

Recognizing the interconnected focus areas among these groups, the organizers consolidated this year’s separate gatherings into one comprehensive event – the “PAC3” meeting. The combined meeting took place from Feb. 18–21, 2025 at NASA’s Goddard Institute for Space Studies (GISS) in New York City, just 10 days after the first anniversary of the PACE launch – see Photo 1 and Photo 2.

PACE photo 1
Photo 1. Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) scientists celebrated the one-year anniversary of the satellite’s orbit (February 8, 2025) during the PAC3 meeting. A “birthday” celebration took place during the meeting, complete with cake. Shown here are [left to right]: Ivona Cetinić [NASA’s Goddard Space Flight Center (GSFC)/Morgan State University, Ocean Ecology Laboratory (OEL)—PACE Validation Science Team lead, PACE-PAX Deputy Mission Scientist], Erin Urquhart Jephson [NASA Headquarters (HQ)—Program Manager of the NASA Earth Action Water Resources Program, PACE Program Applications Lead], Cecile Rousseaux [GSFC, OEL—PACE Science and Applications Team Lead], Kirk Knobelspiesse [GSFC, OEL—PACE Polarimeter Lead, PACE-PAX Mission Scientist], Jeremy Werdell [GSFC, OEL—PACE Project Scientist], Laura Lorenzoni [NASA HQ—Ocean Biology and Biogeochemistry Program Scientist, PACE Program Scientist], Brian Cairns [NASA Goddard Institute for Space Studies (GISS)—PACE Deputy Project Scientist, PACE-PAX Deputy Mission Scientist], and Bryan Franz [GSFC, OEL—PACE Science Data Segment Lead].
Photo credit: Judy Alfter [NASA Ames Research Center (ARC)/Bay Area Environmental Research Institute (BAER)]
PACE photo 2
Photo 2. With over 100 in-person and virtual attendees, the PAC3 meeting brought together representatives from each of the three overlapping activities for discussions on the status and plans for Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) and related activities. The recently renovated meeting space at the NASA Goddard Institute for Space Studies (GISS) in New York City provided an ideal venue for interdisciplinary discussions and knowledge-sharing.
Photo credit: Sabrina Hosein [NASA GISS/Adnet Systems]

The PACE Mission and Payload

PACE’s long-term objectives focus on understanding ocean and terrestrial ecosystem productivity, detecting harmful algal blooms, exploring relationships between aerosols and clouds, and integrating these insights into Earth system science to enhance both research and decision-making capacities. These goals are accomplished by the advanced suite of three complementary instruments.

The Ocean Color Instrument (OCI) is a hyperspectral radiometer that measures ocean ecosystems’ biological, biogeochemical, and physical dynamics by capturing light over hundreds of narrow wavelengths from the deep ultraviolet to the infrared. Additionally, the broad spectral range and spectral resolution of the measurements allow the research community to characterize aerosols, clouds, land surfaces, and trace gases.

The Hyper-Angular Rainbow Polarimeter #2 (HARP2) is a multiangle polarimeter with a wide swath, four visible–near infrared (VIS–NIR) spectral channels, and between 10 and 60 viewing angles (i.e., the hyperangular capability) in each spectral channel. HARP2 is designed for retrieval of cloud and aerosol properties.

The Spectropolarimeter for Planetary Exploration (SPEXone) is also a multiangle polarimeter with different and complementary properties to HARP2. SPEXone has a narrow swath and five viewing angles with a spectral sensitivity of 100 bands from the ultraviolet to the near infrared. It is optimized for the retrieval of aerosol properties.

More details about the PACE mission can be found at its website.

PACE Mission Updates

The PAC3 meeting included a review of the PACE mission’s status and recent developments. This overview included meeting status updates on OCI, SPEXone, and HARP2 from their respective instrument scientists: Gerhard Meister [NASA’s Goddard Space Flight Center (GSFC)], Otto Hasekamp [Space Research Organization, Netherlands (SRON)], and Vanderlei Martins [University of Maryland, Baltimore County (UMBC)]. This section of the meeting covered updates on the early mission data availability and accessibility, including a review of the PACE data website. These details are summarized on the PACE data availability website and the ‘help hub’.

OCI

Meister reported that OCI has exceeded radiometric performance requirements, delivering highly accurate hyperspectral data. He noted that, with the release of Version 3 (V3) data reprocessing, OCI calibration now uses only on-orbit solar diffuser measurements to improve temporal stability. Key improvements of V3 include enhanced corrections for atmospheric absorbing gas effects and updated bidirectional reflectance distribution function (BRDF) parameters. Meister said that analysis of temporal trends has revealed solar diffuser degradation in the ultraviolet range, with ongoing corrections being made. For example, he cited how the team is using the solar diffuser that is only exposed once a month to correct the observations of the solar diffuser that is exposed daily. He also discussed other anomalies, including striping around 10° scan angle, reduced accuracy in the 590–610 nm region and implementation of crosstalk correction to compensate for reduced accuracy of wavelength measurements in the ultraviolet (i.e., for wavelengths shorter than 340 nm).

SPEXone

Hasekamp reported that SPEXone is delivering quality radiometric and polarimetric data. The team has developed the Remote Sensing of Trace Gases and Aerosol Products (RemoTAP) algorithm, an advanced aerosol retrieval algorithm that determines the total atmospheric column of aerosols, aerosol size distribution information, energy absorbed by aerosols, and vertical extent of the aerosol layer. Hasekamp showed that observations demonstrate minimal bias in size distribution retrievals across low aerosol optical depth (AOD) environments and these observations have good agreement with observations from ground-based Sun photometers that are part of the Aerosol Robotic Network (AERONET). He added that future updates will address radiometric calibration discrepancies with OCI.

HARP2

Martins reported that HARP2 continues to perform well and is delivering polarization-sensitive observations of aerosols and clouds. He noted that plans include making continued geolocation and calibration refinements, as well as cross-calibration with OCI and SPEXone to harmonize all the PACE radiometric data products.

PACE Data Access and Website Resources

Several presentations outlined the tools and platforms available to make data from the PACE mission accessible to the broader scientific community.

Alicia Scott [GSFC/Science Applications International Corporation (SAIC)] described capabilities provided by the Ocean Biology Distributed Active Archive Center (OB.DAAC). The OB.DAAC stores and processes data from all PACE instruments using tools, such as Earthdata Search and earthaccess Python libraries that enable user-friendly data retrieval pipelines. Training resources and tutorials are available to streamline usage.

Carina Poulin [GSFC/Science Systems and Applications, Inc (SSAI)] provided an overview of the PACE Data Website, which serves as a central hub for accessing datasets, reprocessing information, and product tutorials. The V3 landing page provides details on calibration updates, validation results, and pathways for integrating PACE data into user workflows.

EarthCARE Mission Updates

Many of PACE’s science objectives dovetail with that of the Earth Clouds, Aerosols, and Radiation Explorer (EarthCARE), a joint venture by the European Space Agency (ESA) and Japan Aerospace Exploration Agency (JAXA). Hence, the PAC3 meeting included participation from the EarthCARE teams. The EarthCARE observatory has four advanced instruments: a high spectral resolution ATmospheric LIDar (ATLID), a doppler capable Cloud Profiling Radar (CPR), a Multi-Spectral Imager (MSI), and a Broad-Band Radiometer (BBR). The measurements from EarthCARE complement those of PACE and enable cross validation, enriching scientific knowledge of complex Earth system processes. The synergistic nature of these missions also means that validation activities for one are well suited to both. For example, the Plankton, Aerosol, Cloud, ocean Ecosystem Postlaunch Airborne eXperiment (PACE-PAX) field campaign (discussed later in this article) incorporated validation activities for EarthCARE, and EarthCARE funded campaigns have made observations during PACE overpasses.

Rob Koopman [ESA] outlined progress on EarthCARE, including preparation for validation activities as part of ESA and JAXA’s joint efforts. He reported that the mission’s ATLID lidar data products are in excellent alignment with airborne High Spectral Resolution Lidar (HSRL) datasets (flown during PACE-PAX). Koopman showed preliminary results from underflights with NASA aircraft that demonstrate high accuracy for cloud and aerosol retrieval, albeit with some calibration challenges that will require further refinement. He also said that several EarthCARE–PACE mutual validation campaigns are planned to ensure inter-mission consistency across critical science products.

PACE–PAX Sessions

The first component of the PAC3 meeting focused on PACE–PAX, a field campaign conducted in California and adjacent coastal regions during Sept. 2024 – see Figure 1. Kirk Knobelspiesse [GSFC, OEL—PACE Polarimeter Lead, PACE-PAX Mission Scientist], Ivona Cetinić [NASA’s Goddard Space Flight Center (GSFC)/Morgan State University, Ocean Ecology Laboratory (OEL)—PACE Validation Science Team lead, PACE-PAX Deputy Mission Scientist], and Brian Cairns [NASA Goddard Institute for Space Studies (GISS)—PACE Deputy Project Scientist, PACE-PAX Deputy Mission Scientist] led the campaign, which, in addition to personnel from most NASA Centers, had participation from academia (e.g., University of Maryland, Baltimore County), other government agencies (e.g., Naval Postgraduate School and National Oceanic and Atmospheric Administration), and international space agencies (e.g., Space Research Organization, Netherlands).

PACE photo 3
Figure 1. Montage of activities during the Plankton, Aerosol, Cloud, ocean Ecosystem Postlaunch Airborne eXperiment (PACE–PAX) field campaign, which successfully concluded on Sept. 30, 2024. The campaign made atmospheric, ocean, and land surface measurements to validate observations from the recently launched NASA PACE and European Space Agency (ESA) and Japan Aerospace Exploration Agency (JAXA) Earth Clouds, Aerosols, and Radiation Explorer (EarthCARE) missions. Clockwise from top left: Mike Ondrusek [NOAA R/V Shearwater Mission Scientist] waves to the Naval Postgraduate School (NPS) Twin Otter as it performs a low altitude sample. Photo of the Bridge fire from Kirt Stallings [NASA ARC Earth Resources-2 (ER-2) Pilot]. Carl Goodwin [NASA/Jet Propulsion Laboratory] performs calibration at Ivanpah Playa, CA, the primary reference site for space-based remote sensing observations located in the Mojave Desert. Scott Freeman and Harrison Smith [both GSFC] deploy instrumentation from the R/V Shearwater in the Santa Barbara Channel. Instrument integration on the NASA ER-2 in preparation for PACE-PAX. San Francisco observed by the NPS Twin Otter as it samples at low altitude over the San Francisco Bay. The R/V Shearwater seen from the NPS Twin Otter. 
Figure credit(s): Clockwise from top left: NASA; Kirt Stallings; Regina Eckert [NASA/Jet Propulsion Laboratory]; Luke Dutton [National Oceanic and Atmospheric Administration]; Martijn Smit [Space Research Organization, Netherlands]; Luke Ziemba [NASA’s Langley Research Center (LaRC)]; Luke Ziemba.

Campaign Overview

The PACE–PAX mission supported the PACE Science Data Product Validation Plan. This included validation of new PACE and EarthCARE products, data collection during instrument overpasses, verification of radiometric and polarimetric measurements, and targeted investigation of region-specific phenomena (e.g., multilayer aerosols and phytoplankton blooms).

Operational Highlights

PACE–PAX used a diverse array of platforms to collect atmospheric and oceanic data, including aircraft [e.g., NASA Earth Resources-2 (ER-2) and the Naval Postgraduate School’s Center for Interdisciplinary Remotely Piloted Aircraft Studies (CIRPAS) Twin Otter], research vessels (NOAA’s R/V Shearwater and the 30-foot sailboat R/V Blissfully), and ground-based instruments such as Sun photometers and lidars. Key achievements include 13 ER-2 and 17 Twin Otter science flights, 15 RV Shearwater and 9 R/V Blissfully day cruises. These flights and ocean surveys supported 16 days of observations during a PACE overpass, six days of observations during an EarthCARE overpass, ground vicarious calibration at Ivanpah Playa, CA, numerous overflights of AERONET ground sites. Beyond validation, several unique events were observed that may be of interest for scientific purposes. Intense wildfires (e.g., the Bridge, Airport, and Line fires in 2024) were observed in Southern California in mid-September, while a red tide outbreak was observed later in the month along the Northern California coast – see Figure 2. Additionally, elements of the PVST coordinated their own validation efforts with the PACE–PAX campaign.

PACE photo 4
Figure 2. Red tide blooms in Northern California as seen from three remote sensing tools on the Plankton, Aerosol, Cloud, ocean Ecosystem Postlaunch Airborne eXperiment (PACE–PAX). [Left] An image taken from the NPS Twin Otter on Sept. 24, 2024. [Right] The PACE Ocean Color Instrument (OCI) image collected on Sept. 27, 2024 with modified red-tide index applied to OCI data. [Center Inset] An Imaging FlowCytobot (IFCB) image taken on Sept. 27, 2024 at the Santa Cruz, CA pier.
Figure Credits: [Left] Eddie Winstead [NASA’s Langley Research Center (LaRC)]; [right] NASA; [inset] Clarissa Anderson [University of California, San Diego]

Preliminary Findings

Highlights of the PACE-PAX sessions demonstrated:

  • validation of EarthCARE and PACE aerosol and cloud products using the HSRL2 on NASA ER-2,
  • validation of PACE cloud products using polarimeters operating on the NASA ER-2 and in situ sensors on the CIRPAS Twin Otter,
  • numerous successful matchups of hyperspectral data from OCI on PACE with field measurements of chlorophyll-a captured during ship campaigns, and
  • observations of diverse phenomena (e.g., marine stratocumulus clouds and transported wildfire aerosols over clouds), which supported the testing of new retrieval algorithms.

The early results show the critical role that validation activities, such as PACE–PAX, play in creating a bridge between orbital science and ground truth.

PACE Science and Application Team (SAT3) Session

SAT3, with a focus on both science and applications, offered a compelling second component of the PAC3 meeting. The Earth Observer has previously reported on PACE applications, most recently in the 2023 article, Preparing for Launch and Assessing User Readiness: The 2023 PACE Applications Workshop [Nov–Dec 2023, 35:6, 25–32]. The SAT3 team convened during PAC3 to explore how PACE data could enhance research in diverse scientific fields and support applied uses for societal benefit. Dedicated sessions provided updates on ongoing NASA-funded projects to retrieve new geophysical variables, improve data assimilation, and refine product development pipelines.

SAT3 teams presented early results including studies that use PACE’s OCI to make pigment-specific absorption measurements, study diatom biomass retrieval, and gather chlorophyll concentration estimation. These studies emphasized new tools for tracking individual phytoplankton groups, such as diatoms and cyanobacteria that are vital for ecosystem research and understanding phytoplankton dynamics. Participants also showcased efforts to develop predictive models for the detection of harmful algal blooms (HABs) and improvement of early warning systems to mitigate public health impacts and economic consequences in both coastal regions and the Great Lakes. Several presentations highlighted new aerosol absorption and scattering measurements that are using polarimetry (i.e., SPEXone and HARP2) and how these findings are being incorporated into models of aerosol–cloud radiative forcing. Presenters also described how machine learning tools can integrate PACE measurements into Earth system models, through innovations in data assimilation, with promising results for global climate monitoring.

The SAT3 discussions highlighted PACE’s potential to impact disciplines ranging from oceanography to climate science.

PACE Validation Science Team Sessions

Sessions dedicated to the PACE PVST emphasized the ongoing role of PVST initiatives in confirming the reliability, accuracy, and long-term stability of PACE data products. Topics of focus for the PVST group included algorithm development and validation, cross-mission synergies, field-based campaign integration, and cloud products.

Some of the presenters shared updates on validation pipelines for radiometric and polarimetric products, with an emphasis on comparing against well-characterized datasets from AERONET Sun photometers, HSRL, and the Pan-and-Tilt Hyperspectral Radiometer (PANTHR) developed by Vlaams Instituut voor de Zee (VLIZ), or the Flanders Marine Institute, Belgium – see Photo 3. This radiometer was installed on a 30-m (~98-ft) tower in the Chesapeake Bay in May 2024 and is part of WATERHYPERNET network, which seeks to provide time series of hyperspectral water reflectance data from oceanic, coastal, and inland waters for the validation of satellite data at all wavelengths in the range 400–900 nm.

PACE photo 5
Photo 3. Inia Soto Ramos [Goddard Space Flight Center/Morgan State University] leads a Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) Validation Science Team (PVST) breakout group discussion.
Photo credit: Judy Alfter [NASA Ames Research Center (ARC)/ Bay Area Environmental Research Institute (BAER)]

Reports from PVST members highlighted how data from PACE–PAX campaigns and satellite overpasses are contributing to the validation of error budgets developed prelaunch and refined uncertainty characterization. Other presentations highlighted the development of validation strategies for PACE-derived cloud properties, including cloud optical thickness, top height, and droplet size distributions with significant contributions from EarthCARE observations. Ocean observation validation was represented as well, with presentations from many groups that are focusing on retrieval of not only oceanic optical properties but biological components. This data offers crucial validation for the advanced phytoplankton composition and general ocean productivity products from PACE.

The PVST’s work continues to provide the foundation for confidence in PACE data products. Their accuracy ensures broad usability of those products across global science applications.

Conclusion

The PAC3 meeting, held at NASA’s GISS, highlighted the collective efforts of the PACE mission’s diverse teams to address a broad range of Earth system science challenges. By combining the meetings for PACE–PAX, SAT3, and PVST, participants were able to strengthen collaborations, align ongoing efforts, and lay the groundwork for future research and validation activities.

Roundtable discussions and team updates also revealed the critical role of PACE in addressing long-standing Earth system science questions, such as understanding the influence of aerosols on cloud formation and characterizing the impacts of oceanic changes on global biogeochemical cycles at a global scale. The meeting concluded with participants compiling action items for further exploration. Topics identified for future efforts included strategies for ensuring long-term data calibration, improving data delivery pipelines, and refining algorithm development processes.

This meeting was one of the last significant events hosted at GISS before the facility’s closure at the end of May 2025. The findings and outcomes from PAC3 continue to inform and inspire PACE mission science, further enhancing its importance in advancing our understanding of the Earth system.

Kirk Knobelspiesse
NASA’s Goddard Space Flight Center
kirk.d.knobelspiesse@nasa.gov 

Cecile S. Rousseaux
NASA’s Goddard Space Flight Center
cecile.s.rousseaux@nasa.gov

Ivona Cetinić
NASA’s Goddard Space Flight Center/Morgan State University
ivona.cetinic@nasa.gov

Andrew Sayer
NASA’s Goddard Space Flight Center
andrew.sayer@nasa.gov

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Last Updated
Dec 22, 2025

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