Monday, February 24, 2025

ECMWF – Europe’s leading centre for weather prediction makes forecast data from AI model available to all





ECMWF

Artificial Intelligence Forecasting System (AIFS) @ECMWF 2025 

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ECMWF Artificial Intelligence Forecasting System (AIFS)

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Credit: ECMWF






A newly operational model, known as the Artificial Intelligence Forecasting System (AIFS), has been launched by the European Centre for Medium-Range Weather Forecasts (ECMWF), an intergovernmental centre and leader in numerical weather prediction. For many measures including tropical cyclone tracks, the AIFS outperforms state-of-the-art physics-based models, with gains of up to 20%. This high accuracy model complements the portfolio of ECMWF's physics-based models, advancing numerical weather prediction, and leverages the opportunities made available by machine learning (ML) and artificial intelligence (AI), such as increased speed and a reduction of approximately 1,000 times in energy use for making a forecast.

Amongst the available AI models, the AIFS provides the greatest granularity sought by its user community. On top of vital fields for users, like wind and temperature, and details on precipitation types from snow to rain, ECMWF says this new service is the first fully operational weather prediction open model using machine learning with the widest range of parameters. The AIFS has been designed holistically with all users in mind. For example, in the renewable energy sector it will help with predictions such as surface solar radiation levels or wind speeds at turbine levels so that operations can be maximised.

The availability of this operational machine learning model in conjunction with ECMWF’s other services is set to positively impact how national weather services in ECMWF’s 35 Member and Co-operating States and beyond will be able to make their predictions. Similarly, it potentially could help industries where forecasts for the medium range (days to weeks) can affect decision making, such as the energy sector for pricing forecasts, insurance, security and shipping sectors.

Dr Florence Rabier, Director-General of ECMWF, comments:

“This milestone will transform weather science and predictions. It showcases our dedication to delivering a machine learning forecasting model that pushes the boundaries of efficiency and accuracy, and it underscores our commitment to harnessing the power of machine learning for the weather forecasting community.

“At ECMWF, we have some of the world’s leading computing models for weather prediction, the world’s largest catalogue of meteorological data sets on which machine learning models are trained, and a team of experts from scientists to engineers who are driving the science and technology forward. It is credit to their hard work that we have achieved this today, making the AIFS operational producing the widest range of parameters using machine learning available to date. But it does not stop here as the roadmap for improvements of the models we have is a top priority. It is not only us who are innovating as it is important to remember that with ECMWF, 35 nations are working together to advance weather science to improve global predictions. This is to help national meteorological agencies in their work to contribute to a safe and thriving society. This will also trigger new services and products to benefit those who do not have access to meteorological capabilities, for example in developing countries.”

How does the model work?

Florence continues explaining how the model works: “Imagine 800 million observations processed on a daily basis, from more than 100 different satellite data and other streams including planes, boats, sea buoys and many other Earth-based measurement stations. These observations contain information about, for example, the Earth’s atmosphere, pressure, moisture, temperature, wind. Scientists next select around 60 million quality-controlled observations out of those daily observations which are then ingested into our Integrated Forecasting System (IFS). These then form what we call the initial conditions, the starting point of the next stage to deliver forecasts. Our set of initial conditions data as well as our historical meteorological dataset archive are widely used the world over, from big tech companies to small starts-ups to help them innovate.

“Every 6 hours, these initial conditions feed into the newly operational Artificial Intelligence Forecasting System (AIFS), where the machine learning model, using special mathematical rules, assesses how the current meteorological conditions will influence the entire weather system on the Earth for the coming days. Today, we are launching the first fully operational model of this kind based on machine learning.”

This model joins a series of other ECMWF services, one of which is the delivery of global weather forecasts by the Integrated Forecasting System (IFS), which not only provides the ability to gather the initial conditions but also produces forecasts at a world-leading resolution of 9 km over the globe. It uses physics-based capabilities to reach this, integrating the laws of physics in its computer code.

The first operational version is called AIFS-single. It runs one single forecast at a time, known as a deterministic forecast. However, ECMWF is pushing this model to create a collection of 50 different forecasts with slight variations at any given time to provide the full range of possible scenarios, which is known as ensemble modelling, a technique developed and implemented by ECMWF more than thirty years ago.

ECMWF says its roadmap for its Artificial Intelligence Forecasting System is clear, and the launch of this AIFS-single 1.0 model as an operational service is only the first step. The next step will be making ensemble forecasts available following the same path. The potential to hybridise the two approaches, data driven and physics-based, will also be a field of research over the coming years to explore this potential further.

Dr Florian Pappenberger, Director of Forecasts and Services at ECMWF, adds:

"This is a huge endeavour that ensures the models are running in a stable and reliable way. At the moment, the resolution of the AIFS is less than that of our model (IFS), which achieves 9 km resolution using a physics-based approach. We see the AIFS and IFS as complementary, and part of providing a range of products to our user community, who decide what best suits their needs.”

ECMWF's weather predictions are focused on the medium range (3 days to 15 days), sub-seasonal, and seasonal (up to a year ahead). These are critical to help national weather services plan for extreme events – the earlier it is known that an event is likely to take place, the easier it is for governments and relevant agencies to better prepare for those events.

Florian concludes:

"ECMWF's AIFS was an experimental model for some months whilst we enhanced its capabilities by interacting with our Member States and users to refine it. We have brought it to an operational state for the benefit first and foremost of our Member and Co-operating States as well as many industry sectors, such as energy. Making such a system operational means that it is openly available and has 24/7 support for our meteorological community. As always, we have to ramp up this service to full maturity, and we look forward to engaging directly with our users to ensure all needs are covered where possible."

Whilst ECMWF concentrates on predictions from days to months ahead over the whole globe, the national meteorological services also focus on forecasts that are nationally and regionally relevant, and they oversee issuing weather warnings for their country in collaboration with other agencies. This year marks 50 years since the creation of ECMWF, and the complementarity between ECMWF and the meteorological centres across its Member States is essential to have trust, excellence and resilience in services and advance science for the benefit of everyone.

ENDS

For further information please contact:

All enquiries should be directed in first instance to: pressoffice@ecmwf.int

In case you need urgent help please reach out to Lorna Campbell 0044 (0)7836 625999

 

Note to editors

About ECMWF

The European Centre for Medium-Range Weather Forecasts (ECMWF) is a world leader in numerical weather predictions providing high-quality data for weather forecasts and environmental monitoring. As an intergovernmental organisation, we collaborate internationally to serve our members and the wider community with global weather predictions, data and training activities that are critical to contribute to safe and thriving societies.  

The success of our activities depends on the funding and partnerships of our 35 Member and Co-operating States who provide the support and direction of our work. Our talented staff together with the international scientific community, and our powerful supercomputing capabilities, are at the core of a 24/7 research and operational centre with a focus on medium- and long-range predictions. We also hold one of the largest meteorological data archives in the world, including ERA5 funded by the European Union Copernicus programme. 

Our mission: Deliver global numerical weather predictions focusing on the medium-range and monitoring of the Earth system to and with our Member States. 

Our vision: World-leading monitoring and predictions of the Earth System enabled by cutting-edge physical, computational and data science, resulting from a close collaboration between ECMWF and the members of the European Meteorological Infrastructure, will contribute to a safe and thriving society.

ECMWF has established a strong partnership with the European Union and has been entrusted with the implementation and operation of the Climate Change and Atmosphere Monitoring Services of the Copernicus Programme, as well as being an important contributor to the Copernicus Emergency Management Service and to the Destination Earth initiative. Other areas of work include high-performance computing and the development of digital tools that enable ECMWF’s provision of data and products covering weather, climate, air quality, fire and flood prediction and monitoring.  

ECMWF is a multi-site organisation, with its headquarters in Reading, UK, a data centre in Bologna, Italy, and a large presence in Bonn, Germany, as a central location for our EU-related activities. ECMWF is internationally recognised as a voice of expertise in numerical weather predictions for forecasts and climate science. 

 

www.ecmwf.int

About Copernicus www.copernicus.eu

About Destination Earth https://destine.ecmwf.int/

More about the AIFS operational model can be found here

SPACE/COSMOS

 

Laser-powered device tested on Earth could help us detect microbial fossils on Mars



Scientists successfully identify microbe fossils in terrestrial rocks like those found on Mars, opening up the possibility of searching for fossils on the Red Planet


Frontiers




The first life on Earth formed four billion years ago, as microbes living in pools and seas: what if the same thing happened on Mars? If it did, how would we prove it? Scientists hoping to identify fossil evidence of ancient Martian microbial life have now found a way to test their hypothesis, proving they can detect the fossils of microbes in gypsum samples that are a close analogy to sulfate rocks on Mars.  

“Our findings provide a methodological framework for detecting biosignatures in Martian sulfate minerals, potentially guiding future Mars exploration missions,” said Youcef Sellam, PhD student at the Physics Institute, University of Bern, and first author of the article in Frontiers in Astronomy and Space Sciences. “Our laser ablation ionization mass spectrometer, a spaceflight-prototype instrument, can effectively detect biosignatures in sulfate minerals. This technology could be integrated into future Mars rovers or landers for in-situ analysis.” 

Water, water everywhere 

Billions of years ago, the water on Mars dried up. Gypsum and other sulfates formed when pools evaporated, leaving behind minerals that precipitated out of the water – and potentially fossilizing any organic life left behind. This means that if microbes such as bacteria lived there, traces of their presence could be preserved as fossils.  

“Gypsum has been widely detected on the Martian surface and is known for its exceptional fossilization potential,” explained Sellam. “It forms rapidly, trapping microorganisms before decomposition occurs, and preserves biological structures and chemical biosignatures.” 

But to identify these microbial fossils we first need to prove we can identify similar fossils in places where we know such microbes existed — such as Mediterranean gypsum formations that developed during the Messinian Salinity Crisis.  

“The Messinian Salinity Crisis occurred when the Mediterranean Sea was cut off from the Atlantic Ocean,” said Sellam. “This led to rapid evaporation, causing the sea to become hypersaline and depositing thick layers of evaporites, including gypsum. These deposits provide an excellent terrestrial analog for Martian sulfate deposits.” 

The scientists selected an instrument that could be used on a spaceflight: a miniature laser-powered mass spectrometer, which can analyze the chemical composition of a sample in detail as fine as a micrometer. They sampled gypsum from Sidi Boutbal quarry, Algeria, and analyzed it using the mass spectrometer and an optical microscope, guided by criteria which can help distinguish between potential microbial fossils and natural rock formations. These include morphology which is irregular, sinuous, and potentially hollow, as well as the presence of chemical elements necessary for life, carbonaceous material, and minerals like clay or dolomite which can be influenced by the presence of bacteria. 

Life on Mars? 

The scientists identified long, twisting fossil filaments within the Algerian gypsum, which have previously been interpreted as benthic algae or cyanobacteria, and are now thought to be sulfur-oxidizing bacteria like Beggiatoa. These were embedded in gypsum, and surrounded by dolomite, clay minerals, and pyrite. The presence of these minerals signals the presence of organic life, because prokaryotes — cells without a nucleus — supply elements which clay needs to form. They also facilitate dolomite formation in an acidic environment like Mars by increasing the alkalinity around them and concentrating ions in their cell envelopes. For dolomite to form within gypsum without the presence of organic life, high temperatures and pressures would be needed that would have dehydrated the gypsum, and which aren’t consistent with our knowledge of the Martian environment. 

If mass spectrometers identify the presence of clay and dolomite in Martian gypsum in addition to other biosignatures, this could be a key signal of fossilized life, which could be reinforced by analyzing other chemical minerals present and by looking for similar organically formed filaments.  

“While our findings strongly support the biogenicity of the fossil filament in gypsum, distinguishing true biosignatures from abiotic mineral formations remains a challenge,” cautioned Sellam. “An additional independent detection method would improve the confidence in life detection. Additionally, Mars has unique environmental conditions, which could affect biosignature preservation over geological periods. Further studies are needed.” 

“This research is the first astrobiology study to involve Algeria and the first to use an Algerian terrestrial analog for Mars,” said Sellam. “As an Algerian researcher, I am incredibly proud to have introduced my country to the field of planetary science.  

“This work is also dedicated to the memory of my father, who was a great source of strength and encouragement. Losing him during this research was one of the most difficult moments of my life. I hope that he is proud of what I have achieved.” 


Gulf of Mars: Rover finds evidence of ‘vacation-style’ beaches on Mars



Penn State





UNIVERSITY PARK, Pa. — Mars may have once been home to sun-soaked, sandy beaches with gentle, lapping waves according to a new study published today (Feb. 24) in the Proceedings of the National Academy of Sciences (PNAS).

An international team of scientists, including Penn State researchers, used data from the Zhurong Mars rover to identify hidden layers of rock under the planet’s surface that strongly suggest the presence of an ancient northern ocean. The new research offers the clearest evidence yet that the planet once contained a significant body of water and a more habitable environment for life, according to Benjamin Cardenas, assistant professor of geology at Penn State and co-author on the study.

“We’re finding places on Mars that used to look like ancient beaches and ancient river deltas,” Cardenas said. “We found evidence for wind, waves, no shortage of sand — a proper, vacation-style beach.”

The Zhurong rover landed on Mars in 2021 in an area known as Utopia Planitia and sent back data on the geology of its surroundings in search of signs of ancient water or ice. Unlike other rovers, it came equipped with rover-penetrating radar, which allowed it to explore the planet’s subsurface, using both low and high-frequency radar to penetrate the Martian soil and identify buried rock formations.

By studying the underground sedimentary deposits, scientists are able to piece together a more complete picture of the red planet’s history, Cardenas explained. When the team reviewed radar data, it revealed a similar layered structure to beaches on Earth: formations called “foreshore deposits” that slope downwards towards oceans and form when sediments are carried by tides and waves into a large body of water.

“This stood out to us immediately because it suggests there were waves, which means there was a dynamic interface of air and water,” Cardenas said. “When we look back at where the earliest life on Earth developed, it was in the interaction between oceans and land, so this is painting a picture of ancient habitable environments, capable of harboring conditions friendly toward microbial life.”

When the team compared the Martian data with radar images of coastal deposits on Earth, they found striking similarities, Cardenas said. The dip angles observed on Mars fell right within the range of those seen in coastal sedimentary deposits on Earth.

The researchers also ruled out other possible origins for the dipping reflectors, such as ancient river flows, wind or ancient volcanic activity. They suggested that the consistent dipping shape of the formations as well as the thickness of the sediments point to a coastal origin.

“We’re seeing that the shoreline of this body of water evolved over time,” Cardenas said. “We tend to think about Mars as just a static snapshot of a planet, but it was evolving. Rivers were flowing, sediment was moving, and land was being built and eroded. This type of sedimentary geology can tell us what the landscape looked like, how they evolved, and, importantly, help us identify where we would want to look for past life.”

The discovery indicates that Mars was once a much wetter place than it is today, further supporting the hypothesis of a past ocean that covered a large portion of the northern pole of the planet, Cardenas explained. The study also provided new information on the evolution of the Martian environment, suggesting that a life-friendly warm and wet period spanned potentially tens of millions of years.

“The capabilities of the Zhurong rover have allowed us to understand the geologic history of the planet in an entirely new way,” said Michael Manga, professor of Earth and planetary science at the University of California, Berkeley, and a corresponding author on the paper. “Its ground-penetrating radar gives us a view of the subsurface of the planet, which allows us to do geology that we could have never done before. All these incredible advancements in technology have made it possible to do basic science that is revealing a trove of new information about Mars.”

The other corresponding authors on the paper are Hai Liu of Guangzhou University and Guangyou Fang of the Chinese Academy of Sciences. The other Penn State co-author is Derek Elsworth, the G. Albert Shoemaker Chair and professor of energy and mineral engineering and geosciences. The other authors are Jianhui Li, Xu Meng, Diwen Duan and Haijing Lu of Guangzhou University; Jinhai Zhang and Bin Zhou of the Chinese Academy of Sciences; and Fengshou Zhang of Tongji University in Shanghai, China.