Earth Matters

Petermann Glacier’s New Crack

April 24th, 2017 by Kathryn Hansen

In early April, remote sensing scientist Stef Lhermitte examined Sentinel-2 satellite images and saw a new crack developing on Greenland’s Petermann Glacier. About two weeks later, Landsat 8 also got a look (top image). Read more about that image here.

But the space-based view is not the only evidence of a new crack in the large glacier. NASA’s Operation IceBridge has been making science flights in the area this month, and scientists got a first-hand look. Kelly Brunt, a glaciologist at NASA’s Goddard Space Flight Center, snapped the photograph above from a window of a P-3 Orion research plane on April 14. The new crack is the feature running diagonal from the bottom-left of the photo toward the center.

“What’s interesting here is that the crack originated in the center of the glacier, not along the edges,” Brunt said. “When John Sonntag and I were looking for the new crack during the flight, we were looking for something substantial emanating from the edge. This totally surprised me!”

Most cracks start along a glacier’s edge, where a huge amount of strain is produced as the glacier slides along the walls of a fjord. That is especially true for Petermann—a narrow glacier that has previously rifted along the edges of its floating shelf.

Cracks that make their way across an ice shelf can eventually release icebergs. Petermann has launched two huge icebergs since 2010, so scientists are watching for additional retreat. It remains to be seen whether this crack will result in an iceberg. If the crack continues to lengthen, it could potentially meet the older rift at the edge of the glacier, visible near the top-center of the photo.

View more images of the rift and other icy phenomenon here.

One Response to “Petermann Glacier’s New Crack”

  1. Gary R. Stephens says:

    I have studies the satellite photograph from Google Earth, dates 4/2017 (day not specified). I have made a low-level pass over the glacier surface from East to West along the existing crack and past (West of) the “new” crack.

    I believer that I have traced a COMPLETE CRACK TRACK across the ice from NE to SW that includes the “New” crack.

    Therefore this “new” crack is part of an existing crack system clear across the glacier. I have a KMZ file of my analysis.