Researchers at the University of California in Irvine identified that warm ocean currents penetrate kilometres below the base of the Thwaites Glacier in Western Antarctica. The study mapped the contact line where the frozen layer separates from the continental rock and starts to float directly over the polar sea. Data indicate that salt water [...]
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Researchers at the University of California in Irvine identified that warm ocean currents penetrate kilometres below the base of the Thwaites Glacier in Western Antarctica. The study mapped the contact line where the frozen layer separates from the continental rock and starts to float directly over the polar sea. Data indicate that salt water [...]