Marco Tedesco, a polar scientist on the Local weather Faculty’s Lamont-Doherty Earth Observatory, explains how distant sensing information from satellites and drones can reveal the processes behind the melting of Greenland’s ice sheets, at present one of many largest contributors to sea-level rise.
“The acceleration of melting in Greenland now contributes 30-35% of the entire sea stage rise,” Tedesco says. “It’s anticipated to be, along with Antarctica, round 50% of the entire contribution over the subsequent few a long time as a result of we don’t anticipate any slowdown.”
That is the sixth video of Science for the Planet, a brief explainer collection about how scientists and students from throughout the Columbia Local weather Faculty are attempting to grasp the results of local weather change and assist resolve the disaster.
Learn extra about Tedesco’s work:
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