Characterising the regional glaciological context of relevance for IceCube-Gen-2
2021
The internal layer architecture and crystal anisotropy in ice are two main parameters to take into account for analysing particle signals within the IceCube and follow-on arrays. Using airborne and ground-based radar measurements we present a new approach to especially define the horizontal anisotropy of the bulk fabric in ice and suggest implementation during pre-site surveys in particular for the RNO-G test array near Summit, Greenland.
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