NASA's Operation IceBridge Completes Eleven Years of Polar Surveys
Narration: Katie Jepson
Transcript:
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Narrator: Operation IceBridge, you may know it from the
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the beautiful photos that pop up in your feed.
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But did you know that IceBridge is the largest polar airborne survey of its kind?
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IceBridge was designed to study annual changes in thickness of sea ice, glaciers, and ice sheets. As well as bridge the
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gap between the ICESat and ICESat-2 polar observing satellites.
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Between 2009 and 2019, IceBridge flew over a thousand
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missions, gathering data that has redefined
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our understanding of the cryosphere.
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So, let’s take a look back at some of the mission milestones from over the years.
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One of the first steps to measure sea ice thickness is to get a handle on the amount of
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snow that accumulates on top of it.
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The IceBridge team pioneered the use of a snow radar instrument to gather the first
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widespread dataset of snow thickness on top of both Arctic and Antarctic sea ice.
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Closer to land,
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the point at which a glacier begins to float is called a grounding line,
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and it’s a very challenging place to measure ice thickness.
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Using two instruments, a radar sounder and a gravimeter,
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the IceBridge team was able to survey hundreds of these complex transition zones,
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enhancing scientists’ understanding of the rapid changes in glacier behavior.
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In 2011, NASA scientists discovered
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a 19-mile long crack across the Pine Island Glacier,
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one of the fastest retreating glaciers in Antarctica.
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The crack measured 260 feet wide and 195 feet deep
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when it was observed.
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Throughout the mission, IceBridge was able to map rifts in ice shelves prior to major
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calving events. And while these events are part of a natural cycle,
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IceBridge’s observations helped scientists better record the changes in calving
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frequency and model how they may be related to a thinning ice shelf.
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The motion of the Antarctic Ice Sheet,
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the largest ice sheet in the world, is heavily influenced by
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the topography of the bedrock underneath.
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In 2013, the British Antarctic Survey used over 25 million measurements
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collected by IceBridge and other projects
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to develop a 3D map of Antarctica’s bedrock topography.
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Called Bedmap-2, it provided unprecedented
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detail of how the continents bedrock shaped the flow of the ice sheet.
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Data collected by IceBridge enabled
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many discoveries in the Arctic as well.
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A team from the University of Bristol used IceBridge’s radar data,
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along with other datasets, to uncover a 400-mile long canyon buried
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under nearly two miles of ice.
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This hidden canyon is longer than any other known on earth, provides a critical clue to modeling how melting ice
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is funneled into the Arctic Ocean.
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Using ice-penetrating radar data collected by IceBridge,
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scientists were able to build the first-ever age map of the layers
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deep inside the Greenland Ice Sheet.
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For the first time, scientists could navigate the history of Greenland’s ice layers,
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extending previously collected ice cores to better understand
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the ice sheet’s history and help build models of its future.
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An international team of scientists
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used decades of NASA data to uncover a massive impact crater
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hiding beneath the Hiawatha Glacier in northwest Greenland.
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At roughly a thousand feet deep and more than 19 miles wide,
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it is potentially one of the youngest large impact craters on Earth.
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Cockpit: "It’s going to happen..5..4..3
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..2..Mark on the overpass 043435 Zulu"
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Narrator: Ice was bridged on April 8, 2019,
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with the direct underflight of the ICESat-2
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satellite over Arctic sea ice.
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For the first time, both ICESat-2 and IceBridge would be taking the same
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elevation measurements of the same ice.
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These mirrored measurements were critical in validating the satellites instruments
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and continue the legacy of IceBridge after the mission was completed.
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Over the course of its 11-year mission, IceBridge
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completed 1056 scientific flights and provided a wellspring of data
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that fueled the publication of more than 660 papers
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and counting.
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The mission provided new insight into the processes driving the changes in the cryosphere,
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helping scientists better understand what we can expect in the future.
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