Lost Submarine’s Final Data Reveals Antarctica’s Hidden Melt Terrain

Lost Submarine’s Final Data Reveals Antarctica’s Hidden Melt Terrain

By
Jamie Davis

Publish Date:June 2, 2026

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📰 The quick summary: An autonomous submarine mapped 54 square miles beneath Antarctica’s Dotson Ice Shelf before disappearing, leaving behind rare data that reveals how hidden fractures and complex terrain drive ice loss in ways current models often fail to capture.
📈 One key stat: Some of the pits mapped on the underside of the Dotson Ice Shelf reach roughly 980 feet long and 165 feet deep, showing just how dramatically warm ocean water can carve into ice that satellites cannot directly observe.
💬 One key quote: “A more extensive and complete picture” of ice shelf bases than researchers had before, said Karen Alley, a glaciologist at the University of Manitoba, describing what the submarine’s data revealed.

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1️⃣ The big picture: Antarctica’s ice shelves act as natural brakes for the glaciers behind them, and when warm ocean water eats away at their undersides, those glaciers can speed up and raise sea levels around the world. For years, scientists lacked direct views of what that erosion actually looks like up close. An autonomous submarine named Ran changed that in 2022 by spending 27 days beneath the Dotson Ice Shelf, traveling more than 620 miles and scanning 54 square miles of the ice ceiling with sonar. What it found was not a smooth surface but a complex hidden landscape of plateaus, terraced steps, deep channels, fractures, and teardrop-shaped pits carved by basal melting. Ran later disappeared during a follow-up mission in January 2024, but the data it sent back has given scientists one of the clearest pictures yet of how ocean heat attacks Antarctic ice from below.

2️⃣ Why is this good news: For the first time, scientists have detailed maps of the intricate terrain beneath an Antarctic ice shelf, filling a major gap that satellites simply cannot close on their own. Knowing that fractures, channels, and terraces steer warm water into specific weak spots helps researchers understand why some parts of an ice shelf melt far faster than others. That knowledge directly improves sea level forecasts, giving coastal planners, insurers, and city governments a more accurate foundation for long-term decisions. Beyond Dotson, the findings push the entire field toward building more realistic ice shelf models that treat the underside as complex terrain rather than a flat slab, which raises the quality of climate projections globally. Each improvement in those projections means communities have better information to adapt and prepare.

3️⃣ What’s next: Scientists will now work to incorporate the detailed terrain data into ice melt models so future sea level projections better reflect how fractures and channels concentrate heat. New robotic missions are likely to follow, as the loss of Ran has reinforced both the value and the challenge of sending autonomous vehicles under Antarctic ice. The findings, published in Science Advances, are expected to shape how researchers design the next generation of under-ice surveys across West Antarctica.

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Read the full story here: ECOnews / Ecoticias – An autonomous submarine named Ran mapped 54 square miles under Antarctica’s Dotson Ice Shelf and found plateaus, terraced “steps,” and teardrop pits carved by basal melt, then lost contact and disappeared, leaving behind data that shows why melt can concentrate in hidden fractures models often miss

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