IBM and NASA open-source a lunar foundation model: up to 23% better at spotting ice, volcanoes and craters, with the dataset released too

2026-09-15·9 min read

On September 10, 2026, IBM and NASA announced in an official press release from Yorktown Heights, New York, the open-source release of the NASA-IBM Lunar Foundation Model. In IBM's words, it is one of the first publicly available foundation models for scientific exploration of the Moon. What it targets is lunar remote sensing data: for decades, sensors and instruments have continuously observed the Moon, generating petabytes of data, yet to study the lunar surface scientists have had to either sift through maps and images by hand or rely on low-resolution, task-specific machine learning models. The headline numbers are concrete: the model exceeds widely used methods by up to 23% in identifying key geographic features on the Moon's surface, including potential ice deposits, craters and volcanic formations. Both the model and its dataset are now open on Hugging Face.

Start with the three specific metrics in the official release, because that is where the value of this story sits. First, potential lunar ice: permanently shadowed regions are among the Moon's most difficult environments to observe, yet they may hold lunar ice below the surface. Ice means water and oxygen — resources considered essential for a future Moon base and for producing rocket fuel for missions to Mars. A technical paper authored by IBM and NASA researchers shows the model reduced error (RMSE) in identifying areas with high potential for lunar ice by up to 22% compared with the SwinV2-B (ImageNet) model. Second, volcanic history: scientists study lunar volcanic features called Irregular Mare Patches to understand the Moon's volcanic history and thermal evolution, and detecting these changing regions is also strategic for future surface operations. Using imperfect labels, the model captures the extent of volcanic features 3% better than SwinV2-B, with comparable accuracy, greater efficiency and lower fine-tuning costs. Third, crater detection: the model can identify, contextualise and classify craters at metre-scale resolution with accuracy comparable to state-of-the-art models like SwinV2-B while offering greater efficiency and lower fine-tuning costs. At context-scale resolution (~100 m) it outperforms SwinV2-B by nearly 19% using just half the training data.

Why this is hard in itself is stated plainly in IBM's release: despite the wealth of lunar data, no publicly available, unified dataset existed that brings multi-modal, multi-resolution data into a common framework suitable for modern machine learning. So they open-sourced the dataset too. It is the first open-source lunar dataset of its kind, aggregating over 30 spatially aligned layers from nine instruments across four missions — tens of thousands of images and maps showing unique geophysical properties of the lunar surface. The sources include NASA's Lunar Reconnaissance Orbiter (LRO) and the GRAIL mission, with complementary lunar data from the Japan Aerospace Exploration Agency's SELENE/Kaguya for a rich, multi-modal view of the lunar surface and subsurface. That detail is especially relevant to anyone working with data: model performance gains often come not from a more complicated architecture but from genuinely aligning layers that were scattered across different coordinates, resolutions and instrument conventions onto one spatial reference. Getting 30-plus layers spatially aligned is serious upstream engineering.

There is one line about methodology worth quoting on its own. Juan Bernabe-Moreno, Director of IBM Research Europe, UK and Ireland, said the model gives scientists a foundation to explore the Moon at scale — connecting observations across instruments, revealing patterns that are difficult to see in isolation, and providing an open platform the global research community can build on. Kevin Murphy, chief science data officer and acting chief data and AI officer at NASA Headquarters, points at the more general problem: NASA has spent decades building an extraordinary scientific record of the Moon, but collecting data is only part of the job, and the data also has to become easier for scientists to explore and use. That sentence explains the real value of this class of foundation model for research institutions — not replacing scientists' judgment with AI, but lowering the entry barrier to cross-instrument data. The operational significance is explicit too: crater mapping helps NASA select safe landing sites, avoid hazards such as steep slopes and boulders, and plan locations for long-term lunar infrastructure, all of which are concrete requirements under the Artemis programme.

Finally, the positioning: this model joins the Prithvi family of open foundation models, which until now spanned geospatial, weather and heliophysics, and now the Moon. IBM's framing of the family is that instead of building a new algorithmic system for every scientific question, researchers can start from a shared model and adapt it to new tasks to accelerate discovery across domains. That logic will be familiar to developers — it is the same move software engineering made from rebuilding wheels to reusing shared components. The difference is that in science the data is far more heterogeneous and the labels are far worse than in most commercial settings, so whether a shared model transfers is a real question rather than a slogan. The technical paper's approach here — training with imperfect labels and reporting error rates — is more useful than a single flattering number. The model, the dataset and the technical report are all directly available on Hugging Face, which makes reproduction straightforward, and for an open-source community reproducibility matters more than a claimed benchmark.

🤔 Frequently Asked Questions

Q1: What can you actually do with this model?

Three task families per the official release: identifying where potential lunar ice deposits may be, studying the extent of volcanic features (Irregular Mare Patches), and detecting and classifying craters at metre-scale and roughly 100-metre resolution. It is positioned as a multimodal, multi-resolution foundation model for lunar remote sensing, which means you use it as a starting point to fine-tune downstream tasks rather than as a finished product. The technical paper is titled Multimodal-Multiresolution Foundation Model for Lunar Remote Sensing, and both model and dataset live under the nasa-ibm-ai4science organisation on Hugging Face.

Q2: Where does the 23% figure come from?

The release says the model exceeds widely used methods by up to 23% in identifying key geographic features on the Moon's surface, including potential ice deposits, craters and volcanic formations. Broken down it is more specific: up to 22% lower RMSE than SwinV2-B (ImageNet) on high-potential lunar ice; 3% better on capturing the extent of volcanic features; nearly 19% better crater detection at context-scale (~100 m) using just half the training data; and comparable accuracy to SwinV2-B at metre-scale resolution with greater efficiency and lower fine-tuning costs. So 23% is a cross-task ceiling, not a single-task result — look at the per-task number for whatever you care about.

Q3: Why is the dataset as important as the model?

Because on tasks like these the bottleneck is usually data, not the model. IBM states plainly that despite the wealth of lunar data, no publicly available unified dataset existed that could bring multi-modal, multi-resolution data into a common framework suitable for modern machine learning. This release aggregates more than 30 spatially aligned layers from nine instruments across four missions — covering NASA's LRO and GRAIL and incorporating complementary data from JAXA's SELENE/Kaguya — into one unified dataset. For researchers that means no longer spending months aligning layers of different projections and resolutions before running an experiment.

Q4: How does it relate to the rest of the Prithvi family?

It is the lunar member of the Prithvi family of open foundation models, which previously spanned geospatial, weather and heliophysics. IBM's framing of the family is a shared starting point: rather than building a separate algorithmic system for every scientific question, start from a shared model and adapt it to new tasks to accelerate discovery across domains. In practice that means the model's interfaces and usage patterns resemble the rest of the family, so if you have already worked with a Prithvi geospatial or weather model, the migration cost is well below starting from scratch.

🛠️ Recommended Tools

  • CSV Viewer - This lunar dataset has more than 30 spatially aligned layers; scan the column structure in a viewer first instead of debugging it from inside a training script
  • JSON to CSV - Model cards and metadata usually ship as JSON; converting layer manifests to CSV makes it much easier to check them off against the paper's task setup
  • Markdown Table Generator - The three sets of results are scattered across the press release and the paper; putting them in one comparison table (task / baseline / gain / share of training data) before it goes into your notes avoids mixing them up

Reading news about scientific foundation models, I look first for the line that least resembles marketing. Here it is the second half of Kevin Murphy's quote: collecting data is only part of the job, and the data also has to be made easier for scientists to explore and use. That captures something easily overlooked — the long-standing AI bottleneck in science has not been a shortage of algorithms but data locked inside separate coordinate systems, resolutions and toolchains. So what carries weight for me here is not the 23% but the fact that more than 30 layers were actually aligned and released. Another detail worth keeping: the technical paper trains on imperfect labels and reports that honestly. Clean labels are rare in science, and saying so out loud makes the numbers more credible, not less.

Summary

On September 10, 2026, IBM and NASA announced in an official press release the open-source release of the NASA-IBM Lunar Foundation Model, one of the first publicly available foundation models for scientific exploration of the Moon. Official figures: up to 23% better than widely used methods at identifying key surface features including potential ice deposits, craters and volcanic formations; up to 22% lower RMSE than SwinV2-B (ImageNet) for high-potential lunar ice; 3% better at capturing volcanic feature extent; nearly 19% better crater detection at ~100 m context-scale resolution using just half the training data; and comparable accuracy to state-of-the-art models at metre-scale resolution with greater efficiency and lower fine-tuning costs. The model is multimodal and multi-resolution, built to help scientists turn decades of multi-instrument, petabyte-scale data into insights supporting a sustained human presence on the Moon. It ships with the first open-source lunar dataset of its kind: more than 30 spatially aligned layers from nine instruments across four missions, including tens of thousands of images and maps, drawing on NASA's LRO and GRAIL plus complementary data from JAXA's SELENE/Kaguya. It joins the Prithvi family of open foundation models, which previously spanned geospatial, weather and heliophysics. Quoted officially: NASA Headquarters chief science data officer Kevin Murphy notes that collecting data is only part of the job and the data must also become easier to explore and use; Juan Bernabe-Moreno, Director of IBM Research Europe, UK and Ireland, says the model provides an open platform for exploring the Moon at scale and connecting observations across instruments. The model, dataset and technical paper Multimodal-Multiresolution Foundation Model for Lunar Remote Sensing are all open under the nasa-ibm-ai4science organisation on Hugging Face.

Sources: IBM Newsroom(官方新闻稿) · Hugging Face 模型页 · 技术报告 PDF · CNET