Kinematic response of ice-rise divides to changes in ocean and atmosphere forcing
The majority of Antarctic ice shelves are bounded by grounded ice rises. These ice rises exhibit local flow fields that partially oppose the flow of the surrounding ice shelves. Formation of ice rises is accompanied by a characteristic upward-arching internal stratigraphy (“Raymond arches”), whose g...
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Universitaet Tuebingen
2019
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| Online Access: | https://dx.doi.org/10.15496/publikation-35487 https://publikationen.uni-tuebingen.de/xmlui/handle/10900/94103 |