Skip to main content
Scientific American
  • Cart 0
  • Forgot password?Loading
    Not yet registered?
  • |Newsletters
Advanced Search
  • COVID
  • Health
  • Mind & Brain
  • Environment
  • Technology
  • Space & Physics
  • Video
  • Podcasts
  • Opinion
  • Store
  • Subscribe
  • Current Issue
  • Cart0
  • Sign In
  • Newsletters
      • Share
      • Latest

      Greenland Meltdown Driven by Collapse of Glaciers at Ocean Outlets [Slide Show]

      The interactions between the island's glaciers and the surrounding seas may be driving ice loss, according to aerial photographs

      • Share on Facebook
      • Share on Twitter
      • Share on Reddit
      • Share on LinkedIn
      • Share via Email
      • Print
      Greenland Meltdown Driven by Collapse of Glaciers at Ocean Outlets [Slide Show]
      Slideshow (7) images
      View
      Credits: Anders A. Bjork, Natural History Museum of Denmark

      Greenland Meltdown Driven by Collapse of Glaciers at Ocean Outlets [Slide Show]

        • Share
      • NOT-SO-GLACIAL RETREAT: This visualization of the Kong Oscar Glacier in northwestern Greenland shows the ice loss as well as the release of icebergs from the glacier. Anders A. Bjork, Natural History Museum of Denmark
      • FUTURE LOSS: Massive icebergs prepare to calve from the Upernavik Ice Stream. Niels J. Korsgaard, Natural History Museum of Denmark
      • ICE HEIGHT: The glacier pictured here rises about 40 meters above sea level. Some glaciers like it, such as Sverdrup, lost as much as 80 meters of height between 2005 and 2010. Niels J. Korsgaard, Natural History Museum of Denmark
      • ICE STREAM: Fast-flowing ice reveals itself with crevasses and other wrinkles in the sheet, as compared with the smooth, slower-moving surrounding ice. Niels J. Korsgaard, Natural History Museum of Denmark
      • Advertisement
      • ICEBERG: At the calving front, icebergs break off from the Upernavik Ice Stream. The overturned iceberg in the center of this picture is roughly 200 meters across. Niels J. Korsgaard, Natural History Museum of Denmark
      • MELTDOWN: In one week in mid-July this year nearly the entire surface of the Greenland ice sheet melted for a few days. NASA
      • OCEAN FRONT: The Upernavik Ice Stream meets the ocean here in northwestern Greenland, calving icebergs. A plume of meltwater from beneath the glacier darkens the center of the ice sheet and reaches all the way to the sea... Niels J. Korsgaard, Natural History Museum of Denmark
      • Previous
      • Next
      of
      • View all
      • Link copied!
      • NOT-SO-GLACIAL RETREAT:
      • FUTURE LOSS:
      • ICE HEIGHT:
      • ICE STREAM:
      • ICEBERG:
      • MELTDOWN:
      • OCEAN FRONT:
      Advertisement
      Advertisement

      Newsletter

      Get smart. Sign up for our email newsletter.

      Sign Up

      Support Science Journalism

      Discover world-changing science. Explore our digital archive back to 1845, including articles by more than 150 Nobel Prize winners.

      Subscribe Now!Support Science Journalism

      Follow us

      • instagram
      • soundcloud
      • youtube
      • twitter
      • facebook
      • rss

      Scientific american arabic

      العربية
      • Return & Refund Policy
      • About
      • Press Room
      • FAQs
      • Contact Us
      • Site Map
      • Advertise
      • SA Custom Media
      • Terms of Use
      • Privacy Policy
      • California Consumer Privacy Statement
      • Use of cookies/Do not sell my data
      • International Editions
      Scientific American is part of Springer Nature, which owns or has commercial relations with thousands of scientific publications (many of them can be found at www.springernature.com/us). Scientific American maintains a strict policy of editorial independence in reporting developments in science to our readers.

      © 2023 Scientific American, a Division of Springer Nature America, Inc.

      All Rights Reserved.

      Scroll To Top

      Support science journalism.

      Scientific American paper issue and on tablet

      Thanks for reading Scientific American. Knowledge awaits.

      Already a subscriber? Sign in.

      Thanks for reading Scientific American. Create your free account or Sign in to continue.

      Create Account

      See Subscription Options

      Continue reading with a Scientific American subscription.

      You may cancel at any time.

      Sign in.