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NSIDC turns 50

Дата публикации: 14-09-2026 18:11:56

"Stranger Things" in the 2026 Arctic
The continuation of cool and stormy conditions over the Arctic Ocean during September bookends the strange summer of 2026. While global air temperatures were at or near record highs for June, July, and August, the summer was cool and stormy over the Arctic Ocean. The Arctic sea ice minimum extent tied for tenth lowest on the satellite record with 2008, 2010, and 2025, with a loose ice pack on the Atlantic side extending to the pole. However, the post-minimum freeze up has been rapid. Antarctic sea ice extent, which reached its maximum on September 14, dropped sharply through September, hitting record low daily extents since October 2.Overview of conditionsArctic sea ice extent for September 2026 averaged 4.81 million square kilometers (1.86 million square miles), thirteenth lowest in the satellite record (Figure 1a). This monthly average extent was 1.6 million square kilometers (618,000 square miles) below the 1981 to 2010 average (Figure 1b). Since the seasonal sea ice minimum that occurred on September 12, tying for tenth lowest in the satellite record, extent as of early October remains below average along the Eurasian coast, especially in the Kara and Barents Seas. While the Northern Sea route appears to be largely free of ice, significant ice remains in the southern (Amundsen’s) route of the Northwest Passage. Heavy ice cover blocks M’Clure Strait, the west end of the deepwater northern route. While a loose icepack in over the Atlantic side of the Arctic Ocean allowed the Swedish icebreaker Oden to reach the North Pole, open water areas quickly refroze after the seasonal sea ice minimum, and as of early October, extent had risen to the lower interdecile range of extents in the satellite record. 
























Figure 1a. Arctic sea ice extent for September 2026 was 4.81 million square kilometers (1.86 million square miles). The magenta line shows the 1981 to 2010 average extent for that month. Sea Ice Index data. About the data — Credit: National Snow and Ice Data CenterFigure 1b. This graph shows Arctic sea ice extent as of October 5, 2026, along with daily ice extent data for four previous years and the record low year. 2026 is shown in blue, 2025 in green, 2024 in orange, 2023 in brown, 2022 in magenta, and 2012 in dashed brown. The 1981 to 2010 median is in dark gray. The gray areas around the median line show the interquartile and interdecile ranges of the data. Sea Ice Index data. — Credit: National Snow and Ice Data CenterConditions in contextAs was the case for all of summer (see summer summary below), low sea level pressure dominated the Arctic Ocean during September, accompanied by below-average temperatures that fostered rapid ice growth (Figure 2a). Air temperatures at the 925 hPa level (about 2,500 feet above the surface) were 0 to 1 degree Celsius (0 to 2 degrees Fahrenheit) below average over much of the Arctic Ocean, but strongly above average over northern Eurasia (Figure 2b).
























Figure 2a. This plot shows average sea level pressure in the Arctic in hectopascals for September 2026. Yellows and reds indicate high air pressure; blues and purples indicate low pressure. — Credit: NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences LaboratoryFigure 2b. This plot shows the departure from average air temperature in the Arctic at the 925 hPa level, in degrees Celsius, for September 2026. Yellows and reds indicate above average temperatures; blues and purples indicate below average temperatures. — Credit: NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences LaboratorySeptember 2026 compared to previous yearsThe downward linear trend in September Arctic sea ice extent through 2026 is 74,100 square kilometers (28,600 square miles) per year or 11.6 percent per decade relative to the 1981 to 2010 average (Figure 3). Based on the linear trend, since 1979, September has lost 3.24 million square kilometers (1.25 million square miles) of sea ice. This is equivalent to twice the size of Alaska.  














Figure 3. Monthly September ice extent for 1979 to 2026 shows a decline of 11.6 percent per decade.



— Credit:
National Snow and Ice Data Center


Regional contributions to September extentFor this monthly post, we present a time series of September monthly ice extents in a new format (Figure 4). The black line depicts the overall trend. Regional differences from average for each year are shown as colored bars for each sector of the Arctic. This presents the data in a way that allows some insight into the contributions to the overall positive or negative September extent difference from average. Since 2007, with few exceptions, differences from average have been negative in all sectors; in the last century, regional differences were more varied. Since 2007, negative differences from average in the Beaufort and Chukchi Seas and in the East Siberian and Laptev Seas have remained prominent, but their magnitudes have shifted from year to year largely in response to shifting summer weather patterns.














Figure 4. This time series shows Arctic sea ice extent for the month of September as a whole (black line) along with regional differences from the 1981 to 2010 average for every year since 1979.



— Credit:
J. Stroeve, National Snow and Ice Data Center


Spring in the AntarcticAfter reaching its maximum extent on September 14, Antarctic sea ice extent sharply declined, and as of October 6, was close to the record low for the date set in 2023. As was done for the Arctic, a graph presents the September Antarctic sea ice extent time series along with differences from average for each year (Figure 5). While the low extents since 2022 stand out clearly, in each of these low years, extent was above average in some sectors. This stands in sharp contrast to the Arctic. Note how in 2022, extent was above average in the Ross Sea, shifting to below average in 2023. However, during the record maximum extents of 2012 to 2015, nearly all regions showed a positive difference from average. 














Figure 5. This time series shows Antarctic sea ice extent for the month of September as a whole (black line) along with regional differences from the 1981 to 2010 average for each year since 1979.



— Credit:
J. Stroeve, National Snow and Ice Data Center


The 2026 summer melt season in summaryThe 2026 melt season in the Arctic was unusual in the extreme. Through most of May, extent was tracking at near record low levels. Starting in June, the pace of ice loss substantially slowed, and the minimum extent, which occurred on September 12, ended up as tenth lowest in the satellite record, tying with 2008, 2010, and 2025. Nevertheless, the loose ice pack on the Atlantic side of the Arctic Ocean, extending nearly to the North Pole, eased the voyage of the Swedish icebreaker Oden to the pole, carrying scientists along with tourists.A highly stormy atmospheric pattern over the central Arctic Ocean attended by cool and cloudy conditions inhibited sea ice melt. A pronounced average low pressure centered near the North Pole lingered in June, July, and August (Figure 6a). While cyclone activity over the central Arctic Ocean tends to be maximized in summer, the persistence of this cyclonic pattern was remarkable. In summer, in “free drift” conditions, where there is little floe-to-floe interaction, cyclonic (counterclockwise) winds promote the spreading of the sea ice cover, which likely accounts for the loose ice conditions just noted. Past research shows that summer cyclones that enter the Arctic Ocean, especially from Eurasia and mature in their passage, develop a cold-cored structure. Each cyclone moving into the region reinforces the persistent cold-cored, low structure, which extends into the tropopause much like a vertical stack. Interestingly, based on the ERA5 reanalysis, despite all the cyclones, summer precipitation over the Arctic Ocean as a whole was not notably above average.   The attendant pattern of summer air temperature as a difference from average at the 925 millibar level (about 2,500 feet above the surface) was equally unusual (Figure 6b). When sea ice cover is melting, air temperatures will hover around the freezing point. However, over much of the ocean, temperatures remained below average. This was especially clear in June when melt started late. While temperatures over the ocean reflected the cold-cored nature of cyclone maximum and extensive cloud cover, temperatures on Arctic land were far above average over the Canadian Arctic Archipelago, western Europe, and central Eurasia. 
























Figure 6a. This plot shows average sea level pressure in the Arctic in millibars for June, July, and August. Yellows and reds indicate high air pressure; blues and purples indicate low pressure. — Credit: NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences LaboratoryFigure 6b. This plot shows the departure from average air temperature in the Arctic at the 925 hPa level, in degrees Celsius, for the months of June, July, and August. Yellows and reds indicate above average temperatures; blues and purples indicate below average temperatures. — Credit: NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences LaboratoryThe cyclonic pattern persisted through September. After reaching its sea ice minimum on September 12, autumn freeze up was rapid, and as of this post, extent had reached the lowest decile in the satellite record.This cyclonic pattern also played a role in the late melt out of the Beaufort and Chukchi Seas. Unusual compared to recent years, sea ice remained near the Alaskan coast into August, which is near the location of the 1981 to 2010 average. However, the ice melted rapidly and by the end of August, the region was largely ice free in the passive microwave data (though operational ice charts indicated low concentration ice).Relatively cool conditions and cyclonic pressure contributed to the late ice loss. The reason that the ice eventually did melt was because the area was dominated by first-year ice, which is thinner and more susceptible to melt out completely (Figure 6c). Overall, the Arctic sea ice cover has much less multiyear ice and thus is thinner than it was during the 1980s. Since 2007, at the end of the summer melt season, the multiyear extent has varied between 1.3 million and 1.9 million square kilometers (502,000 square miles and 734,000 square miles), significantly lower than the roughly 3.5 million square kilometers (1.35 million square miles) during the 1980s. And since 2012, the oldest, thickest ice (greater than 4-years old) has nearly disappeared, with 250,000 square kilometers (97,000 square miles) or less each year compared to the approximate 1.5 million square kilometers (579,000 square miles) before 2005. While this summer was relatively cool over the Arctic Ocean, the long-term warming trend has resulted in more melt and faster distribution of sea ice, which means that ice is not surviving nearly as long as it used to. 














Figure 6c. The top left map shows Arctic sea ice age during the week of March 12 to 18, 2026, the week of the maximum extent; a larger swath of first-year ice extends into the Beaufort Sea, though older ice is found near the coast. The top right map shows Arctic sea ice age during the week of September 3 to 9, 2026, just before the minimum extent; most of the ice in the Beaufort and Chukchi Seas has melted out. The bottom time series shows extent of multiyear ice in black and ice greater than 4-years old in red at the seasonal minimum for 1985 to 2026. The oldest ice (in red) shows substantial decline.



— Credit:
Tschudi et al., 2019a and 2019b


Sea ice in the Antarctic remained below the lowest interdecile range since the beginning of the austral growth season that started in late March 2026, but above the record low of 2023 (Figure 6d). The maximum extent, reached on September 14, was the third lowest in the satellite record, repeating a recent pattern of low maximum extents discussed in more detail above. Since October 2, extent has fallen to record low daily values, surpassing 2023’s records. The post-maximum areas of loss are in the Ross and Amundsen seas, and the Indian Ocean sector (Figure 6e). 
























Figure 6d. The graph above shows Antarctic sea ice extent as of October 6, 2026, along with daily ice extent data for four previous years and the record 2014 year. 2026 is shown in blue, 2025 in green, 2024 in orange, 2023 in brown, 2022 in magenta, and 2014 in dashed brown. The 1981 to 2010 median is in dark gray. The gray areas around the median line show the interquartile and interdecile ranges of the data. Sea Ice Index data. — Credit: National Snow and Ice Data CenterFigure 6e. Antarctic sea ice extent for September 2026 was 17.32 million square kilometers (6.69 million square miles). The magenta line shows the 1981 to 2010 average extent for that month. Sea Ice Index data. About the data — Credit: National Snow and Ice Data Center    
agnieszka.gaut…
Wed, 10/07/2026 - 14:00

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Analysis - Sea Ice Today


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Wed, 10/07/2026 - 12:00


Geophysical Measurement

Sea ice



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Основное содержимое страницы с новостью.

MONDAY, SEPTEMBER 14, 2026

NSIDC 50-years logo

NSIDC celebrates 50 years: 1976 to 2026. — Credit: Agnieszka Gautier/NSIDC

By Michon Scott

In 1976, the United States celebrated its bicentennial, disco topped the charts, and no one had yet seen a Star Wars movie. That same year, the National Snow and Ice Data Center (NSIDC) opened its doors.

The next half-century transformed both the planet and the ways scientists observe it. Global population nearly doubled to 8.2 billion, Earth-observing satellites multiplied, computing power soared, and NSIDC grew from a two-person staff reporting to founding director Roger Barry into an organization of roughly 85 employees (See Our History for a detailed timeline.)

The technological change over that time was even more dramatic. Initially named the World Data Center (WDC-A) for Glaciology, NSIDC started as a small library. Its holdings were mostly on paper. To fit information into a smaller space, the leading technology included microfilm and microfiche—miniature images of paper documents stored on rolls or cards of film.

“One of my favorite artifacts from NSIDC’s early days is a microfiche reproduction of the paper ‘Problems associated with large scientific data bases,’” said NSIDC Director Mark Serreze. The microfiche reproduction sits on the same bookshelf in his office as other vintage data-storage devices, including a magnetic tape reel roughly a foot in diameter, and a supersized floppy disk measuring roughly 8 inches across.

Dating from the year of NSIDC’s founding, the presciently titled “Problems associated with large scientific data bases” by J.M Cheadle occupies a roughly 4-by-6-inch microfiche card in NSIDC Director Mark Serreze’s office, next to other data-storage artifacts. — Credit: Mark Serreze and Mistia Zuckerman/NSIDC

NSIDC’s paper-based library soon changed. Before long, NSIDC became a data repository for satellite observations, aerial photography, fieldwork records, Indigenous perspectives, and rescued data. Throughout, NSIDC employed a staff of scientists and data experts who could interpret the data center’s vast holdings and make science understandable to students, teachers, planners, politicians, and taxpayers.

How Earth-observing technologies have advanced

Field expeditions, ship surveys, and local records of snow and ice go back centuries. Beginning in the twentieth century, aerial photographs also shed light on the planet’s ever-changing surface, but stitching together aerial photographs into reliable maps was complex and expensive.

Satellite technology began to change Earth observation nearly two decades before NSIDC opened. The Soviet Union launched Sputnik 1 in 1957, followed in 1960 by the United States’ TIROS-1, which demonstrated the potential of satellites for observing weather. NASA’s Nimbus missions followed, and Landsat 1 launched in 1972, starting a decades-long satellite record that continues today.

The first Television Infrared Observation Satellite (TIROS-1) captured the world’s first television image from space on April 1, 1960. As opposed to film-based video, television imagery was electronic. — Credit: NASA

NOAA launched the first Geostationary Operational Environmental Satellite (GOES-1) in 1975. Geostationary satellites remain positioned over the same part of Earth, making them valuable for tracking weather. Observing Earth’s polar regions, however—where much of NSIDC’s data and research are focused—needs different, lower-altitude orbits.

The first of the Geostationary Operational Environmental Satellites (GOES-1) captured its inaugural image on October 25, 1975. — Credit: NOAA

Polar-orbiting satellites upgraded Earth observation in 1978—two years after NSIDC started. Polar-orbiting satellites had made earlier observations, including Landsat, starting in 1972, and NOAA satellites, beginning in 1966. But the Nimbus-7 satellite, launched on October 24, 1978, began providing a long-term, consistent polar-observation record.

Nimbus-7 carried the Scanning Multichannel Microwave Radiometer (SMMR) sensor, and starting October 25, 1978, SMMR observed the whole globe every two to three days. Those observations continued until August 20, 1987. Starting July 9, 1987, the Special Sensor Microwave/Imager (SSM/I) took daily observations. Data from those and many other polar-orbiting satellites found a distribution hub at the NASA NSIDC Distributed Active Archive Center, which was formalized in 1993.

The satellite sensors NSIDC has relied on for sea ice measurements have typically been passive microwave sensors. Rather than bouncing a beam of energy off Earth’s surface, these sensors simply observe energy coming from the planet, in the microwave portion of the electromagnetic spectrum. Although invisible to human eyes, a sensor operating in that portion of the electromagnetic spectrum “sees” sea ice through clouds and darkness—including the months-long night of polar winter.

More polar-orbiting instruments followed, including AVHRR, first launched in 1978; NASA’s MODIS sensors aboard Terra and Aqua, beginning in 1999 and 2002; and VIIRS, which NASA and NOAA began using in 2011 to supplement the MODIS record. Together, these increasingly capable instruments provided more frequent and detailed observations of Earth’s surface.

The NASA/NOAA Visible Infrared Imaging Radiometer Suite (VIIRS) captured this image of a nearly ice-free Northwest Passage on August 9, 2016. — Credit: NASA

Laser altimeters offered yet another perspective on changing icy regions.

NASA’s Geoscience Laser Altimeter System onboard NASA's Ice, Cloud, and land Elevation Satellite (ICESat/GLAS) took observations from 2003 to 2010. In 2018, NASA’s Advanced Topographic Laser Altimeter System instrument began flying aboard the Ice, Cloud and land Elevation Satellite-2 (ICESat-2/ATLAS). Both GLAS and ATLAS sent laser pulses toward Earth, measuring the amount of time required for pulses to return to the sensor’s receiver. Whereas ICESat/GLAS sent 40 pulses per second, ICESat-2/ATLAS sends 10,000. These laser altimeters have provided precise measurements of surface elevations, although over narrow tracks.

This image is compiled from repeat observations by the Advanced Topographic Laser Altimeter System (ATLAS) instrument aboard NASA’s Ice, Cloud and land Elevation Satellite-2 (ICESat-2). Showing conditions for May 2021, this still is part of an animation of monthly average Arctic sea ice thickness from November 2018 to April 2022. — Credit: NASA

Satellites have grown in reliability and precision, improving understanding of our planet’s rapidly changing frozen regions. Still, satellites have not been the only source of Earth observation. NASA, for instance, has supplemented satellite observations with fieldwork measurements such as SnowEx, and aerial surveys such as Operation IceBridge, which bridged the gap between the ICESat and ICESat-2 missions. Through it all, NSIDC has managed and shared data on behalf of funding agencies, namely NASA, NOAA, and the US NSF.

Teaching old maps new tricks

Working with satellite observations initially meant adapting existing tools not wholly suited to the task. Reflecting on satellite image processing in 1978, Arthur Cracknell of the University of Dundee recalled, “In those days photographic images were generated in Dundee on old photofacsimile machines salvaged from newspaper offices … [T]ransparent sheets with (curved) grids of latitude and longitude … were placed on top of the photographic paper or negative film while it was being exposed.”

Decades of technological advancement means satellite imagery is often provided in grid format today. Converting satellite observations of a round planet onto a flat grid involves tradeoffs and decisions, though, because there is no perfect method. NSIDC began innovating in the early 1990s with the popular Equal-Area Scalable Earth (EASE) Grids map projections, to improve representation of the polar regions.

Declassification, digitization, preservation, and rescue

NSIDC has provided a home and acted as a distribution hub for newly acquired satellite observations, but NSIDC has done more than that.

NSIDC has, on multiple occasions, rescued records that might otherwise be lost, such as Nimbus observations made before the continuous polar-orbiting satellite record. NSIDC has also preserved historical films, including Good Days on the Trail, 1938-1942, and International Geophysical Year, 1957-1958 Drifting Station Alpha Documentary. Film footage comprises just part of what NSIDC has preserved in the Arctic Ice Dynamics Joint Experiment (AIDJEX) collection, resulting from an American-Canadian Arctic project in the 1970s.

Some data rescues were facilitated by geopolitical change. During the Cold War, Eastern and Western Bloc nations considered the possibility that the Arctic region could become a theater of warfare. So, they collected libraries full of data about the frozen north, including observations gathered by submarines beneath Arctic sea ice. Starting in the 1990s, the United States and Russia cooperated to declassify and share observations of weather, climate, ocean circulation, and sea ice, in the form of Environmental Working Group (EWG) Atlases.

Ensuring historical records remain available to future generations sometimes requires putting old records into new formats.

As a cryospheric library, NSIDC stored more than books and journals. It also held a collection of glacier photographs, taken from the ground, from the air, and from space. NSIDC stored more than 20,000 photographic prints, and an additional 100,000 photographs on microfilm. The photographic prints were beautiful—an archive of glacier change over time. The prints were also fragile, and could only be viewed onsite, requiring interested viewers to travel to Colorado. In 2002, NSIDC began working with the NOAA Climate Database Modernization Program (CDMP). The result is the Glacier Photograph Collection, an online, searchable database of historic glacier photographs, some dating back to the nineteenth century.

Indigenous perspectives

Throughout the satellite era and well before that, some of the keenest insights on the Arctic have come from people who live there, and whose ancestors lived there. NSIDC through the Exchange for Local Observations and Knowledge of the Arctic (ELOKA) program has helped preserve Indigenous Knowledge with observation hubs, digital atlases, and websites while working with communities to ensure their data sovereignty.

Drawing from local observations, NSIDC developed the digital Yup’ik Atlas. — Credit: ELOKA

The US National Science Foundation has funded the ELOKA program and other projects like the Navigating the New Arctic Community Office (NNA-CO), aimed at mitigating threats associated with rapid Arctic warming.

The cooperative efforts strive to foster collaboration and consultation with the aim of preserving and sharing local observations and knowledge of the Arctic. Indigenous perspectives have become a part of NOAA’s annual Arctic Report Card.

Wild salmon dries in the sun in this snapshot from “The Northern Bering Sea: Our Way of Life.” — Credit: Bering Sea Elders/ELOKA How computing and data storage technologies have advanced

Advancements in satellite technology and local observing networks would have been far less useful without corresponding advancements in computing, data processing, and storage.

In the mid-1960s, Intel co-founder Gordon Moore observed that transistors were shrinking in size and growing in number at a predictable rate. He predicted that the number of transistors on a computer chip would continue to double roughly every two years. The prediction became known as Moore’s Law.

This graph shows Moore’s Law tracing the number of transistors per computer chip from 1971 to 2021. While the horizontal (time) axis is linear, the vertical (transistor) axis is logarithmic. — Credit: Our World in Data

In this Moore’s Law graph, the horizontal (time) axis is linear, but the vertical (transistor) axis is logarithmic. If the vertical axis were linear, this graph could run up the side of a skyscraper.

Growth in computing power was accompanied by dramatic declines in the cost of storing data. In 1976, storing a terabyte of data cost tens of thousands of dollars. Increasing demand from artificial intelligence operations has recently raised computer component prices, but even so, storage for a terabyte or more can be had for less than $50 today.

Storing a single terabyte of data in 1976 required 1,575 IBM 3350 Disk Pack Units at a cost of $62,500. — Credit: Kunle Campbell/2X Media, Oxford; Michael Sandberg’s Data Visualization Blog High-volume storage devices cost less than $50 in early August 2026. — Credit: Google

Falling data-storage prices translated into rising data-storage capacity. As satellites, aerial surveys, field expeditions, and local observation networks observed more, NSIDC could take in and share more data.

First, however, NSIDC needed supporting contracts.

Although NSIDC started in 1976, it did not get its current name until 1982. That year, NOAA established NSIDC as part of the Cooperative Institute for Research in Environmental Sciences (CIRES). NASA established its first contract with NSIDC the next year, to archive Scanning Multichannel Microwave Radiometer (SMMR) passive microwave sea ice data from the Nimbus-7 satellite. A decade after that, NSIDC became a NASA Distributed Active Archive Center (DAAC) in 1993, to manage cryospheric and related data for NASA’s Earth Observing System. In addition to SMMR, NSIDC began to manage and distribute data from many other satellite sensors. (See Our History for more.)

How data ingest has grown at NSIDC

Before NSIDC can distribute data on behalf of NASA or any other party, it must first ingest that data. NSIDC’s data ingest has not grown as dramatically as Moore’s Law predicted for transistors, but it has certainly increased.

Taking in more data for distribution to users required upgrades in hardware. — Credit: Photo copyright by Ron Weaver

NSIDC’s total archive volume passed the one-petabyte milestone in June 2019. NSIDC’s archive volume for NASA Earth science data sets stewarded by the DAAC crossed the one-petabyte mark in October 2019. NASA data sets accounting for the greatest growth in NSIDC data archives include NASA missions ICESat-2/ATLAS, VIIRS, SMAP, and Operation IceBridge.

“I remember it felt like a big deal when we passed the one-petabyte mark in data ingest,” said NSIDC technical services manager Daniel Crumly “but we quickly shot past that, especially when we started ingesting ICESat-2 data.”

This graph shows how the volume of Earth science data ingested by NSIDC increased from October 1, 2011, through October 2025. In places, this curve rises sharply then dips. When satellite missions reprocess data sets to newer versions, the processing of the old and new versions often occurs in parallel, which adds to the data load. Once the new version is confirmed reliable, the old version no longer needs to be retained. Note that the data holdings for the NASA NSIDC DAAC completed migration to the NASA Earthdata cloud in 2026. — Credit: Daniel Crumly/NSIDC

Data holdings at NSIDC grew due to technological advancement—satellite sensors able to observe more and NSIDC able to take in and manage more data. NSIDC began stewarding quantities of data unimaginable when the data center started 50 years ago. Continued advancements meant that eventually NASA Earth science data sets moved into the NASA Earthdata cloud. NSIDC still distributes and supports data sets as a NASA DAAC.

As of September 2026, NSIDC hosts over 1,480 data sets, funded by NASA, NOAA, US NSF, and others.

Web surfing changed (not quite) everything

In NSIDC’s earliest days, data requests might arrive via the US Postal Service. Incomplete requests would have to be clarified through follow-up phone calls or correspondence. That would change, but not immediately.

Between late 1989 and late 1990, computer scientist Tim Berners-Lee developed the technology behind the World Wide Web. NSIDC launched its first website in 1994 and migrated to NSIDC.org several years later. The website’s look and feel soon evolved even more.

In May 1997, the NSIDC website operated under a different URL. Like many science institution websites of the time, it could be charitably described as emphasizing substance over style. — Credit: Wayback Machine In February 2005, NSIDC.org was still destined for continued overhauls, but it had grown in both substance and style. — Credit: Wayback Machine

Over time, the site added educational content, scientific analyses, interactive applications allowing users to track changes, news and features, and functionality for data access.

NSIDC.org underwent periodic updates in structure and design, but the most comprehensive overhaul began in January 2020. “When we redesigned and organized the website back in 2020, we were dealing with over 20,000 pages of content that had accumulated over two decades,” recalled senior user engagement specialist Leslie Goldman, who led the effort. That overhaul concluded in July 2022, resulting in more logical design and greater consistency of user experience across programs and projects.

From a certain standpoint, NSIDC.org simply is the National Snow and Ice Data Center. The website is the data center’s face to the world, the portal to expertise about snow and ice, the means of sharing latest developments, and the way to find and use data. “One thing I love about our website is how it really demonstrates what makes NSIDC unique—that partnership between data stewardship and scientific research,” Goldman added.

From August 1, 2025, through July 31, 2026, NSIDC.org served more than 5 million pageviews. A significant portion of NSIDC traffic is focused on scientific data set access.

Making the website a useful portal to data took years of effort on NSIDC’s part, as well as changes in technology. The ease of access common today was a long time coming. Early Internet access still imposed major limitations. Dial-up connections made large files slow to download, and image-heavy or technologically demanding webpages could be impractical for many users.

NSIDC’s website made it easier for many users to contact the data center and request data, but not necessarily easier for NSIDC to distribute data. Requesting a big data set was one thing; downloading that data set at 1990s’ dial-up-modem speed was another. Before high-bandwidth Internet access was widespread, NSIDC had to provide users with an alternative to devoting hours of their time and telephone access to downloads.

Data distributionRemember CDs?

In NSIDC’s earliest days, big data sets had to be relayed on big wheels of magnetic tape. By the early 1990s, NSIDC had switched to compact disc (CD) format. CDs were certainly less cumbersome than magnetic tape, but not without challenges.

Retired NSIDC senior associate scientist Mary Jo Brodzik recalled the early days of Equal-Area Scalable Earth (EASE) Grid data distribution. “For the original EASE-Grid data, we knew that it was so large that the entire time series for Northern Hemisphere would require many CDs, and I was seriously concerned about all that plastic. So, I went on a hunt for better packaging, and I found the vendor that made the soft-pack sleeves with the light cardboard covers. I made my pitch to the DAAC to distribute the EASE-Grid data this way—cheaper, lighter weight to ship, less space on the user’s storage shelf, more environmentally friendly—and we were off to the races.”

NSIDC programs and projects lead Donna Scott remembered how, as a User Services representative in the early 2000s, she spent hours packaging and mailing CDs. Some were for data distribution; others were for educational materials, such as When the Weather is Uggianaqtuq, which shared Indigenous perspectives on a rapidly changing Arctic.

Better bandwidth eases data downloads

Luckily for many scientific data users, growing sizes of data sets coincided with increasing bandwidth. Much of NSIDC’s efforts in recent decades have been to make data findable and downloadable via NSIDC.org. NSIDC user services lead Lisa Booker said, “Data sets are getting larger, and support is more about helping users manage large data. As NASA moves into the cloud, more user support will possibly be technical support.” One development Booker welcomes, as someone who did her share of mailing CDs, is improved online access. “More data are going into always-accessible archives. In earlier years, NSIDC Operations had to stage most of the data. That’s rare now.”

This graph shows total data sets distributed by NSIDC from January 2011 through July 2026, on behalf of NASA, NOAA, and the US NSF. It shows distribution by volume, measured in terabytes (TB). — Credit: Lisa Booker/NSIDC This graph shows total data sets distributed by NSIDC from January 2011 through July 2026, on behalf of NASA, NOAA, and the US NSF. It shows distribution by individual files distributed. — Credit: Lisa Booker/NSIDC

“Users are attempting more technical workflows,” Booker observed. “Still, we aim to make data easier to use for more users.”

Beyond making data easier to use, NSIDC has provided more context and scientific analysis on what is happening in the cryosphere.

Sharing scientific insights

In 2005, the Arctic September sea ice minimum was the lowest extent yet observed in the satellite record. NSIDC scientists began anticipating in June that a record-low minimum might merit a press release. NSIDC worked with NASA and the University of Washington on a joint announcement. On the day of the planned release, however, NASA experienced a delay. At the direction of a NASA scientist, NSIDC went forward with the minimum announcement.

“Whether or not it was NASA’s intention, that made NSIDC the go-to place for sea ice news,” said senior research scientist and DAAC scientist Walt Meier.

After the 2005 Arctic sea ice minimum pushed NSIDC to the forefront of sea ice news, NSIDC got even more proactive and, with support from NASA, launched its Arctic Sea Ice News & Analysis (now named Sea Ice Today) subsite in 2006. Before long, Sea Ice Today expanded its scope to include Antarctic sea ice, as well as freely available statistics spreadsheets and interactive tools.

Today, the analysis posts and data tools under the Sea Ice Today umbrella consistently account for the plurality of web traffic to NSIDC.org. The subsite’s success prompted other analysis subsites at NSIDC.

Greenland Today (now named Ice Sheets Today) launched in 2013, CIRES senior research scientist Ted Scambos, a regular contributor to Sea Ice Today, led the effort with a team of international scientists, starting a year after the Greenland Ice Sheet experienced record melt. Karl Rittger, a research associate with the Institute of Arctic and Alpine Research (INSTAAR), worked with NSIDC to launch Snow Today in 2019. Like Sea Ice Today, Ice Sheets Today and Snow Today come with their own suites of data visualization tools.

Another plus comes from the interactive tools on the analyses subsites that let users equipped with only web browsers visualize what is happening in Earth’s frozen regions. In 2012, some NSIDC software developers found the perfect chance to innovate.

Our killer apps

“I want to do something like Google Finance but for sea ice,” software developer Matt Savoie declared in 2012. Savoie was tossing around ideas with his software-developing colleagues Kevin Beam and Luis Lopez.

Beam had just joined NSIDC. “I had never worked in a science environment before,” he said. He, Savoie, Lopez, and all the other developers were preparing for an upcoming hackathon, a three-day event in which everybody tried to innovate and make something amazing.

Lopez suggested making something interactive. “I made the suggestion that it would be cool if users could click on the curve and get the sea ice extent for that day, making the chart more dynamic,” he recalled. “Kevin implemented that idea a few weeks later!”

The timing was right for a fresh round of innovation.

A decade earlier, NOAA@NSIDC had launched the Sea Ice Index, offering daily and monthly map views, and comparisons of concentrations, extents, and trends. “The Sea Ice Index put easily accessible products in users’ hands and became the basis for other products,” said general project manager Ann Windnagel. “It’s used within NSIDC and outside NSIDC, including the Arctic Report Card.”

Sea Ice Index maps, which had originally been monthly, had become available for daily values in 2012. The code underlying them had just been rewritten and updated. Savoie and Beam put together the first iteration of one of NSIDC’s most popular interactive tools: Charctic. “We got the first version up pretty fast. Then we made the argument of ‘Let’s put some money into this,’” said Savoie.

Users can choose which years to display, time of year to focus on, and hemisphere to show. Making Charctic work meant thinking about the big picture and the details, such as how to handle leap years. The interactive tool has undergone continued refinement since 2012. Meanwhile, Charctic-based visualizations have been published many times outside NSIDC, both for Arctic and Antarctic sea ice. “Seeing images I created in The New York Times is pretty awesome,” Savoie said.

Just as Sea Ice Today inspired other analyses subsites at NSIDC, Charctic inspired other visualization tools, such as the interactive Greenland melt map, and derived visualizations have also appeared outside NSIDC.

This screenshot from August 2026 captures Charctic in its never-ending evolution. — Credit: NSIDC

NOAA@NSIDC’s Multisensor Analyzed Sea Ice Extent - Northern Hemisphere (MASIE-NH) is another interactive tool that makes user visualization easy. MASIE answers the question, “Where is the sea ice edge right now?”

“Answering that question is important to entities operating in the Arctic, because the ice edge determines where ship passage is—and is not—possible,” explained retired NOAA@NSIDC program manager Florence Fetterer. MASIE was developed in partnership with the US National Ice Center. The partnership makes the ice center’s highly accurate operational data available to a wide community of researchers.

As for Beam, his software development did not conclude with Charctic. Years later, he was still hard at work on a NASA project to reduce barriers to finding and working with elevation data. The result was OpenAltimetry, which lets users browse and download data gathered by NASA’s ICESat/GLAS and ICESat-2/ATLAS platforms. As NSIDC’s DAAC manager Amanda Leon said, “OpenAltimetry exemplifies what NSIDC has done throughout its history: bringing together expertise in science, data, technology, and user needs to make complex Earth science data more accessible and useful.”

Led by NSIDC’s deputy lead scientist Twila Moon, QGreenland is an international project designed to work with QGIS open-source software. It has received funding from the US NSF, but also has editorial and coordinating boards in Greenland and Denmark. It lets users explore dozens of data layers across many different topics, from the ice sheet to ocean and infrastructure to landscape. Users can examine Greenland, including the ice sheet, coastal regions, and nearby ocean regions. In fact, some datasets even span the full Arctic.

All these successes came from NSIDC’s culture of innovation but also collaboration. “There is a special synergy at NSIDC,” Donna Scott remarked, “not just between science and data, but also between our data programs. NOAA feeds Sea Ice Today, but NASA DAAC data feed NOAA data.”

Reflecting on NSIDC’s first “modern” interactive tool, Charctic, Beam said, “I wanted to make more interactive visualizations, and Charctic was the first of those.” He also pointed to the value of making the data directly accessible. “You can explore it for yourself,” he said. “It’s all right there.”

Future plans and reflections

Kevin Beam, Luis Lopez, and Matt Savoie hope to finesse Charctic further: to make it responsive so it can function better on all screen sizes, to make it easier for users to select from the near-50-year archive of sea ice observations, and to let others embed the tool in their own webpages.

Leslie Goldman is pleased with what the NSIDC.org website has accomplished so far. “We have a comprehensive data catalog of cryosphere and cryosphere-related data products. We make the data more accessible through easy-to-consume data graphics, scientific analyses, and help articles. And we provide foundational content and articles about what the cryosphere is and why it matters,” she said.

Lisa Booker hopes to grow NSIDC’s user base even further. “We’re focusing more on operational data, for instance, how snow affects water capacity. I want to put more data into the hands of decision makers. I also want to reach beyond the traditional cryospheric researcher,” she said. Booker has also initiated a more integrated approach to training and outreach, incorporating efforts from User Services, Technical Documentation, and Communications groups at NSIDC.

This diagram shows an early iteration of integrated science-enabling planning at NSIDC. — Credit: Lisa Booker/NSIDC

Beyond a small library of published papers, NSIDC scientists have served as authors and editors for the annual Arctic Report Card and the Bulletin of the American Meteorological Association’s annual State of the Climate. These contributions have occurred regularly over decades. Exceptional dedication to NSIDC’s mission spreads well beyond the data center’s science team. Since 2007, CIRES Outstanding Performance Awards have been awarded to NSIDC employees 41 times.

In Mark Serreze’s office—on the same shelf as his data-storage artifacts of microfiche, magnetic tape, and big floppy disks—is a Covid-protection kit from COP26, the United Nations Climate Change Conference he attended in November 2021. “NSIDC has endured a pandemic,” Serreze pointed out. “No matter what has come our way, we’ve continued to do good work. No matter what happens 50 years from now, 100 years from now, people will remember that NSIDC has been on the right side of history.”

NSIDC at 50 related links

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