An iceberg floats in a fjord near the town of Tasiilaq, Greenland, June 18, 2018. New NASA data on water temperature, depth and salinity has helped explain why the rate of ice loss at northwestern Greenland’s Tracy glacier is almost four times the rate of the nearby Heilprin glacier. That’s because the fresh water flowing from Tracy, which sits on deeper bedrock, is mixing with a layer of warm, salty water off Greenland’s coast, accelerating the melting process, the researchers found. REUTERS/Lucas Jackson
NEW YORK (Reuters) – When Reuters photographer Lucas Jackson headed to Greenland in June, he travelled with a heavy, oversized rolling bag containing a crucial piece of equipment to document climate change. Jackson, one of a handful of Reuters photographers licensed to operate a drone, spent seven rainy days camped alongside Greenland’s Helheim glacier, near […]
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