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Dr. Steven “Steve” Platnick stepped down from his role at NASA on August 8, 2025, after more than three decades of public service. Steve began his career at NASA as a physical scientist at Goddard Space Flight Center in 2002. He moved to the Earth Science Division in 2009, where he has served in various senior management roles, including as the Earth Observing System (EOS) Senior Project Scientist. In this role, he led the EOS Project Science Office and continued periodic meetings of the EOS Project Scientists, initiated by Michael King during his tenure. Steve expanded these meetings to include representatives of non-EOS Earth observing missions and representatives from Earth Science Mission Operations (ESMO). In addition, Steve was named Deputy Director for Atmospheres in the Earth Science Division in January 2015 and served in this position until July 2024.
Dr. Steve Platnick Image credit: NASA During his time at NASA, Steve played an integral role in the development, sustainability, and advancement of NASA’s Earth Observing System platforms. From January 2003 – February 2010, Steve served as Deputy Project Scientist for Aqua. In this role, he applied his expertise in theoretical and experimental studies of satellite, aircraft, and ground-based cloud remote sensing to improve algorithms to benefit the data gathered from remote observing systems.
Taking the Lead to Improve Algorithms
Steve was actively involved in the Moderate Resolution Imaging Spectroradiometer (MODIS) Science Team, serving as the MODIS Atmosphere Team Lead. Steve helped advance several key components of the MODIS instrument, which flies on NASA’s Terra and Aqua platforms. He led a team that enhanced, maintained, and evaluated MODIS algorithms that support the Level-2 (L2) Cloud Optical/Microphysical Properties components (e.g., COD06 and MYD06) for MODIS on Terra and Aqua. The algorithms were designed to retrieve thermodynamic phase, optical thickness, effective particle radius, and water path for liquid and ice clouds. The team’s work also contributes to L3 products that address cloud mask, aerosols, clouds, and clear sky radiance for data within 1° grids over one-day, eight-day, and one-month repeat cycles. Under Steve’s leadership, the team also developed L2 products (e.g., MODATML2 and MYDATML2) that include essential atmosphere datasets of samples collected at 5–10 km (3–6 mi) that is consistent with L3 products to ease storage requirements of core atmospheric data.
Steve is also a member of the Suomi-National Polar-orbiting Partnership (Suomi NPP) Atmosphere Team, working on operational cloud optical and microphysical products. In this role, he contributed to algorithm development and refinement for the Cloud Product. In particular, he helped address a critical gap in the Visible Infrared Imaging Radiometer Suite (VIIRS) spectral channel, which was not designed to collect information for carbon dioxide (CO2) slicing and water vapor data in the same way as MODIS. Steve and his colleagues developed a suite of L2 algorithms for the spectral channels that were common to both MODIS and VIIRS to address cloud mask and cloud optical/microphysical properties. Through these efforts, the project has established a continuous cloud data record gathered from both instruments from 2017 to the present.
Steve also participated in numerous other working groups during the past 30 years. He participated in the Global Energy and Water Exchanges (GEWEX) Cloud Assessment Working Group (2008–present), Arctic Radiation-Cloud-Aerosol-Surface Interaction Experiment (ARCSIX) Science Team (2023–present), ObseRvations of Aerosols above CLouds and their intEractionS (ORACLES) Earth–Venture Suborbital (EVS)-2 Science Team (2014–2023), Deep Space Climate Observatory (DSCOVR) Science Team (2014–present), Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) Science Team (2014–2023), PACE Science Definition Team, Deputy Chair (2011–2012), Glory Science Team (2010–2014) NASA Observations for Modeling Intercomparison Studies (obs4MIPs) Working Group (2011), Advanced Composition Explorer (ACE) Science Definition Team (2009–2011), and Geostationary Operational Environmental Satellites (GOES) R-series Advanced Baseline Imager (ABI) Cloud Team (2005–2009).
Steve has also participated in numerous major airborne field campaigns in various roles, including: GSFC Lidar Observation and Validation Experiment (GLOVE, 2025), PACE Postlaunch Airborne eXperiment (PAX, 2024), the Westcoast & Heartland Hyperspectral Microwave Sensor Intensive Experiment (WH2yMSIE, 2024), ORACLES Science Team (2015–2019), Studies of Emissions and Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys (SEAC4RS) Science Team (2011–2015), Tropical Composition, Cloud and Climate Coupling (TC4) Management Team (2007), Cirrus Regional Study of Tropical Anvils and Cirrus Layers – Florida Area Cirrus Experiment (CRYSTAL-FACE) Science Management Team (2002), Southern Africa Fire-Atmosphere Research Initiative (SAFARI, 2000), First ISCCP Regional Experiment (FIRE) Arctic Cloud Experiment (ACE) (1998), Mikulski Archive for Space Telescopes (MAST, 1994), and ACE (1992).
Supporting Earth Science Communications
Through his senior leadership roles within ESD Steve has been supportive of the activities of NASA’s Science Support Office (SSO). He has participated in many NASA Science exhibits at both national and international scientific conferences, including serving as a Hyperwall presenter numerous times. He has met with task leaders frequently and has advocated on behalf of the SSO to management at NASA Headquarters, GSFC, and Global Sciences & Technology Inc.
For The Earth Observer newsletter publication team in particular, Steve replaced Michael King as Acting EOS Senior Project Scientist in June 2008, taking over the authorship of “The Editor’s Corner” beginning with the May–June 2008 issue [Volume 20, Issue 3]. The Acting label was removed beginning with the January–February 2010 issue [Volume 22, Issue 1]. Steve has been a champion of continuing to retain a historical record of NASA meetings to maintain a chronology of advances made by different groups within the NASA Earth Science community. He was supportive of the Executive Editor’s efforts to create a series called “Perspectives on EOS,” which ran from 2008–2011 and told the stories of the early years of the EOS Program from the point of view of those who lived them. He also supported the development of articles to commemorate the 25th and 30th anniversary of The Earth Observer. Later, Steve helped guide the transition of the newsletterfrom a print publication – the November–December 2022 issue was the last printed issue – to fully online by July 2024, a few months after the publication’s 35th anniversary. The Earth Observer team will miss Steve’s keen insight, historical perspective, and encouragement that he has shown through his leadership for the past 85 issues of print and online publications.
A Career Recognized through Awards and Honors
Throughout his career, Steve has amassed numerous honors, including the Robert H. Goddard Award for Science: MODIS/VIIRS Cloud Products Science Team (2024) and the William Nordberg Memorial Award for Earth Science in 2023. He received the Verner E. Suomi Award from the American Meteorological Society (AMS) in 2016 and was named an AMS Fellow that same year.
Steve has received numerous NASA Group Achievement Awards, including for the Cloud, Aerosol and Monsoon Processes Philippines Experiment (CAMP2Ex) Field Campaign Team (2020), Fire Influence of Regional to Global Environments and Air Quality (FIREX-AQ) Field Campaign Team (2020), ORACLES Field Campaign Team (2019), obs4MIPs Working Group (2015), SEAC4RS Field Campaign Team (2015), Advanced Microwave Scanning Radiometer for EOS (AMSR-E) Instrument Recovery Team (2013), Climate Absolute Radiance and Refractivity Observatory (CLARREO) Mission Concept Team (2012), Earth Science Constellation Red Team (2011), Science Mission Directorate ARRA Team (2011), TC4 Team (2009), MODIS Science Data Support Team (2007), Aqua Mission Team (2003), CRYSTAL-FACE Science Team (2003), and SAFARI 2000 International Leadership Team (2002).
Steve received two NASA Agency Honor Awards – the Exceptional Service Medal in 2015 and the Exceptional Achievement Medal in 2008. He was also part of the NASA Agency Team Excellence Award in 2017 for his work with the Satellite Needs Assessment Team. The Laboratory for Atmospheres honored him with the Best Senior Author Publication Award in 2001 and the Scientific Research Peer Award in 2005.
Steve received his bachelor’s degree and master’s degree in electrical engineering from Duke University and the University of California, Berkeley, respectively. He earned a Ph.D. in atmospheric sciences from the University of Arizona. He began his career at the Joint Center for Earth Systems Technology (JCET) at University of Maryland Baltimore County in 1996 as a research associate professor. He held this appointment until 2002. Steve has published more than 150 scholarly articles.
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By NASA
5 min read
NASA’s Apollo Samples, LRO Help Scientists Predict Moonquakes
This mosaic of the Taurus-Littrow valley was made using images from the Narrow Angle Cameras onboard NASA’s Lunar Reconnaissance Orbiter. The orbiter has been circling and studying the Moon since 2009. The ancient-lava-filled valley is cut by the Lee-Lincoln thrust fault, visible as a sinuous, white line extending from South Massif (mountain in the bottom left corner) to North Massif (mountain in the top center) where the fault abruptly changes direction and cuts along the slope of North Massif. The Lee-Lincoln fault has been the source of multiple strong moonquakes causing landslides and boulder falls on both North and South massifs. The approximate location of the Apollo 17 landing site is indicated to the right of the fault with a white “x”. NASA/ASU/Smithsonian As NASA prepares to send astronauts to the surface of the Moon’s south polar region for the first time ever during the Artemis III mission, scientists are working on methods to determine the frequency of moonquakes along active faults there.
Faults are cracks in the Moon’s crust that indicate that the Moon is slowly shrinking as its interior cools over time. The contraction from shrinking causes the faults to move suddenly, which generates quakes. Between 1969 and 1977, a network of seismometers deployed by Apollo astronauts on the Moon’s surface recorded thousands of vibrations from moonquakes.
Moonquakes are rare, with the most powerful ones, about magnitude 5.0, occurring near the surface. These types of quakes are much weaker than powerful quakes on Earth (magnitude 7.0 or higher), posing little risk to astronauts during a mission lasting just a few days. But their effects on longer-term lunar surface assets could be significant. Unlike an earthquake that lasts for tens of seconds to minutes, a moonquake can last for hours, enough time to damage or tip over structures, destabilize launch vehicles on the surface, or interrupt surface operations.
“The hazard probability goes way up depending on how close your infrastructure is to an active fault,” said Thomas Watters, senior scientist emeritus at the Smithsonian’s National Air & Space Museum in Washington.
Watters is a long-time researcher of lunar geology and a co-investigator on NASA’s LRO (Lunar Reconnaissance Orbiter) camera. Recently, he and Nicholas Schmerr, a planetary seismologist at the University of Maryland in College Park, developed a new method for estimating the magnitude of seismic shaking by analyzing evidence of dislodged boulders and landslides in an area, as the scientists reported on July 30 in the journal Science Advances. Studies like these can help NASA plan lunar surface assets in safer locations.
Unlike an earthquake that lasts for tens of seconds to minutes, a moonquake can last for hours, enough time to damage or tip over structures, destabilize launch vehicles on the surface, or interrupt surface operations.
There are thousands of faults across the Moon that may still be active and producing quakes. Watters and his team have identified these faults by analyzing data from LRO, which has been circling the Moon since 2009, mapping the surface and taking pictures, providing unprecedented detail of features like faults, boulders, and landslides.
For this study, Watters and Schmerr chose to analyze surface changes from quakes generated by the Lee-Lincoln fault in the Taurus-Littrow valley. NASA’s Apollo 17 astronauts, who landed about 4 miles west of the fault on Dec. 11, 1972, explored the area around the fault during their mission.
By studying boulder falls and a landslide likely dislodged by ground shaking near Lee Lincoln, Watters and Schmerr estimated that a magnitude 3.0 moonquake — similar to a relatively minor earthquake — occurs along the Lee Lincoln fault about every 5.6 million years.
“One of the things we’re learning from the Lee-Lincoln fault is that many similar faults have likely had multiple quakes spread out over millions of years,” Schmerr said. “This means that they are potentially still active today and may keep generating more moonquakes in the future.”
The authors chose to study the Lee-Lincoln fault because it offered a unique advantage: Apollo 17 astronauts brought back samples of boulders from the area. By studying these samples in labs, scientists were able to measure changes in the boulders’ chemistry caused by exposure to cosmic radiation over time (the boulder surface is freshly exposed after breaking off a larger rock that would have otherwise shielded it).
This cosmic radiation exposure information helped the researchers determine how long the boulders had been sitting in their current locations, which in turn helped inform the estimate of possible timing and frequency of quakes along the Lee-Lincoln fault.
This 1972 image shows Apollo 17 astronaut Harrison H. Schmitt sampling a boulder at the base of North Massif in the Taurus-Littrow valley on the Moon. This large boulder is believed to have been dislodged by a strong moonquake that occurred about 28.5 million years ago. The source of the quake was likely a seismic event along the Lee-Lincoln fault. The picture was taken by astronaut Eugene A. Cernan, Apollo 17 commander. NASA/JSC/ASU Apollo 17 astronauts investigated the boulders at the bases of two mountains in the valley. The tracks left behind indicated that the boulders may have rolled downhill after being shaken loose during a moonquake on the fault. Using the size of each boulder, Watters and Schmerr estimated how hard the ground shaking would have been and the magnitude of the quake that would have caused the boulders to break free.
The team also estimated the seismic shaking and quake magnitude that would be needed to trigger the large landslide that sent material rushing across the valley floor, suggesting that this incident caused the rupture event that formed the Lee-Lincoln fault.
A computer simulation depicting the seismic waves emanating from a shallow moonquake on the Lee-Lincoln fault in the Taurus-Littrow valley on the Moon. The label “A17” marks the Apollo 17 landing site. The audio represents a moonquake that was recorded by a seismometer placed on the surface by astronauts. The seismic signal is converted into sound. Both audio and video are sped up to play 10 times faster than normal. The background image is a globe mosaic image from NASA’s Lunar Reconnaissance Orbiter’s Wide-Angle Camera. Red and blue are positive (upward ground motion) and negative (downward ground motion) polarities of the wave. Nicholas Schmerr Taking all these factors into account, Watters and Schmerr estimated that the chances that a quake would have shaken the Taurus-Littrow valley on any given day while the Apollo 17 astronauts were there are 1 in 20 million, the authors noted.
Their findings from the Lee-Lincoln fault are just the beginning. Watters and Schmerr now plan to use their new technique to analyze quake frequency at faults in the Moon’s south polar region, where NASA plans to explore.
NASA also is planning to send more seismometers to the Moon. First, the Farside Seismic Suite will deliver two sensitive seismometers to Schrödinger basin on the far side of the Moon onboard a lunar lander as part of NASA’s CLPS (Commercial Lunar Payload Services) initiative. Additionally, NASA is developing a payload, called the Lunar Environment Monitoring Station, for potential flight on NASA’s Artemis III mission to the South Pole region. Co-led by Schmerr, the payload will assess seismic risks for future human and robotic missions to the region.
Read More: What Are Moonquakes?
Read More: Moonquakes and Faults Near Lunar South Pole
For more information on NASA’s LRO, visit:
Media Contacts:
Karen Fox / Molly Wasser
Headquarters, Washington
202-358-1600
karen.c.fox@nasa.gov / molly.l.wasser@nasa.gov
Lonnie Shekhtman
NASA’s Goddard Space Flight Center, Greenbelt, Md.
lonnie.shekhtman@nasa.gov
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A Tapestry of Tales: 10th Anniversary Reflections from NASA’s OCO-2 Mission
When woven together, the tapestry of experiences of staff and scientists provide the complete picture of OCO-2.
Breathe in… Breathe out.
This simple rhythm sets the foundation of life on Earth – and it’s a pattern that a NASA satellite has been watching from space for over a decade.
On July 2, 2024, NASA’s Orbiting Carbon Observatory-2 (OCO-2) celebrated 10 years since its launch. Built by NASA/Jet Propulsion Laboratory (NASA/JPL), OCO-2 is now viewed as the gold standard for carbon dioxide (CO2) measurements from space and has quietly become a powerful driver of technological, ecological and even economic progress – including providing unexpected insights into plant health, crop-yield forecasting, drought early warning systems, and forest and rangeland management.
While the mission can point to many scientific achievements – some of which will be highlighted in the pages that follow – these accomplishments have occurred in the context of a larger human story. Scientists from around the world have come together to bring the important data from this satellite to the broader community, making OCO-2 the success that it is today.
This article provides readers an introduction to several transformative characters in this carbon story. The text peers behind the scenes to reveal the circuitous path that scientists and engineers must navigate to take a brilliant scientific concept and turn it into flight hardware that can be launched into space to make beneficial observations. The article depicts milestones that mark the mission’s successes, but also the failures, dead ends, long nights, and discouragements that make up the complexity of any science story.
2003: The First OCO Science Team Meeting
Measuring CO2 from space: Great idea but can it really be done?
When the idea for OCO was first proposed, it wasn’t universally embraced. At the time, more than a few experts scoffed at the idea that CO2 could be measured from space. Unlike nitrogen and oxygen, which are the dominant components of Earth’s atmosphere, CO2 is a trace gas, often no more than a few hundred parts per million. Miniscule, elusive, and nomadic, these measurements, though challenging, are crucial because of the important role CO2 plays in global climate.
In April 2003, a handful of hopeful scientists gathered at the California Institute for Technology (Caltech) for the first OCO Science Team meeting. To mark the occasion, they took a break during the meetings and lined up for a group photo – see Photo 1. Upon returning to work, they took up the arduous task of determining how to measure CO2 from space with a satellite and instrument hardware that simply did not exist.
OCO-2 was developed as part of NASA’s Earth System Science Pathfinder program, which supports small, low-cost missions that can still provide tremendous value for high-impact goals. The satellite carries a high-resolution spectrometer that collects data in three, narrow spectral bands. These spectral bands follow a divide and conquer strategy – two measure the clear “fingerprint” that CO2 leaves when it absorbs sunlight, and one takes the same measurement for oxygen (O2). The satellite is able to estimate CO2 concentrations by comparing the CO2 and O2 measurements.
Photo 1. A photo of participants during the original OCO Science Team meeting in 2003 at the California Institute of Technology. Photo credit: NASA/Jet Propulsion Laboratory OCO-2 2014: A Night at Vandenberg Air Force Base – To Launch or Not to Launch
A Mother and daughter await the midnight launch.
On a warm July evening in 2014, Vivienne Payne [JPL—current OCO-2 Project Scientist] would normally have tucked her four-year-old daughter into bed. But this night was special. They were lined up in a crowd waiting for a bus to take them to Vandenberg Air Force Base (now Space Force Base) in California. The group huddled in the chill night air awaiting the launch of the OCO satellite into the cosmos.
Shortly after midnight, hundreds of guests spread blankets across the gravelly ground to make their wait more comfortable. The air was charged with excitement. The participants waited quietly, murmuring to one another while the soft slosh of the Pacific Ocean offered a steady pendulum counting down to the impending launch. Like most people there that night, Vivienne felt upbeat and excited, but she also understood the gravity of the moment – a lot was riding on this launch.
While Vivienne had not been part of OCO since inception – having joined the project in 2012 – she knew OCO’s story. The first launch in 2009 ended in failure – when a faulty launch vehicle doomed the first OCO to a watery grave just moments after launch. In the aftermath, the OCO community were left in limbo, unsure if the project would survive. All was not lost. The Japan Aerospace Exploration Agency (JAXA) had successfully launched the Greenhouse-gas Observing satellite (GOSAT or IBUKI, Japanese for “breath”) that same year. This launch gave the OCO team an opportunity to test and refine their methods and algorithms using data from GOSAT.
As the gravel poked through the thick flannel blankets, Vivienne shifted uncomfortably waiting for the interminable countdown to reach its conclusion – and then everything stopped. A technical issue was detected, triggering a command to abort the launch.
Vivienne tried to explain to her disappointed daughter that this was simply how things went with space work. Sometimes you put in 1000 work-years of labor, get up in the middle of the night, and sit on uneven ground just to have everything stopped, unceremoniously.
Fortunately, the problem was quickly resolved, and the launch was rescheduled for the very next night. The participants returned to the staging site – rinse and repeat. This time Vivienne’s daughter was decidedly more sluggish. At 3:00 AM PDT, OCO-2 launched flawlessly into space. Unfortunately, a layer of fog obscured the spectators’ view. While it could not be seen, the resounding boom of the rocket taking off could be heard for miles.
For Vivienne, the sonic boom shocked the ears and rumbled through the bodies of the assembled crowd, who erupted in cheers. Having invested a lot of her time in the OCO project during the past two years, she was thrilled to see a successful launch.
As they returned to their hotel, Vivienne’s daughter remained unimpressed. “Mummy, let’s not do that again,” she said as she splayed out on the hotel bed and soon fell fast asleep.
2014: OCO-2 Joins A Larger Earth Observing Story
Leading to surprising new insights about how we see plants – and fires.
When OCO-2 launched in 2014, it joined a tightly coordinated group of Earth-observing satellites known as the Afternoon Constellation (or the “A-Train”) – see Figure 1. Flying in formation, the satellites could combine their observations to unlock more than any one mission could reveal on its own. Around the same time, scientists discovered that OCO-2 could do more than measure CO2 – it could also detect signs of plant health.
Figure 1. As of January 2024, the international Afternoon Constellation (“A-Train”) has two missions remaining: OCO-2 and GCOM-W. While Aqua and Aura continue to collect science data, the satellites have both slowly drifted out of the constellation – and will soon be decommissioned. CALIPSO ended its scientific mission on August 1, 2023. CloudSat radar operations ceased on December 20, 2023. Figure credit: NASA This discovery opened the possibilities for many different people, including Madeleine Festin, a former wildland firefighter in Montana, to work with OCO-2 data through an internship sponsored by the DEVELOP program, under the Earth Action element (formerly known as Applied Sciences) of NASA’s Earth Science Division.
When she was on the ground battling fires, Madeleine faced the harsh reality that fire prediction is notoriously difficult. In the field, she might be surrounded by smoke with just 20 ft (6 m) of visibility and red flames tearing through dry brush. Through her internship, she’s continued to tackle fires – just from a very different vantage point.
OCO-2 can detect the faint glow given off by plants during photosynthesis. This glow, called solar-induced fluorescence (SIF), offers a fast, sensitive indicator of plant health – see Figure 2. While other satellite-based tools, such as soil moisture or vegetation indices often detect stress only after damage has already occurred, SIF values drop the moment photosynthesis slows down – even if the plant still looks green. These data open the door to new applications: monitoring crop performance, identifying flood-damaged areas, and tracking drought before it sparks wildfires. That’s exactly how Madeleine is now using the data.
Madeleine’s team, a collaboration between OCO-2 scientists and the U.S. Forest Service, is working to update fire-risk models – some of which were developed in the 1980s – by incorporating SIF data.
“It’s fulfilling to know that you’re helping people,” Madeleine says. “And it’s nice to see science and firefighting work align.”
What makes the data even more powerful is OCO-2’s synergy with its A-Train counterpart, the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument on NASA’S Aqua platform. MODIS contributes land-cover information that, when paired with OCO-2’s SIF measurements, creates a detailed, global dataset of plant photosynthesis far beyond what either satellite could produce on its own. This example is a perfect synergistic pairing of measurements the A-Train has made possible. This information gives Madeleine and her team a better foundation for improving fire prediction tools.
“When firefighting, I used to hear about all these fire indices and metrics, and never knew what they meant,” Madeleine says. “Now, I’m learning the science behind it. And it’s interesting to think about how to get that information to firefighters on the ground, without overburdening them. What do they really need to know, and how can we deliver it in a way that helps?”
Figure 2. OCO-2 can measure plant health and photosynthesis from space. Puente Hills in eastern Los Angeles County, CA was once one of the largest landfills in the United States. The landfill has since been closed and its surface replanted to resemble a natural hill rising above the surrounding densely populated neighborhoods. These two images show how solar induced fluorescence (SIF), or “plant glow,” measured from OCO-2 and OCO-3 can be used to study urban greenery. The satellite image of the landfill and surrounding area [left] is followed by the SIF data overlay [right]. It is possible to compare the photosynthetic activity in the reclaimed landfill to nearby green spaces, as well as the plant health in the surrounding neighborhoods. Figure credit: NASA/Jet Propulsion Laboratory OCO-2, OCO-3 2016: Trekking to the Desert to Calibrate OCO-2
A technologist tramps around in the desert for instrument calibration.
Carol Bruegge [OCO-2—Technologist] had been to the Nevada desert so many times that she knew the way by heart. After skirting the Sequoia Forest and stopping for the night just past the Nevada border, she led a caravan of scientists along Highway 6 to mile marker 100, turning right onto a dirt road between two fence posts. Traveling 10 mi (16.5 km) down the road, a cloud of dust raised up from the car tires before the vehicle came to a stop at their destination – a patch of spindly instruments hammered into the barren desert floor. A big plaque marked the spot with the NASA logo and the words, “Satellite Test Site.” Standing under vast blue sky, Carol felt like she’d come home. Over the past few years, Carol had grown accustomed to leading these summer expeditions to Railroad Valley, NV. Often the team from JPL is joined by guests from Japan and other international colleagues representing various satellite missions – see Photo 2.
Photo 2. Group photo at Railroad Valley, NV during a summer field campaign. Carol Bruegge [OCO-2—Technologist, fifth from left] joins JPL members and guests from Japan working on the Greenhouse-gas Observing satellite. The group included [left to right] Hirokazu Yamamoto, Atsushi Yasuda, Hideaki Nakajima, Kei Shiomi, Thomas Pongetti, Bruegge, Dejian Fu, Junko Fukuchi, Makoto Saito, and Rio Kajiura. Photo credit: Tom Pongetti Carol knew that a successful field campaign required that they protect the instruments from the thick corrosive salt on the ground. Then the work could begin. The team hiked through the desert, collecting data that would ensure that OCO-2 could continue to provide high-quality data. As they hiked, the team carried hand-held spectrometers and measured the reflection of sunlight off Earth’s surface – timed precisely to match the moment the satellite passes overhead. By comparing the satellite’s readings with the ground-based measurements, the team can check the accuracy of the satellite readings. Reflection is one ingredient used in calculating the concentration of CO2 in the overlying air.
This remote location in Nevada wasn’t chosen by accident. In this part of the desert, the ground is perfectly flat, free of plants, and surrounded by ground littered with salt. This smooth, bare surface means no bumps and textures could disrupt the signal. For satellite calibration, it doesn’t get better than this.
2018: A Contentious Meeting in Noordwijk, Netherlands Sparks A Revolution
Could OCO-2 data be used to construct a nation-by-nation CO2 budget?
David Crisp [JPL emeritus—original OCO Principal Investigator and former OCO Science Team Leader] was tired. He didn’t know if it was jet lag or a reflection of the 16- to 18-hour workdays that had persisted for weeks. This particular week had started with a 10-hour flight from Los Angeles to the Netherlands. Now, he was standing in front of carbon scientists who had gathered from around the world.
“We need to put together a team that will be brave enough to make a CO2 budget, nation-by-nation,” David said.
His statement was met with thoughtful silence. Neither the data nor the models were ready. The consensus in the room was that the proposed venture may not work. David was magnanimous toward his critics, but he persisted with his idea.
Despite the rocky start, David met with representatives in charge of creating national emission inventories. He could see exasperation on their faces – running ragged, short-staffed, and trying to tally up every single barrel of oil and bushel of coal burned within their country’s boundaries. Even more challenging was tallying other tasks, such as deforestation and agricultural practices. David firmly believed that if OCO-2 could provide independent estimates from space as promised, it would provide the on-the-ground “carbon accountants” a reliable comparison – see Figure 3.
“We might have a satellite that can help,” Dave told them.
Although David has since retired, his perseverance is now bearing fruit. What began as a hypothetical solution is now much closer to reality. OCO-2’s high-precision measurements can now detect CO2 linked not just to countries, but large cities, industrial zones, and even individual power plants – all while researchers continue perfecting efforts to identify contributions from specific city sectors. OCO-2 provides a valuable, independent reference that nations can use to track the progress of their emission inventories. Researchers have created an entire OCO-2-sourced database of CO2 estimates by country, available through the U.S. Greenhouse Gas Center.
Figure 3. A map of the net emissions and removals of carbon dioxide (CO2) for 2015–2020 using estimates informed by OCO-2. Green depressions represent countries that remove more CO2 than emitted. Tan or red ridges represent countries with higher CO2 emissions than removed. Figure credit: NASA Science Data Visualization Studio 2019: Another OCO Takes flight – This Time to The International Space Station
Using “spare parts” to get more details about plant health and the carbon cycle.
After completing OCO-2, enough spare parts remained to construct a sister mission — OCO-3, which launched in 2019 to continue the work of measuring CO2 in the atmosphere from the International Space Station (ISS). The satellite’s unique orbit gives it a new vantage point. While OCO-2 continues to orbit Earth in a near-polar path, OCO-3 travels aboard the ISS in a lower, shifting orbit that allows it to study different areas of Earth’s surface at different times of day. OCO-3 also features a special scanning mode, called the snapshot area mapping (SAM) that lets scientists zoom in on areas of interest (e.g., cities or volcanoes) to study carbon emissions and vegetation in greater detail. Together, OCO-2 and OCO-3 provide complementary perspectives on Earth’s carbon cycle and plant health at space and time resolutions that have not been possible from space before.
2021: LA During a Pandemic Is a Far Cry from Finland
A data scientist foregoes saunas and berry-picking to make the dream of OCO-2 a reality.
Otto Lamminpää [JPL—Data Scientist] opened the picture his sister had texted him. His family looked back with wide smiles, holding buckets overflowing with scarlet berries and framed by the velvety firs of Finland. It had been almost two years since he’d seen them in person. He’d moved to Los Angeles to work at JPL on the OCO-2 and OCO-3 mission just as the COVID-19 pandemic engulfed the planet – see Photo 3.
Photo 3. Otto Lamminpää and Amy Braveman [both from JPL] in Finland. Photo credit: Otto Lamminpää Otto had never gone a week without seeing his family or skipped a berry-hunting party in the forests of his native Finland. With the forced distance, he placed himself in his home forests in his mind. He used this memory to marvel at the capacity of the vast forests to “breathe in” CO2 and convert it into trunks, branches, and roots through photosynthesis. With the COVID-19-imposed travel restrictions, Otto wasn’t sure how long he’d have to wait to go back home.
But whenever that homecoming occurred, Otto knew that a piece of OCO-2 would be waiting for him. North of the Arctic Circle in Sodankylä, a cluster of Earth instruments nestled in a snowy meadow include a field station that is part of the Total Carbon Column Observing Network (TCCON) of Fourier Transform Spectrometers (FTS). These stations act as OCO-2 and OCO-3’s “ground crew.” As the satellites orbit Earth, the FTS simultaneously measures direct solar spectra in the near-infrared spectral region, which allows for retrieval of column-averaged CO2 concentrations, as well as other key atmospheric constituents, over the snowy meadow. Back in the lab, Otto, along with other OCO-2 and OCO-3 scientists, compare the data collected at the field station to the satellite data. This feature was detailed in The Earth Observer article, titled “Integrating Carbon from the Ground Up: TCCON Turns Ten,” was published July–August 2014, Volume 26 issue 4, pp. 13–17).
Figure 4. Global map of the ground stations, also known as the Total Carbon Column Observing Network (TCCON). The red dots mark the active ground observation stations to validate OCO-2 and OCO-3 data. Figure credit: NASA-JPL/OCO-2 The station in Finland is one of about 30 similar TCCON sites scattered across the world, located in a variety of settings, from isolated tropical islands to the Pacific rim of Asia – see Figure 4. The stations in the far north play an especially valuable role since satellites often struggle to accurately measure CO2 over snow-covered ground. Therefore, reliable measurements from the ground stations become crucial to adjust and improve the satellite data.
Validation efforts such as the one described here are crucial to satellite observations. Comparisons between OCO-2 and TCCON show agreement is good, with a less than 1 ppm difference. It’s an impressive level of accuracy for a satellite orbiting more than 435 mi (700 km) away in polar orbit. The “ground truth” data collected at these field sites help to ensure that the satellite is accurately measuring “Earth’s breathing.”
For Otto, not just his family, but OCO-2 and OCO-3 itself was calling him home. As the pandemic began to ease, he returned to Finland to pick berries, jump in the sauna every night, and follow it up with snow angels. The homecoming was also coordinated with a trip past the Arctic Circle to the TCCON field station. The mission was part of him. Wherever he was, OCO-2 and OCO-3 would be there, too.
2023: The Annual Science Team Meeting Continues
Tracking changes in soil moisture during a colorful fall day.
Saswati Das [JPL—Postdoctoral Fellow] had missed the magnificent display of fall colors in deciduous forests of the East Coast of the United States. She’d seen nothing of the sort since moving to Los Angeles in 2022 to work on OCO-2. Before that, she’d been working on her Ph.D. at the Virginia Polytechnic Institute and State University (Virginia Tech), where the surrounding mountain peaks, meadows, and forests burned and sparked with crimson and gold in the autumn – see Photo 4. Now she was in another mountain town, Boulder, CO, to attend the OCO science team meeting. The aspens glittered like golden lanterns as her gang carpooled up the Flatiron Range to the science institute at Table Mesa.
Photo 4. Saswati Das takes a break from her Ph.D studies at nearby Virginia Tech (located in Blacksburg, VA) to enjoy the famous fall colors in the mountains of West Virginia. Photo credit: Saswati Das The research presented that week spanned a variety of topics. OCO-2 was being used to develop early drought forecasts. Because of its ability to detect the SIF “glow” that results from plant photosynthesis, OCO-2 can hint at flash droughts as early as three months before environmental decay unfold. By pairing OCO-2 data from other satellites, such as soil moisture data from NASA’s Soil Moisture Active Passive (SMAP) mission, scientists have opened a new window into drought forecasts and how water supply affects plant growth.
Surprises about our planet have also emerged. The tropical rainforests, long nicknamed the “lungs” of our planet, don’t always inhale and store carbon. At times, this region can exhale CO2, such as during the 2015–2016 El Niño. That period saw large tropical forests temporarily transform into net carbon sources – see Figure 5. The driver for this shift varied by region. The Amazon rainforest was driven by drought. Central Africa was driven by unusually high temperatures. Indonesia was driven by widespread fires.
Figure 5. The 2015–2016 El Niño increased the net carbon dioxide released by Earth’s tropical regions into the atmosphere. Figure credit: NASA-JPL/Caltech Data from OCO-2 and OCO-3 have also been used to study emissions from both cities and large power plants. This approach offers a new way to track changing emissions over time – without needing to continuously measure them on the ground. In addition, scientists are combining the satellite data with wind models and urban maps to trace CO2 to its sources (e.g., factories, ships, and roadways), helping to disentangle emissions from overlapping city sectors. These methods have been used to isolate industrial emissions in places, such as Europe, China, as well as over cities, such as Los Angeles, Paris, and Seoul. It has also revealed pandemic-era drops in traffic-related CO2 and increases in CO2 tied to shipping backlogs at the port. Two representatives from the World Bank shared how they used data from OCO-2 to demonstrate that building subway systems in cities can lower emissions. The goal is to eventually use these tools to evaluate local strategies (e.g., bike lanes and public transit) to reduce local carbon footprints.
When massive wildfires blazed through Australian forests and bushland in 2019, researchers used OCO-2 data to study the unfolding crisis. OCO-2 captured the increase in atmospheric CO2, and scientists used this data to refine estimates of how these events contribute to the global carbon budget.
As her mind wandered from the rich research she’d been immersed in for the past hour, Saswati spied Otto Lamminpää across the aisle in the wood-paneled auditorium. She thought back to the forests she loved on the East Coast, and the forests in Finland where Otto had grown up. OCO-2 was telling a story about the role that forests play in absorbing carbon and how this has changed over time.
2025 and Beyond
The Tapestry Continues to Expand…
In many ways, OCO-2 has had a long and unexpected journey. So has Hannah Murphy, another DEVELOP intern who will be starting a Master’s degree at Hunter College in New York in Fall 2025. She’s studied art and worked as a set designer in Los Angeles. She never pictured herself working with satellite data, but then she saw how visual it could be. The glowing, evocative images of Earth from space spoke to her artistic heart.
Now, Hannah works on SIF data as a 2025 NASA DEVELOP intern with the OCO-2 team, developing tools for wildfire risks. This project in particular hits close to home for Hannah, because she lived through the wildfires that tore through Los Angeles in January 2025. Although she remained safe, she knew several people who lost their homes, and the air was unsafe to breathe for weeks.
Just a few short months later, Hannah began studying the data from OCO-2. She is now part of the new generation of researchers that will take the mission’s remote sensing data and pave the way for implementing the findings to benefit society. Hannah understands, on a personal level, how closely our lives are linked to Earth systems that satellites, such as OCO-2 and OCO-3, study from space.
OCO-2 (and OCO-3) are built to study CO2 and plant health, but its impact goes deeper to the connections that tie our atmosphere, ecosystems, and lives together. That work continues to the new generation of scientists – one breath at a time.
Mejs Hasan
NASA/Jet Propulsion Laboratory
mejs.hasan@jpl.nasa.gov
Alan Ward
NASA’s Goddard Space Flight Center/Global Science & Technology Inc.
alan.b.ward@nasa.gov
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Last Updated Aug 12, 2025 Related Terms
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By NASA
NASA’s Nancy Grace Roman Space Telescope will be a discovery machine, thanks to its wide field of view and resulting torrent of data. Scheduled to launch no later than May 2027, with the team working toward launch as early as fall 2026, its near-infrared Wide Field Instrument will capture an area 200 times larger than the Hubble Space Telescope’s infrared camera, and with the same image sharpness and sensitivity. Roman will devote about 75% of its science observing time over its five-year primary mission to conducting three core community surveys that were defined collaboratively by the scientific community. One of those surveys will scour the skies for things that pop, flash, and otherwise change, like exploding stars and colliding neutron stars.
These two images, taken one year apart by NASA’s Hubble Space Telescope, show how the supernova designated SN 2018gv faded over time. The High-Latitude Time-Domain Survey by NASA’s Nancy Grace Roman Space Telescope will spot thousands of supernovae, including a specific type that can be used to measure the expansion history of the universe.Credit: NASA, ESA, Martin Kornmesser (ESA), Mahdi Zamani (ESA/Hubble), Adam G. Riess (STScI, JHU), SH0ES Team Called the High-Latitude Time-Domain Survey, this program will peer outside of the plane of our Milky Way galaxy (i.e., high galactic latitudes) to study objects that change over time. The survey’s main goal is to detect tens of thousands of a particular type of exploding star known as type Ia supernovae. These supernovae can be used to study how the universe has expanded over time.
“Roman is designed to find tens of thousands of type Ia supernovae out to greater distances than ever before,” said Masao Sako of the University of Pennsylvania, who served as co-chair of the committee that defined the High-Latitude Time-Domain Survey. “Using them, we can measure the expansion history of the universe, which depends on the amount of dark matter and dark energy. Ultimately, we hope to understand more about the nature of dark energy.”
Probing Dark Energy
Type Ia supernovae are useful as cosmological probes because astronomers know their intrinsic luminosity, or how bright they inherently are, at their peak. By comparing this with their observed brightness, scientists can determine how far away they are. Roman will also be able to measure how quickly they appear to be moving away from us. By tracking how fast they’re receding at different distances, scientists will trace cosmic expansion over time.
Only Roman will be able to find the faintest and most distant supernovae that illuminate early cosmic epochs. It will complement ground-based telescopes like the Vera C. Rubin Observatory in Chile, which are limited by absorption from Earth’s atmosphere, among other effects. Rubin’s greatest strength will be in finding supernovae that happened within the past 5 billion years. Roman will expand that collection to much earlier times in the universe’s history, about 3 billion years after the big bang, or as much as 11 billion years in the past. This would more than double the measured timeline of the universe’s expansion history.
Recently, the Dark Energy Survey found hints that dark energy may be weakening over time, rather than being a constant force of expansion. Roman’s investigations will be critical for testing this possibility.
Seeking Exotic Phenomena
To detect transient objects, whose brightness changes over time, Roman must revisit the same fields at regular intervals. The High-Latitude Time-Domain Survey will devote a total of 180 days of observing time to these observations spread over a five-year period. Most will occur over a span of two years in the middle of the mission, revisiting the same fields once every five days, with an additional 15 days of observations early in the mission to establish a baseline.
This infographic describes the High-Latitude Time-Domain Survey that will be conducted by NASA’s Nancy Grace Roman Space Telescope. The survey’s main component will cover over 18 square degrees — a region of sky as large as 90 full moons — and see supernovae that occurred up to about 8 billion years ago.Credit: NASA’s Goddard Space Flight Center “To find things that change, we use a technique called image subtraction,” Sako said. “You take an image, and you subtract out an image of the same piece of sky that was taken much earlier — as early as possible in the mission. So you remove everything that’s static, and you’re left with things that are new.”
The survey will also include an extended component that will revisit some of the observing fields approximately every 120 days to look for objects that change over long timescales. This will help to detect the most distant transients that existed as long ago as one billion years after the big bang. Those objects vary more slowly due to time dilation caused by the universe’s expansion.
“You really benefit from taking observations over the entire five-year duration of the mission,” said Brad Cenko of NASA’s Goddard Space Flight Center in Greenbelt, Maryland, the other co-chair of the survey committee. “It allows you to capture these very rare, very distant events that are really hard to get at any other way but that tell us a lot about the conditions in the early universe.”
This extended component will collect data on some of the most energetic and longest-lasting transients, such as tidal disruption events — when a supermassive black hole shreds a star — or predicted but as-yet unseen events known as pair-instability supernovae, where a massive star explodes without leaving behind a neutron star or black hole.
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This sonification that uses simulated data from NASA’s OpenUniverse project shows the variety of explosive events that will be detected by NASA’s Nancy Grace Roman Space Telescope and its High-Latitude Time-Domain Survey. Different sounds represent different types of events, as shown in the key at right. A single kilonova seen about 12 seconds into the video is represented with a cannon shot. The sonification sweeps backward in time to greater distances from Earth, and the pitch of the instrument gets lower as you move outward. (Cosmological redshift has been converted to a light travel time expressed in billions of years.) Credit: Sonification: Martha Irene Saladino (STScI), Christopher Britt (STScI); Visualization: Frank Summers (STScI); Designer: NASA, STScI, Leah Hustak (STScI) Survey Details
The High-Latitude Time-Domain Survey will be split into two imaging “tiers” — a wide tier that covers more area and a deep tier that will focus on a smaller area for a longer time to detect fainter objects. The wide tier, totaling a bit more than 18 square degrees, will target objects within the past 7 billion years, or half the universe’s history. The deep tier, covering an area of 6.5 square degrees, will reach fainter objects that existed as much as 10 billion years ago. The observations will take place in two areas, one in the northern sky and one in the southern sky. There will also be a spectroscopic component to this survey, which will be limited to the southern sky.
“We have a partnership with the ground-based Subaru Observatory, which will do spectroscopic follow-up of the northern sky, while Roman will do spectroscopy in the southern sky. With spectroscopy, we can confidently tell what type of supernovae we’re seeing,” said Cenko.
Together with Roman’s other two core community surveys, the High-Latitude Wide-Area Survey and the Galactic Bulge Time-Domain Survey, the High-Latitude Time-Domain Survey will help map the universe with a clarity and to a depth never achieved before.
Download the sonification here.
The Nancy Grace Roman Space Telescope is managed at NASA’s Goddard Space Flight Center in Greenbelt, Maryland, with participation by NASA’s Jet Propulsion Laboratory in Southern California; Caltech/IPAC in Pasadena, California; the Space Telescope Science Institute in Baltimore; and a science team comprising scientists from various research institutions. The primary industrial partners are BAE Systems, Inc. in Boulder, Colorado; L3Harris Technologies in Melbourne, Florida; and Teledyne Scientific & Imaging in Thousand Oaks, California.
By Christine Pulliam
Space Telescope Science Institute, Baltimore, Md.
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Last Updated Aug 12, 2025 EditorAshley BalzerLocationGoddard Space Flight Center Related Terms
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6 min read NASA’s Roman Mission Shares Detailed Plans to Scour Skies
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By NASA
Explore This Section Science Courses & Curriculums for… STEM Educators Are Bringing… Overview Learning Resources Science Activation Teams SME Map Opportunities More Science Activation Stories Citizen Science 4 min read
STEM Educators Are Bringing Hands-On NASA Science into Virginia Classrooms
Professional learning experiences are integral to the enhancement of classroom instruction. Teachers, at the forefront of Science, Technology, Engineering, & Mathematics (STEM) education, play a key role in the advancement of STEM learning ecosystems and citizen science.
On June 24-25, 2025 – despite a major east coast heat wave – twenty-four educators from eight school districts in the Hampton Roads region of southeastern Virginia (Newport News, Hampton City, Virginia Beach City, Isle of Wight County, Poquoson City, Norfolk, York County, and Suffolk Public Schools) converged at the National Institute of Aerospace (NIA) in Hampton, VA for a professional development workshop led by experts from NASA Langley Research Center and the NASA Science Activation program’s NIA-led NASA eClips team. Developed in collaboration with another NASA Science Activation team, GLOBE (Global Learning and Observations to Benefit the Environment) Mission Earth, and with support from the Coastal Virginia STEM Hub (COVA STEM) – a “STEM learning ecosystem targeting pre-K to adult residents in Coastal Virginia” – this two-day training, also provided comprehensive resources, including lesson plans, pacing guides, classroom activities, and books, all designed for integration into Hampton Roads classrooms.
The NASA Langley team led workshop participants through a training about GLOBE, a program dedicated to advancing Earth System science through data collected by volunteer members of the public, also known as ‘citizen scientists’. GLOBE invites educators, students, and members of the public worldwide (regardless of citizenship) to collect and submit cloud, surface temperature, and land cover observations using the GLOBE Observer app – a real-time data collection tool available right on their smartphones. These observations are then used to help address scientific questions at local, regional, and global scales. Through this training, the educators participated in K-20 classroom-friendly sample lessons, hands-on activities, and exploring the GLOBE Observer app, ultimately qualifying them as GLOBE Certified Educators. Earth System science lessons, activities, and information on how to download the GLOBE Observer citizen science app are available on the GLOBE website. Similarly, NASA eClips, which focuses on increasing STEM literacy in K-12 students, provided educators with free, valuable, standards-based classroom resources such as educator guides, informational videos, engineering design packets, and hands-on activities, which are available to educators and students alike on the NASA eClips’ website. Throughout the training, educators collaborated in grade-level groups, brainstorming new ways to integrate these standards-based NASA science resources.
One educator envisioned incorporating GLOBE’s cloud resources and supportive NASA eClips videos into her energy budget unit. Others explored modifying a heat-lamp experiment to include humidity and heat capacity. One teacher enthusiastically noted in response to a GLOBE urban heat island lesson plan, “The hands-on elements are going to be really great deliverables!” The creative energy and passion for education were palpable.
The dedication of both NIA and NASA Langley to education and local community support was evident. This professional learning experience offered educators immediately-applicable classroom activities and fostered connections among NASA science, NASA eClips, the GLOBE Program, and fellow educators across district lines. One educator highlighted the value of these networking opportunities, stating, “I do love that we’re able to collaborate with our colleagues so we can plan for our future units during the school year”. Another participant commented, “This is a great program…I am going to start embedding [this] in our curriculum.”
GME (supported by NASA under cooperative agreement award number NNX16AC54A) and NASA eClips (supported by NASA under cooperative agreement award number NNX16AB91A) are part of NASA’s Science Activation Portfolio. Learn more about how Science Activation connects NASA science experts, real content, and experiences with community leaders to do science in ways that activate minds and promote deeper understanding of our world and beyond: https://science.nasa.gov/learn
GLOBE educator Marilé Colón Robles demonstrates a kinesthetic activity. Share
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Last Updated Aug 04, 2025 Editor NASA Science Editorial Team Location NASA Langley Research Center Related Terms
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