I had the great fortune to be involved in Operation IceBridge Alaska for almost a decade. But all good things must end. We had a last campaign this May. This was primarily a radar mission. We had fantastic results, seeing glacier bed in places we were never before successful. As usual, some pictures:
Malaspina Glacier: we flew a very dense grid over the Malaspina Glacier. Much of this large glacier is based below sea level and it is likely that this glacier will not survive in the current climate. We have just started a project to look at this in more detail.
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The snow covered moraine patterns on the Malaspina Lobe | |
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The Gulf of Alaska coast in front of Malaspina
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Sitkagi Lagoon is one of the places where warm ocean water is gaining access to glacier ice
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Fresh crevassing from an ongoing surge on the Malaspina
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Near the surge front: the ice is advancing into proglacial lakes
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A wall of advancing ice
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A view from the surge front up the lobe of the glacier
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This ice would have been easy to walk over, just a few months ago. Now it is totally broken up.
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Ice spilling out of the Seward Glacier into the lobe of Malaspina.
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The mighty St. Elias
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Mt. Bona: The saddle between Mt. Bona and Mt. Churchill was used as a drill site many years ago to retrieve an ice core. We acquired good ice penetrating and snow accumulation radar data over the area.
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The neighboring Twaharpies sticking up through the clouds
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University Peak
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The saddle between Mt.Bona and Mt.Churchill
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The Bagley Ice Valley: This is the largest expanse of ice in Alaska. We managed to image its base at up to 1500 m thick. I believe this is the deepest warm ice ever seen by an airborne radar.
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The Bagley Ice Valley with the massive Mt. Logan and Mt. St.Elias in the far distance.
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This is a view of the Hubsew ridge on Mt. Logan. This was first climbed by my PdD advisor Will Harrison, who recently passed away. He wrote a really entertaining and amazing story about the climb in the American Alpine Journal.
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Clouds boiling over into the Bagley Valley; time to get out of there....
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Mt. Wrangell is a large shield volcano with a deep caldera and it is the origin of one of the biggest land terminating glaciers in Alaska: Nabesna Glacier.
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Mt. Blackburn on the way to Mt. Wrangell. The ridge that extends towards the viewer was first climbed (I think) by my friends Keith Echelmeyer, Franz Mueter and myself.
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That's our route (approximately). The good old days ...
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The Mt. Wrangell caldera with steam
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And here are a few random pictures:
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Granite Creek valley on the way back from a mission. I like this beautiful old moraine.
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Icebergs breaking off from the Nizina Glacier
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Vitus Lake in front of Bering Glacier
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The team from University of Arizona, UAF, and University of Kansas (who did snow accumulation measurements)
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