Characterising the regional glaciological context of relevance for IceCube-Gen-2
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 anisotro...
Main Authors: | , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2021
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/53548/ https://epic.awi.de/id/eprint/53548/1/Eisen_2021_Ice-Cube_workshop_opt.pdf https://hdl.handle.net/10013/epic.19a352d5-4b23-47fa-b199-21789c582e9b https://hdl.handle.net/ |
Summary: | 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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