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A Revolution is Coming in Satellite Imagery: Why 30cm Satellites are Set to Transform the Industry

The world today finds itself more divided than ever, with an unstable geopolitical landscape and significant tension between major global powers. As a result, governments are seeking a continuous flow of information about their territories, those of their allies, and those of their enemies, in order to stay proactive and fully aware. Businesses are also looking to enable full situational awareness over large areas for a wide variety of use cases. The best way to achieve these is through leveraging the emerging technology of 30cm satellite imagery.

With the current (limited) satellites that are in orbit, you can observe a given location 2-3 times a day with 30-50cm imagery as long as there is no cloud coverage. This is useful, but it’s not enough for many advanced use cases. If users could see this data every couple of minutes, it would blow open the industry and catalyze a plethora of new commercial use cases. That’s where 30cm satellites come in.

The Emergence of 30cm Satellite Imagery

The ecosystem is seeing established operators launching next-generation 30cm satellites at a staggering rate, and this is augmented by newer players who are scaling up from their low-resolution satellites to take advantage of this new technology. It feels like every week we see a new startup aiming to disrupt the market with even higher-resolution data.

This combination of fleet upgrades from incumbent operators and new satellites from emerging players will result in nearly 10x the number of very high-resolution satellites in orbit by the end of the decade (forecast to be more than 100). Most of these future satellites will be small and with limited imaging capacity, but the sheer volume will push the industry to a place where there are much more rapid revisits.

Let’s explore some of the current and planned 30cm satellites from both the established incumbents and the emerging players in the space:

who provides 30cm satellite imagery

 

  • Airbus has two of their satellites from the Pléiades Neo constellation that are operational (from 2021 and 2022 respectively) and these are delivering unprecedented visual clarity. Unfortunately, the last two satellites didn’t make it to orbit as planned in December 2022 as the launch rocket crashed, and as such, it will take the company a few years to get those back into orbit.
  • Maxar Technologies was one of the first companies to offer commercial 30cm satellite data with their WorldView-3 and WorldView-4 satellites. Unfortunately, WorldView 4 suffered a hardware failure back in 2021 and is currently not operational. However, the company is about to launch a new constellation of 6 satellites called WorldView Legion and these are set to offer 29cm spatial resolution and a 15 times per day revisit rate.
  • Imagesat International is an Israeli company that established itself as a key player with their EROS NG constellation which has 3 very high-resolution satellites in orbit and one more planned for 2026.
  • SI Imaging Services is a Korean company that plans to launch 3 new 30cm satellites in 2024, namely Kompsat 7 & 7a and SpaceyEye-T.
  • Planet is an emerging company that expects to begin launching its Pelican satellites in 2023. This constellation consists of 32 spacecraft and it will enable a revisit rate of 30 times.
  • Satellogic is an Argentinian operation that plans to launch a constellation of 30cm satellites with a 40 times a day revisit rate. We’re still awaiting further details on what this might look like – but the industry is excited about this potential.
  • China Siwei is another emerging company on the rise with their SuperView Neo 1 and 2 satellite constellation. The company plans to expand this by building 28 RS commercial satellites before 2025 with 16 high-resolution (0.2-0.3m resolution) optical satellites, 4 wide-width (0.7m resolution + 100km swath width) optical satellites, and 8 SAR (0.5m resolution) satellites to have global coverage with high resolution, wide-width, sensor-rich, and fast receiving technology.
  • Albedo was granted a license to collect 10cm commercial panchromatic satellite imagery in July 2020 from NOAA and they will start launching their first satellite in 2024. This is to be followed by plans to complete the constellation of 24 satellites in 2027.

The amount of development in the space is staggering and so it’s clear to see that the industry as we know it is set for major disruptions as this technology grows in scale and influence.

Why is 30cm Data Important?

30cm satellite imagery represents a significant leap in image clarity and detail when we compare it to 50-70cm, not to mention lower resolution data. The higher resolution and image clarity afforded to us by this new technology will allow users to identify objects and features on the ground with much greater accuracy which then opens up a whole range of new use cases.

For example, in the world of construction monitoring or industrial inspections, 30cm data means that companies can gather the same quality of data that they used to rely on drones or airplanes for, but using satellites instead. This makes a big difference in terms of cost when you’re mapping an area that is over 20-30km2  because it’s prohibitively expensive to use a drone or an airplane to capture those images and provide photogrammetry processing of the data.

Also, when the revisit rate for a given area of interest is every hour or even several times within an hour, this makes it possible to unlock new commercial use cases where rapid change detection is needed. Examples here include port management, traffic monitoring, and the tracking of construction progress.

Source: Satellogic

30cm data is a force multiplier for the industry and if used effectively, can have a dramatic impact on how satellite imagery is captured, processed, and used more broadly.

What are the Challenges?

Of course, there is no such thing as a free lunch, and there are a number of challenges that come with 30cm satellite imagery that must be navigated in order to leverage its capabilities:

  • Business Processes that are Resistant to Change. Most people don’t realize that 30cm resolution, potentially enhanced with super-resolution AI algorithms to a readability of 15cm is sufficient to address 90% of their needs – and solve most of the challenges for many industrial use cases. Until this is more widely understood, the status quo bias is going to slow progress as users stick with what they know. It’s going to take a lot of education and awareness to break those habits and usher in a new era. On the other side of the coin, there is also a cohort of users that will need to be convinced that 30cm is good enough and that they don’t need 1mm resolution to get the job done.
  • Data Storage and Processing. 30cm satellite data brings with it a vast amount of information that needs to be stored and processed. This can put strain on existing storage infrastructure and may require additional investments into cloud-based storage and other processing solutions that can handle the sheer volume of data involved.
  • Bandwidth and Transmission. Transmitting high-resolution satellite data from space to Earth requires substantial bandwidth. As the demand for 30cm satellite imagery increases, the availability of this bandwidth may become limited, resulting in slower data transmission and reduced real-time access to imagery. This can then hinder the effectiveness of certain commercial applications.
  • Cost of Access. The costs of accessing this imagery can be prohibitive for many organizations. Satellite imagery providers must invest heavily in advanced technology and infrastructure which then gets passed on to the end user. Consequently, some organizations are likely to opt for lower-resolution alternatives due to budget constraints.
  • Integration with Existing Systems. Integrating 30cm satellite data with existing systems and processes may pose significant challenges for organizations, particularly those that have routinely relied on lower-resolution data in the past. This integration may require updates to software and hardware infrastructure as well as retraining staff to work with the new data.

None of these challenges are insurmountable, but they are obstacles to be overcome if 30cm satellite imagery is to deliver on its promise. We’re excited to see how this is going to develop as more players enter the space and we’re hopeful that it will act as an accelerator for the industry as a whole – bringing more awareness and more practical applications into this domain.

 


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Improving Tsunami Safety with Remote Sensing Satellites

Technological advances in satellite imaging are making it possible to increasingly understand the impact of natural disasters. This is mainly due to multi-temporal satellite imagery, which is a powerful tool for disaster management and risk reduction. Multi-temporal satellite imagery combines images taken at different times, to create a more detailed picture of an area. Such images can provide valuable information on the effects of disasters such as floods, storms, earthquakes and landslides. Not every country is able to effectively deal with natural disasters, which is why the International Charter on Space and Major Disasters was established. It is a non-commercial initiative to collect and provide remote sensing data on natural disasters and catastrophes anywhere in the world to improve disaster management processes. These data are provided to organizations involved in mitigating their effects and helping those affected. The imagery is currently acquired from satellites belonging to seventeen member countries, partners involved in the Charter project, and other data providers.

A Finnish company belonging to the initiative, ICEYE, is developing a constellation of lightweight SAR satellites as part of the project, which enables monitoring, mapping and analysis of post-disaster changes detected on the Earth’s surface. The technology has been used for, among other things: assessing damage, analyzing infrastructure before and after disasters, the effects of floods, volcanic eruptions and landslides, and measuring oil spills.

Another example of satellites supporting the initiative is Planet’s PlanetScope constellation, a fleet of miniature satellites called CubeSats, which collects weekly or daily images of the entire planet, and produces about 1,700 images each month. The captured data is used to monitor the spread of wildfires, among other things. Thanks to PlanetScope’s huge data sets, 3D reconstructions or digital surface models of any area can be created.

A detailed list of all satellites providing data under the International Charter on Space and Major Disasters appears below.

Many natural disasters are caused by tsunamis. A United Nations (UN) report estimates that each year some 60,000 people and assets worth $4 billion are exposed to the threat of a tsunami. In addition, more than 700 million people are currently living in coastal areas at risk from extreme events such as tsunamis and storm surges. This number is likely to increase as coastal populations grow. The average tsunami wave is less than 10 feet in height, but some exceed 100 feet. It can produce extremely strong currents, quickly flooding the land and causing great destruction. These currents and floods can last for days. Since the beginning of the 20th century, 34 tsunamis have been recorded, collectively causing more than 500 deaths in the United States alone, and more than $1.7 billion in damage to US territories and coastal areas. The dangers posed by tsunamis emphasize the need for early warning systems – the longer the lead time, the more opportunities to evacuate and secure critical infrastructure.

Overview of Tsunami early warning systems

Currently, there are three technologies that can provide real-time early warnings of tsunamis. One of these is DART, a buoy-based technology. DART stations have many advantages, but they primarily serve as local and remote tsunami detection systems. In addition, they are portable, so the location of the arrays can be easily changed. Another advantage is the unified sensors, making it possible to share data with other countries in real time. Importantly, the buoys represent a distributed system, so one failure will not affect other DARTs.

Another technology is wired observatories, which are sensors located on underwater cable systems. The Joint Task Force on Monitoring Science and Reliable Telecommunications (SMART) Subsea Cables, a United Nations initiative, aims to equip new commercial undersea telecommunication cables with simple sensors that measure pressure, acceleration and temperature. The sensors can be added to fiber-optic cable signal boosters – watertight cylinders filled with equipment to amplify signals every 50 kilometers or so. With cabling that powers the sensors and transmits data, scientists can collect information about the seafloor on an unprecedented scale – and identify potential tsunamis much faster.

The image below depicts a surface buoy with a global positioning system (GPS) antenna docked about 20 kilometers off the coast to monitor sea level changes using real-time kinematic (RTK) GPS technology with a ground station. The buoys serve as a wave gauge to enable early detection of tsunamis. The real time GPS data is processed by PARI (Ports and Airports Research Institute), and then sent to the JMA responsible for tsunami monitoring and warning.

Detecting tsunami with DART buoys

Tsunami early warning using Deep-ocean Assessment and Reporting of Tsunami, Source: NOAA

What are the limitations of these systems?

Unfortunately, despite their many advantages, these systems have a number of disadvantages, depending on the technology. In the case of DART, these include high emergency maintenance costs due to vessel-related expenses, and buoy locations must avoid strong ocean currents and seamounts. A surface buoy with a GPS antenna, on the other hand, requires a location close to the coast in order to communicate with GPS base stations. In addition, the sensors are non-standard, which makes the measurements incompatible with DART sensors and wired observatories.

However, regardless of the technology, early detection systems generally have two major limitations: late tsunami warnings and false alarms. A tsunami warning system is regarded as efficient if it provides enough time – referred to as “golden time” – for people to save themselves. The longer the golden time, the earlier the warning. Unfortunately, some countries still receive insufficient warning. “Tsunami warning systems are useless in most of the countries like Indonesia and Papua New Guinea, because the lead time is too short,” McCue told Reuters. “Far better to educate people to make for high ground immediately after they feel shaking that lasts more than about 30 seconds,” McCue said. The Pacific Ocean early warning system’s false alarm rate is estimated at 75 percent. “It’s definitely one of our biggest challenges,” said Charles McCreery, director of the Pacific Tsunami Warning System in Honolulu, which sends seismic data and tsunami bulletins to 26 nations around the Pacific. When a warning is issued, sirens sound on the beach, and urgent messages are displayed on television, and broadcast on the radio. Evacuation maps direct people to higher ground, but the tsunami often does not occur.


The Role of Remote Sensing Satellites in Tsunami Detection

How remote sensing satellites can detect early signs of tsunamis

How can orbiting satellites detect tsunamis at an early stage? Most tsunamis are caused by underwater earthquakes or volcanic eruptions, many of which produce atmospheric effects that satellites can easily detect.

An example is the recent eruption of the HTHH volcano in Vietnam, which ejected a volcanic plume that reached into the mesosphere and spread ash over a distance of several hundred kilometers. The satellite-detected atmospheric waves (Lamb) from this event spread around the world. The conjunctions of these atmospheric waves with ocean basins caused sea level fluctuations observed well before the tsunamis. For example, a tide gauge on Lord Howe Island, located about 3,000 kilometers southwest of the eruption site, recorded an initial sea level fluctuation of 0.1 meters about 2.5 hours after the eruption. Much larger waves of up to one meter followed, and the tsunami, moving at about 200 meters per second, arrived after another two hours.  Atmospheric acoustic waves travel faster than tsunamis. Waves generated by extreme events, such as volcanic eruptions and tsunamis, penetrate the troposphere and stratosphere and reach as far as the ionosphere. Consequently, the upper layers of the atmosphere are ideal for detecting anomalies associated with these extreme events, since the amplitudes of atmospheric perturbations increase dramatically with altitude. Satellite technologies must be used to detect these atmospheric perturbations, providing high-resolution, wide-area information in the fastest possible time.

Satellites also provide early tsunami detection by monitoring the Earth’s crust for subtle changes in pressure, temperature and other factors, which may indicate an impending seismic event. In this way, a tsunami can be detected before it even occurs. In addition to detecting seismic activity, navigation satellites can also be used to provide data on ocean currents to predict the path and intensity of an approaching tsunami.

 

The advantages of using satellites for tsunami detection

Evacuation time is critical to minimize tsunami mortality rates. The sooner the threat is communicated, the greater the chance to minimize loss of life. A NASA Earth Applied Sciences project with NOAA has developed new technology for their tsunami early warning system to potentially predict tsunamis within just five minutes of an earthquake, which could significantly affect the number of fatalities. “The problem we’re trying to solve is that it’s difficult to produce a tsunami forecast within the first 20 minutes that says when and where a tsunami might occur, or how big the waves might be,” said Diego Melgar from University of Oregon, who leads the project’s research team in the NASA Disasters Program area. “That’s where GNSS [Global Navigation Satellite System] comes in – it can measure tectonic displacement within the first minute, determine the magnitude of the earthquake, and trigger an alert to the region within those critical first five minutes.” Melgar’s team also uses real-time data from Global Differential Global Positioning System. This helps to provide more accurate and immediate estimates of tsunami size and direction. “Incorporating this data from NASA means we can enable emergency response managers to provide actionable tsunami impact information to their communities sooner, giving local residents as much time as possible to take life and property saving actions,” Angove said.

Examples

An earthquake measuring 9.0 on the Richter scale, the strongest ever recorded in Japan and the fourth strongest since 1900, occurred in the Pacific Ocean near the Tohoku region of Japan. The earthquake and subsequent tsunami caused massive damage along the Tohoku-Kanto Pacific coast. The Japan Aerospace Exploration Agency (JAXA), together with Sentinel Asia and the International Charter on Space and Major Disasters, planned satellite observations of areas immediately after the disaster. The images acquired were used to assess the overall extent of damage, analyze tsunami-inundated areas, landslides, damage to structures, road accessibility and shelter locations. In addition, thanks to the satellite images, SAR rescue workers had knowledge of the availability of key facilities and rescue routes, which contributed to a more efficient evacuation. The use of satellites has proven the unrivaled speed of relief efforts during mass disasters.

Post-tsunami effect with satellite imagery

Japan’s changed landscape from space, Source:
https://www.esa.int/About_Us/ESRIN/Mapping_Japan_s_changed_landscape_from_space

Satellites were also helpful in the December 2004 Indian Ocean tsunami. About two hours after the initial earthquake, Jason, the joint U.S.-French satellite took measurements of sea surface elevation and waves to study ocean circulation and climate. The maximum sea surface elevation of 50 cm was measured about 1,200 km south of Sri Lanka, where the leading wave length was about 800 km, followed by another with a crest of 40 cm. Near the northern end of the Gulf, two waves of 40 cm and 20 damaged the coast of Myanmar. Topex/Poseidon, simultaneously orbiting about 150 kilometers west of Jason, made similar observations of tsunami waves, confirming that the measurements were consistent. “The observations made by Jason and Topex/Poseidon are unique and of tremendous value for testing and improving tsunami computer models and developing future tsunami early warning systems,” said JPL’s Dr. Lee-Lueng Fu, Jason and Topex/Poseidon project scientist.

Conclusion

Remote sensing satellites provide great support in early tsunami warning. Current technologies, while not yet perfect, make it possible to predict a natural disaster before high waves are even captured at sea. This provides more time for evacuation, minimizing loss of life and damage to infrastructure.

Fast availability of data enables more efficient management of emergencies, where every minute counts. However, new solutions usually present challenges. Satellite imagery is expensive, and the cost of acquiring and processing the data can be prohibitive for some researchers. The second issue is the need for international cooperation. For example, the cooperation between different organizations during the 2011 floods in Japan enabled more effective action, which is crucial when dealing with natural disasters. Remote sensing satellites have enormous potential for early detection of tsunamis, and to reduce the damage and loss of life these disasters cause.

 


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