Radio echo sounding data analysis of the Shackleton Ice Shelf

In this study, our initial results are presented for the interpretation of the radio echo sounding data collected over the Shackleton Ice Shelf and adjacent ice sheet (East Antarctica) during the 2003/2004 Australian- Italian expedition. The Shackleton Ice Shelf is one of the larger ice shelves of t...

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Bibliographic Details
Published in:Annals of Geophysics
Main Authors: Urbini, S., Cafarella, L., Zirizzotti, A., Tabacco, I. E., Bottari, C., Baskaradas, J. A., Young, N.
Other Authors: Urbini, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Cafarella, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Zirizzotti, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Tabacco, I. E.; Università degli Studi di Milano, Dipartimento Scienze della Terra, Milano, Italy, Bottari, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Baskaradas, J. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Young, N.; Australian Antarctic Division, and Antarctic Climate and Ecosystems Cooperative Research Centre, Hobart, Australia, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Università degli Studi di Milano, Dipartimento Scienze della Terra, Milano, Italy, Australian Antarctic Division, and Antarctic Climate and Ecosystems Cooperative Research Centre, Hobart, Australia
Format: Article in Journal/Newspaper
Language:English
Published: INGV 2010
Subjects:
Ice
Online Access:http://hdl.handle.net/2122/6205
https://doi.org/10.4401/ag-4563
Description
Summary:In this study, our initial results are presented for the interpretation of the radio echo sounding data collected over the Shackleton Ice Shelf and adjacent ice sheet (East Antarctica) during the 2003/2004 Australian- Italian expedition. The Shackleton Ice Shelf is one of the larger ice shelves of the East Antarctic Ice Sheet. The radar survey provided data relating to ice thickness and bed morphology of the outlet glaciers, and thickness of their floating portions. The glacier grounding lines were determined by assessment of the basal echo characters. The information derived is compared with data from the BEDMAP database and from other sources. Published 79-87 3.8. Geofisica per l'ambiente JCR Journal open