Category: earth

Earth has caught itself a new mini-moon, and it is sticking around for Christmas.

The space rock, designated 2026 QQ8, was first observed in August 2026 after entering orbit around Earth in April 2026. The discovery was reported by the International Astronomical Union's Minor Planet Center on Thursday (Oct. 29).

The stay of QQ8 is a temporary one. The mini-moon will remain in the thrall of Earth's gravity through December before breaking away in 2027.

Scientists have recreated the orbital path of QQ8, finding that it takes 359 days, or about 0.98 of an Earth year, to orbit the sun. QQ8 closely approaches Earth around once every ten years, but this time the object came so close that Earth has been able to gravitationally seize it.

According to the Minor Planet Center, the closest QQ8 will come to our planet during this stay is around 353,000 miles (568,000 kilometers). That is around 110,000 miles (177,000 km) further out than the average distance between Earth and the moon.

Even if QQ8 were to come close enough to collide with Earth, it would likely be completely destroyed in our planet's atmosphere before it reaches the surface, as it is only around 6 feet (2 meters) in diameter.

This is far from the first time Earth has snagged itself a mini-moon, more accurately called a temporary satellite. In fact, research last year suggested that our planet could be orbited by as many as six mini-moons at any given time, with many of these being fragments of our more permanent natural satellite, the moon.

While QQ8 is tiny, it is larger than the average mini-moon. That is according to modelling earlier this year that suggested the average size for a temporary satellite is 75 centimeters (30 inches) across.

The same modelling suggested the average stay for such an object would be around nine months.

So if QQ8 was captured in April 2026, that means it should move away in January 2027.

The researchers behind those findings suggested that, were Earth to gravitationally grip a space rock around 10 feet (3 meters) wide, it could serve as a mini-moon for 10 to 20 years.

An iceberg has quickly escaped from the Weddell Sea in Antarctica, on its way to an icy new destination.

What is it?

As captured by a satellite in orbit, the Antarctic iceberg A-81 has quite quickly (for an iceberg) parted ways from its icy home, breaking off to drift toward a shallow underwater shelf in Georgia.

The 600-square-mile (1,550-square-kilometer) iceberg first broke off from the Brunt Ice Shelf in January of 2023. Now, generally speaking, giant icebergs don't travel that fast. But In just three years, this massive iceberg has traveled 1,400 miles (2,300 kilometers) north of the Brunt Ice Shelf. For an iceberg, that's really fast.

Over this time period, the iceberg drifted through the Weddell Sea in Antarctica's Southern Ocean before reaching the tip of the Antarctic Peninsula, floating further into the Scotia Sea and then finally now reaching the edge of a remote island in South Georgia.

In this satellite snapshot captured on Oct. 20, 2026, we can see the iceberg in its current location near an underwater shelf off the coast of South Georgia. While it isn't abnormal for icebergs like A-81 to break off from larger ice shelves, Brunt has recently had multiple large icebergs break off one quickly after the other, according to a statement from NASA.

Why is it incredible?

This image was captured by the MODIS (Moderate Resolution Imaging Spectroradiometer), an instrument on board NASA's Terra satellite.

Earth-observing satellites like Terra keep a close eye on changes on our home planet. In addition to this image, observations from Terra have showed how the iceberg has traveled over the last few years.

With satellites like Terra, scientists can keep a close eye on these changes in Antarctic ice, which is becoming increasingly important as climate change continues to progress across the globe, affecting everything from Arctic ice to sea levels rising, worsening natural disasters and more.

In 1927, Norwegian civil engineer and amateur radio operator Jørgen Hals made an unusual discovery: while monitoring transmissions from a shortwave radio station in Eindhoven, The Netherlands, he began hearing odd, "delayed" radio echoes, arriving approximately three seconds after the original transmissions, that sometimes accompanied the station's signals.

"From where this echo comes I cannot say for the present," Hals wrote of his peculiar discovery, adding that he could "only confirm that I really heard it."

Almost a century after Hals' discovery, the exact cause of this unusual phenomenon — known today as long delayed echoes, or LDEs — remains unknown. Their baffling nature has prompted a range of potential explanations, most of which focus on a variety of unexplained natural phenomena occurring in Earth's atmosphere. However, a few more far-out possibilities, including potential evidence of extraterrestrial technology, have also been considered.

What do we know?

A curious discovery

The enigma of long-delayed echoes has perplexed scientists since their initial detection by Hals, who at the time reported his odd findings to Norwegian physicist Carl Størmer. This prompted an investigation by Størmer with physicist Balthasar van der Pol, during which the duo was able to reproduce the phenomenon but were unsuccessful in determining its cause.

Since those early observations, ongoing reports of long-delayed echoes have continued to be recorded. Under normal conditions, radio echoes occur whenever a radio signal reflects or "bounces" off an object, although other conditions such as signals traveling through a delayed path can also cause echoes to occur.

Long delayed echoes, by contrast, are generally characterized by radio signals that return after more than 2.7 seconds following their original transmission, although the terminology has sometimes been applied more broadly.

Complicating investigations into this unusual brand of radio phenomena over the years has been their unpredictable nature, along with significant reported variances in the timing and nature of the delays, which has made it difficult for researchers to narrow down a single cause.

Possible explanations

Despite the challenges presented by this unique class of space mysteries, there are several theories that have been put forward over the years about what could cause long-delayed echoes.

In the mid 1980s, researchers R. J. Vidmar and F. W. Crawford conducted experiments in Alaska that aimed to detect long-delayed echoes, which built on earlier research they published involving possible detections in 1970. According to their findings at the time, Vidmar and Crawford hypothesized that radio signals could be captured between ionized layers in the atmosphere and "guided" over long distances.

More recently, University of Oslo researcher Sverre Holm has advanced a similar concept that he calls magnetospherically ducted echo (MDE), in which radio waves may become trapped within electrically charged regions of Earth's upper atmosphere and guided along magnetic field lines extending far into the magnetosphere. Under certain conditions, these signals may reach as far away as the opposite hemisphere before they are "bounced" back toward Earth, resulting in the delayed echo effect.

According to Holm, MDE "is the best understood mechanism for long delayed echoes" out of five promising explanations he outlines, adding that based on the MDE model, such long delayed echoes "can be predicted to what seems like about 5 ms accuracy using a simple model for the magnetic field lines."

Still, one problem that arises involves the relatively short delays associated with this mechanism, which may not necessarily account for the much longer, multi-second echoes reported in some historical observations. Since radio waves travel at close to the speed of light, a signal could theoretically cover distances equivalent to the planet's circumference several times in a single second. While this doesn't prove the signals actually followed such paths, it does imply that some of the reported instances of long-delayed echoes might correspond to dozens of journeys around the planet.

Speaking with Space about historical cases involving much lengthier long-delayed echoes, Holm was clear in expressing that the MDE theory also has its limitations.

"In my view," Holm told Space in an email, "Magnetospheric Duct Echoes cannot [account] for those historical LDEs at all."

To illustrate this, Holm points to two primary differences. First, the historical echoes were detected at approximately 9.55 MHz, well above the 1–4 MHz frequency range typically associated with MDEs. Additionally, historical LDEs reportedly exhibited delays ranging from 3 to 30 seconds, whereas MDEs generally produce delays of only a few hundred milliseconds.

By contrast, "MDES are only a few hundred milliseconds," Holm explained, meaning that they cannot account for all the characteristics of the earlier historic observations of long-delayed echoes.

Other theories that might be capable of filling some of the gaps in the long-delayed echo mystery include the idea that electromagnetic radio energy could be coupled into slower plasma-wave "modes" while traveling through Earth’s upper atmosphere, which, according to Holm’s review of the earlier work by Vidmar and Crawford, could potentially create much longer delays than ordinary radio propagation would allow.

After this proposed coupling into a plasma-wave mode, the signals may be converted back to ordinary electromagnetic signals and bounced back down to lower levels of Earth's atmosphere. Finally, a similar line of investigation has looked at whether clouds of plasma originating from the sun might also be able to produce the well-characterized echo effect.

What remains unknown?

Extraterrestrial origins?

Although scientific research has identified several promising explanations for long-delayed echoes, the mysterious nature of these events has also inspired more speculative theories over the decades, including some involving the search for extraterrestrial intelligence.

This unique dimension to the LDE mystery has its roots in the theories of Australian physicist Ronald Bracewell, who was the first to propose the idea that autonomous interstellar probes might be used by an advanced civilization as a means of establishing contact.

According to Bracewell, the initiators of such a hypothetical contact scenario might choose to reveal their presence by intercepting and re-transmitting radio signals rather than engaging in direct communication. Carl Sagan explored a similar concept in his novel "Contact", in which transmissions from the 1936 Olympics — the earliest broadcast signals to leave Earth's ionosphere — are intercepted and rebroadcast back to Earth as a data-encoded message originating from the Vega system.

However, more than a decade before the publication of Sagan's famous novel, Scottish writer Duncan Lunan attracted international attention for his 1973 article in the journal "Spaceflight" outlining his belief that he had successfully decoded a radio message dispatched from an extraterrestrial probe. According to Lunan, the initial detection of this "hidden" alien signal had taken place decades earlier in 1927, with the famous discovery of long-delayed echoes by Jørgen Hals.

Lunan's theory essentially went like this: an extraterrestrial civilization in the Epsilon Boötis system had deployed a hypothetical autonomous communications probe (known as a Bracewell probe) to Earth in the distant past, which had been comfortably orbiting in one of Earth's gravitationally stable Lagrange points for thousands of years.

Using the original long-delayed echo detections from Hals and Størmer's research decades earlier, Lunan placed the transmitted sequence on a vertical axis, while placing the recorded echo delay time on a horizontal axis, revealing what he believed to be a view of the constellation Boötes as it might have looked 15,000 years ago — right around the time the suspected space probe would have been dispatched to Earth.

Despite Lunan's imaginative theory, an alternative hypothesis proposing a natural cause behind long-delayed echoes was subsequently advanced by Anthony Lawton, which ultimately garnered an award from the British Interplanetary Society. By 1976, Lunan had withdrawn his ideas in an article published in the Journal of the Society of Electronic and Radio Technicians, although he would eventually revisit a version of the theory in the 1990s.

The mystery continues

While few modern researchers seriously consider extraterrestrial hypotheses to explain long-delayed echoes, these obscure phenomena remain intriguing, even as ongoing research sheds light on their possible causes. Explanations such as Sverre Holm's magnetospherically ducted echo model offer promising mechanisms that may account for at least some of these unusual signals, although important questions remain unanswered.

For now, long-delayed echoes serve as a reminder of the challenges of studying electromagnetic phenomena, and how even seemingly familiar aspects of our physical world can harbor mysteries that resist straightforward explanations, even after nearly a century of investigation.

From the dangerous Sydney funnel-web to the common huntsman, Australia is home to its fair share of spiders. It even has a crater shaped like one.

What is it?

One stretch of the vast Western Australia wilderness is imprinted with a curious crater, which likely formed after a meteor impact hundreds of millions of years ago. Geologists think the spider-like pattern in the crater's center was created when its floor rebounded following the initial impact, NASA has said.

In the hundreds of millions of years since the initial impact, erosion has continued to carve this formation into its current, signature shape. Complete with "legs," the planetary imprint has earned its name Spider Crater.

This image shows the impact structure in its entirety, which stretches 8 by 7 miles (13 by 11 kilometers) in full, with the central "spider" piece measuring 2.5 miles (4 km).

Why is it incredible?

In this image, we can see this "spider" from space. This snapshot shows the geologic feature as captured by the OLI (Operational Land Imager) aboard the Landsat 9 satellite, an Earth-observing craft that launched back in 2021.

The satellite, a collaborative effort between NASA and the U.S. Geological Survey, is the ninth in the Landsat Earth-observing series, which goes all the way back to the launch of Landsat 1 in 1972. On a near-weekly basis, Landsat 9 delivers observations of everything from deforestation to water quality and crop growth.

The series of Landsat satellites have been a critical piece in the modern understanding of how our planet continues to change. Whether it's the repercussions of climate change or fluctuations in agriculture, observations from orbit do more than provide interesting photos of our home world; they also capture critical data.

Antarctica is a magnificent sight, and that beauty is visible all the way from space.

What is it?

Orbiting planet Earth, the European Space Agency's (ESA) Copernicus Sentinel-3 mission captured a close-up of West Antarctica.

Winter is ending in the Southern Hemisphere, meaning this is the peak of icy weather and sea ice in the Arctic.

In this image snapped by Sentinel-3, you can see a massive swath of ice which includes Elephant Island on the left-hand side. An ice-covered island off the Antarctic coast, Elephant Island floats in the Southern Ocean. It got its name both from the island's shape, which some liken to that of an elephant's head, and the fact that the island is home to a community of elephant seals.

Why is it incredible?

While a seal-inhabited island on the left floats near the Antarctic coast, across the water is a vast, frozen landscape. In just this snapshot, you can see about between 746 and 1,056 miles (1,200 to 1,700 kilometers) of the icy continent.

This image was captured on Sept. 30, 2026. In the Southern Hemisphere, that was just past the end of winter. The absolute peak for sea ice in Antarctica fell just a couple weeks before, on Sept. 14, according to the National Snow and Ice Data Center, ESA reported.

So in this one snapshot, we can see a near-maximum for sea ice in the Antarctic, spanning hundreds of miles. In observing our own planet from space, we are able to peer across vast landscapes, capturing important observational data. This is especially critical for the Antarctic as, with the progression of climate change, this sea ice continues to dwindle, adding to sea level rise among other serious consequences across the planet.

The location of Earth's geographic poles has changed several times over the past 320 million years in a process known as true polar wander, according to measurements of ancient flooding brought about by sea level changes resulting from our planet's crust shifting relative to Earth's spin axis.

Such a shift can affect climate, both on local scales and globally, as regions that were by the poles find themselves moving down to lower latitudes and vice versa. This can then affect atmospheric circulation patterns, which affect climate across the world.

The changes would have affected the environments in which life developed and evolved, from the age of the dinosaurs through to some of our oldest primate ancestors.

True polar wander is not the same as a change in the rotational axis of the Earth. Currently, Earth spins at an angle of 23.4 degrees relative to the plane of its orbit around the sun, and this rotational axis can vary periodically over tens of thousands of years as a result of the Milankovitch cycles caused by the gravitational pull of the sun and planets.

True polar wander is different. Here, the angle of Earth's spin axis does not change relative to its orbital plane. Instead, Earth's crust and mantle shift relative to that rotational axis. This is because Earth is not perfectly spherical. Instead, it is oblate, with Earth's rotation causing the equator to bulge out and the poles to slightly flatten. Because Earth is not spherical, it has multiple axes of inertia, the largest one being aligned with the rotational axis.

These axes need to be balanced to prevent Earth's rotation from becoming chaotic. However, plate tectonics and indeed the Milankovitch cycles can upset that balance of mass, for example by causing more continental crust to congregate in one hemisphere than another.

To rebalance things, Earth's crust and mantle must become decoupled from our planet's core, which stays aligned with the rotational axis. In physical terms, if there is more continental crust in one hemisphere, the crust and mantle might rotate in that direction relative to the rotational axis and the Earth's core in order to balance itself. This sees the geographical locations of the poles change, hence the name 'true polar wander'.

Currently, true polar wander takes place at a rate of 10 centimeters (4 inches) per year, but figuring out when and how fast true polar wander has occurred in the past is not without its difficulties, not least since plate tectonics can mask and even mimic the signal of true polar wander.

Previous studies relied on paleomagnetism, the study of residual magnetic traces in ancient rocks, since the orientation of those magnetic traces would have varied depending upon where that rock was located relative to Earth's magnetic field. Alas, it's not a terribly accurate means of measuring true polar wander and scientists arrived at substantially different conclusions using this technique.

Nevertheless, based on paleomagnetism, scientists had concluded that true polar wander had been negligible, or slow to proceed, in the distant past. However, new results from researchers at the Centre for Planetary Habitability at the University of Oslo in Norway, led by Mathew Domeier, have shown this not to be the case.

Domeier's team looked through the geological record to track how sea level has changed across millions of years. True polar wander would bring about an identifiable pattern in sea-level changes as the oceans reacted in response to changes in the mass distribution of the planet. The sea level changes would be equal but opposite between hemispheres — sea level rises on one side of one hemisphere would be matched by rises on the other side of the opposite hemisphere, creating a 'quadrupolar' effect.

By using statistical modeling on maps of sea level changes across intervals of 10 million years, Domeier's team identified four periods of true polar wander: in the early Jurassic period 190—200 million years ago, the late Jurassic — early Cretaceous period 140—150 million years ago, during the mid-Cretaceous 90—100 million years ago and from the Oligocene period 30 million years ago through to the Miocene 20 million years ago.

The results show that, contrary to established opinion, true polar wander can happen in bursts that are relatively fast on geological timescales, with the results showing that during the episodes of true polar wander the Earth's surface shifted by as much as 0.6 degrees per million years relative to the spin axis. This is slow by human standards, but fairly fast on geological timescales, certainly quicker than plate tectonics.

Domeier's team were also able to rule out a suspected case of true polar wander around 300 million years ago when the last great supercontinent, Pangea, migrated northwards. It turns out that Pangea's movements were entirely due to plate tectonics.

The findings were published on Oct. 1 in the journal Science.

A neon blue pool swirls amongst what look like clouds, all surrounded by a bright red stretch of land. This might look like the surface of an alien planet, but it's actually a salt flat right here on Earth, seen from space.

What is it?

Etosha National Park in northern Namibia hosts the largest salt pan, or piece of land covered with salt and other minerals, in the country.

This image of the Etosha Pan was captured on April 5 of this year by Europe's Copernicus Sentinel-2 mission, which consists of two identical satellites in the same orbit.

The Sentinel-2 pair observe and capture imagery of our planet in different wavelengths using a high-resolution multispectral imager that can see 13 different spectral bands, or ranges of wavelengths.

By looking at our planet from space, and observing it through different wavelengths and colors, we can better understand Earth's topography and how it changes over time. With this image, researchers can better understand this landmark in Namibia, a nation in southwestern Africa.

Why is it incredible?

While this image is strikingly beautiful, the Etosha Pan doesn't exactly look like this in real life. If you were standing close to the pan in the national park, it would look bright white.

While this is a real image, false color has been added, which allows scientists to separate different types of vegetation and topography.

With the false color, the vegetation surrounding the salt pan appears in shades of red, while the salt pan itself looks like a mix of bright, light and dark blues with cloudy sediment floating around.

The varied vegetation captured in this false-color image includes grassland, savannas and mopane trees, which appear bright red. These trees are not only a dominant type of vegetation in areas of this park, they also provide essential shelter and habitats for local wildlife, including elephants, giraffe and leopards.

Decades ago, Captain Kirk faced off against the Gorn on the uncharted desert planet Metron. But as we can see in new satellite imagery from NASA, that mysterious rocky world can actually be found right here on Earth in California.

What is it?

In this new image captured by the Operational Land Imager (OLI) on NASA's Landsat 9 satellite, you can see the wide variety of rock and vegetation in the area around Vasquez Rocks Natural Area County Park in southern California.

The 25-million-year-old Vasquez Rocks is a magnificent natural area with an incredible range of unique, large rocks jutting out of the ground. In this false-color image, you can see the area in shortwave-infrared and near-infrared wavelengths that show the differences in vegetation across the landscape.

And this location hides some amazing history. Not only is Vasquez Rocks home to incredible rock formations and desert vegetation, it is also where Captain Kirk fought the Gorn in Star Trek the Original Series. It's not a surprise the series chose this location for its infamous fight scene (among many other Trek scenes), as the massive, sun-bleached boulders pointing to the sky and barren landscape give it a distinctly alien feel.

Why is it incredible?

While the rocky landscape of Vasquez Rocks is firmly fixed here on Earth, it has consistently made history as the backdrop to a whole host of iconic science fiction moments.

Indeed, Star Trek is one as Vasquez Rocks has been used for filming in a whole host of Trek episodes. It was even Spock's home world of Vulcan in the films Star Trek IV: The Voyage Home and Star Trek (2009).

But beyond Star Trek, the site has been used for filming sci-fi classics like Galaxy Quest, Battlestar Galactica and Planet of the Apes in addition to a whole host of cowboy movies and more.

It turns out that right here on Earth, we can find perfectly good alien worlds.

A volcano on an Indonesian archipelago began erupting on Sept. 4, and satellites in orbit have been watching closely.

What is it?

The volcano Anak Krakatau started spitting out ash and lava on Sept. 4. On an archipelago between Sumatra and Java, the island volcano's sudden eruption grounded flights, closed schools and even stopped fishing in the area.

The volcano launched ash into the air and into the city of Jakarta and the Lampung province during a 25-hour-long eruption. But even following this eruption, Anak Krakatau remained active throughout the weekend. In fact, the volcano is still so active that it could erupt again soon.

But it wasn't just people on Earth watching the volcano erupt this past weekend. The Landsat 8 satellite, operated by NASA and the U.S. Geological Survey (USGS), spotted a white plume of volcanic gas billowing into the atmosphere all the way from space. The white plumes of gas are thought to mainly contain water vapor, carbon dioxide and sulfur dioxide, while ash and debris make up the brown clouds surrounding the plumes.

Why is it incredible?

While Anak Krakatau simmers after this most recent eruption, this event isn't a major shock, as the volcano sits in what is known as the "Ring of Fire." This "ring" (a loose term, as it's not exactly a ring) snakes about 25,000 miles (40,000 kilometers) around the Pacific Ocean and includes over 750 volcanoes, some dormant and some active.

In fact, in Indonesia alone there are 500 volcanoes, and 127 of them are active, including Anak Krakatau. And this volcano has a particularly interesting story: It emerged from the sea in 1927, rising from the caldera formed by the 1883 eruption of Krakatau (also known as Krakotoa), which was one of the most famous and destructive volcanic events in history. (Anak Krakatau means "child of Krakatau" in the Indonesian language.)

While not all geologists agree on the exact margins of the Ring of Fire, it rests on a string of tectonic plates and has existed for over 35 million years. And not only is this ring home to hundreds of volcanoes, it's also a hot spot for earthquakes.

We are a planet-based species: With a few notable (astronaut) exceptions, everyone who has ever lived remained glued to our spinning Earth, which now houses 8.3 billion people.

That's the gravity of the situation. But we're also a world of floods, typhoons, earthquakes, heat and cold calamities, volcanic eruptions and even encounters with sun-caused auroras and bruises from incoming asteroids.

It's quite a world worth watching — and for decades that's what spacecraft have been doing. But what do they view and who's on the other end of the space-based telescopes capturing our daily doings, faults and all, down here on terra firma?

Privacy, security and trust

Recently, the Organization for Economic Co-operation and Development (OECD), a group based in Paris, published a report on the expanding access to satellite Earth-observation data, spotlighting what it means for privacy, security and trust.

"Advances in optical systems, photonics, cloud computing and artificial intelligence [AI] have democratized both the quality and accessibility of satellite data. However, this convergence of technologies also carries risks, including for national security and privacy," states the report, which was authored by the OECD's Marit Undseth and Claire Jolly.

Broadening access to advanced satellite data also creates new challenges, states the report, such as one of the key characteristics of Earth observation — its dual-use nature. "The same satellites used to track illegal fishing can often also detect military troop movements," the authors write.

New concerns

The OCED report notes that Earth-observation data and the technological convergence with artificial intelligence raise new concerns about national security, privacy and the ethical use of these data.

In fact, the report points to the growing hazard of fake or incorrectly used satellite imagery. "As part of the growing trend of digital disinformation, the trust in satellite data can be eroded by fake, misinterpreted or intentionally misrepresented imagery," it states.

Space.com asked leading remote-sensing specialists what's being done, what's being learned and what we should worry about.

Sovereignty and cost efficiency

Viktor Stoyanov is the chief operating officer of Smart Solutions at Space42, where he oversees the business unit's operational and financial performance.

Space42 is a United Arab Emirates-based space technology company that integrates satellite communications, geospatial analytics and AI capabilities. The group runs the Foresight Earth Observation constellation of synthetic aperture radar (SAR) satellites.

Space.com asked Stoyanov about the growing international use of remote-sensing data.

"Governments increasingly expect Earth-observation systems to deliver both sovereignty and cost efficiency, two goals that were long seen as mutually exclusive, as sovereignty typically meant heavy in-country investment in duplicative research and development and capital infrastructure," he responded.

Dual use

Stoyanov said Space42's focus is to combine those two outcomes.

"We believe that can only be achieved through international cooperation. Our Foresight constellation reflects this model, as the first sovereign dual-use synthetic aperture radar constellation in the region," Stoyanov said.

The satellites were manufactured in partnership with ICEYE in Finland, with critical integration and testing completed in the organization's facility in Abu Dhabi.

"The Abu Dhabi facility was built in cost-cautious and scalable manner, so that it can satisfy current sovereignty requirements commensurate with the constellation size, with the ability to expand the facility and meet demand of future programs," Stoyanov said.

Through cloud, dust and darkness

What new in-orbit technologies are being applied to Earth observation?

"The biggest shift in recent years has been the move from few, large, general-purpose platforms to constellations of small, specialized satellites and synthetic aperture radar," said Stoyanov.

"SAR satellites image through cloud, dust and darkness, which matters enormously for our region and for any customer who needs consistency regardless of timing and weather," he added.

Looking ahead, Stoyanov said that the short lifespan of satellites in low Earth orbit is an opportunity to ensure that each replenishment cycle becomes an upgrade cycle.

"As we plan to maintain and expand our fleet, we will continuously seek to deploy technical improvements across various performance metrics of the system — resolution, latency, satellite life, for example," said Stoyanov.

Artificial intelligence

A SAR constellation generates far more imagery than analysts can review manually within the allocated time, Stoyanov said. So the value lies in what can be extracted from it, not in the pixels themselves.

AI is therefore becoming increasingly important as a sorting tool for remote-sensing data, Stoyanov said. It is now the only practical way to work, for three reasons: volume, speed and accuracy.

Customers responding to a flood, a maritime incident or a supply-chain disruption need an answer in minutes, not a report next week — "decision-grade intelligence within minutes," explained Stoyanov.

On the topic of accuracy, while trained analysts are excellent at interpretation and large-object classification — like buildings and sea vessels — there are changes that the eye can easily miss. "Algorithms comparing each new pass against the historical baseline — they catch those consistently, without fatigue," said Stoyanov.

Hybrid model

Francis Doumet is the CEO and co-founder of Metaspectral, a company based in Vancouver, British Columbia, that builds AI technology to rapidly analyze hyperspectral imagery.

Doumet views collaboration between different national space agencies as "extensive and, somewhat uniquely, very open." Missions are frequently carried out through "shared funding, instruments, expertise and ground infrastructure," he said, with the resulting scientific data made available internationally.

Commercial imagery is less openly distributed because it is commercially licensed and may have security implications, Doumet said, but it is increasingly enabling international cooperation in the defense sector.

For example, the U.S. Space Force's Tactical Surveillance, Reconnaissance and Tracking (TacSRT) program combines commercial satellite imagery and analytics from American companies and allied nations to rapidly respond to operational requests, Doumet said.

"This has shaped the Earth-observation sector into a hybrid model," said Doumet. Governments and allies share requirements and intelligence, he explained, while commercial operators supply imagery and analytics "at a speed and scale that would be difficult or impossible for a single nation to produce alone."

Hyperspectral sensors

The improvement in the spatial resolution of hyperspectral sensors is an important advance in Earth observation, Doumet pointed out.

Better sensors, high-speed compression and improved communications, such as optical links, are now narrowing a "resolution gap." Onboard AI is equally transformative, he added.

"Satellites can analyze imagery in real time, identify relevant signatures and transmit alerts or compact intelligence products instead of waiting to download an entire hyperspectral data cube," Doumet explained.

Spectral fingerprints

Angie Crews is a principal research associate with the University of Colorado, Boulder's Center for National Security Initiatives.

"There has been a tremendous growth in the commercial remote-sensing industry," Crews told Space.com, noting that this field had previously been government-based. "It's now possible for these commercial companies to deploy entire constellations of Earth-observing satellites, which fundamentally changes the architecture in place."

Crews pointed to the hyperspectral nature of Earth remote sensing — taking the "spectral fingerprints" of what's occurring on Earth.

"It's impressive how the industry is moving forward with some of these capabilities," she said.

Balancing act

"There are some tremendous benefits as well as some things that we need to think about" when it comes to the new direction that Earth observation is taking, Crews said. Remote-sensing data can be inherently dual use, she added.

"Overall, I think we're seeing some enormous benefits from our increasingly capable commercial remote-sensing systems. But it does raise some security and governance questions," said Crews.

It's a balancing act to manage, according to Crews. How best to secure the information for national security purposes versus not putting the squeeze on innovation exhibited by the private Earth-observation firms?

Meaningful information

Shifting to her teaching role at the University of Colorado, Boulder, Crews told Space.com that one of the things that's especially important is to train students in the remote-sensing field to think beyond any single sensor or dataset.

"The next generation needs to understand how different sensing technologies work and also how to work with very large datasets and extract meaningful information using AI and machine learning," Crews said.

"We also need to train the students on critical thinking and ensure they are aware of the limitations of AI. The underlying physics need to be understood and the results need to be validated so that the students use and interpret the results appropriately," she concluded.