The waters along Greenland’s east coast are shaped by strong ocean currents which transport Arctic sea ice southwards from the Greenland Sea and into the Denmark Strait. This continuous movement redistributes freshwater, influences marine ecosystems, and helps regulate regional ocean circulation and climate. As the ice drifts, ocean eddies and winds fracture the pack ice into intricate swirls, long trailing streaks, and scattered fragments. The result is a mosaic of sea ice and…
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Source eu-space.europa.eu
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