The Gravity of Larsen CNovember 13th, 2017 by Kathryn Hansen
Perhaps you know the feeling: that moment when you see with your eyes something you have previously only seen in pictures. Before today, I knew the Larsen C ice shelf only from the satellite images we have published since August 2016. The attention paid to the shelf off the Antarctic Peninsula has been due to a rift that eventually calved an enormous iceberg. Today (November 12), the Operation IceBridge mission flew its suite of airborne instruments over the shelf and I caught a first-hand look.
I was aware that I would be seeing an iceberg the size of Delaware, but I wasn’t prepared for how that would look from the air. Most icebergs I have seen appear relatively small and blocky, and the entire part of the berg that rises above the ocean surface is visible at once. Not this berg. A-68 is so expansive it appears if it were still part of the ice shelf. But if you look far into the distance you can see a thin line of water between the iceberg and where the new front of the shelf begins. A small part of the flight today took us down the front of iceberg A-68, its towering edge reflecting in the dark Weddell Sea.
This particular flight, however, aimed to get more than just a surficial look at Larsen C; to understand the system as a whole, scientists also want to know the bathymetry of the bedrock below. To do that, the flight path was planned with gravity measurements in mind. While radar instruments can “see” through snow and ice on land to map the bedrock, radar has trouble when instead of land there is water below the ice. For the gravimeter, that’s not a problem. The new flight lines—flown for the first time—followed the ground tracks of the future ICESat-2 satellite, and simultaneously increased the area of Larsen C mapped with the gravimeter.
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