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...

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Bibliographic Details
Main Authors: Eisen, Olaf, Jansen, Daniela, Franke, Steven, Weikusat, Ilka, Wilhelms, Frank
Format: Conference Object
Language:unknown
Published: 2021
Subjects:
Greenland
Polar Science
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
Description
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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