A remote island turns the Antarctic sky into a fluid-dynamics lesson
New imagery highlighted by NASA Earth Observatory shows one of the atmosphere’s most striking repeating patterns unfolding off the coast of West Antarctica: a chain of cloud swirls known as von Karman vortex streets. The display formed downwind of Peter I Island, an isolated, ice-covered volcanic island in the Bellingshausen Sea, and was captured by the Operational Land Imager on Landsat 8 on February 11, 2026.
The scene is visually dramatic, but it is also scientifically familiar. When steady air flows around an obstruction such as a mountain or island, the current can separate into alternating spinning eddies on the leeward side. In satellite imagery, those eddies can appear as a procession of comma-like cloud curls, each rotating opposite the one before it.
NASA’s description places the event in one of the windiest regions on Earth. The Southern Ocean surrounding Antarctica allows air to move with relatively little interruption from land, creating the powerful prevailing winds long nicknamed the Roaring Forties, Furious Fifties, and Screaming Sixties. Peter I Island acts as a rare obstacle in that open flow, and under the right conditions it can produce a textbook example of atmospheric wake turbulence.
Why Peter I Island matters
Peter I Island is remote even by Antarctic standards. NASA notes that it lies roughly 400 kilometers off the coast of West Antarctica and more than 1,800 kilometers from Cape Horn, Chile. The island’s isolation helps explain why observations like this are compelling: there are relatively few nearby landforms to complicate the picture, so the interaction between wind, cloud, and terrain stands out clearly.
The island itself is described as an ice-cloaked volcano. NASA says a circular crater about 100 meters wide sits at its summit, which rises 1,640 meters above sea level. The Smithsonian Institution’s Global Volcanism Program classifies it as a shield-like volcano, though NASA also notes that there are no records of recent eruptions.
That combination of elevation, shape, and exposure makes the island an efficient trigger for wave patterns and rotating eddies in the lower atmosphere. The resulting cloud structures are more than pretty satellite images. They are evidence of how air parcels lose stability, peel away from an obstacle, and reorganize into repeated vortices.







