Repository logo
  • English
  • Italiano
Log In
New user? Click here to register.Have you forgotten your password?
  1. Home
  2. Affiliation
  3. INGV
  4. Article published / in press
  5. RES Signatures of Ice Bottom Near to Dome C (Antarctica)
 
  • Details

RES Signatures of Ice Bottom Near to Dome C (Antarctica)

Author(s)
Urbini, S.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Cafarella, L.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Tabacco, I. E.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Baskaradas, J.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Zirizzotti, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Language
English
Obiettivo Specifico
7A. Geofisica di esplorazione
Status
Published
JCR Journal
JCR Journal
Peer review journal
No
Journal
IEEE Transactions on Geoscience and Remote Sensing  
Issue/vol(year)
3/53 (2015)
ISSN
0196-2892
Electronic ISSN
1558-0644
Publisher
IEEE / Institute of Electrical and Electronics Engineers Incorporated
Pages (printed)
1558 - 1564
Date Issued
March 2015
DOI
10.1109/TGRS.2014.2345457
URI
https://www.earth-prints.org/handle/2122/10030
Subjects
02. Cryosphere::02.02. Glaciers::02.02.99. General or miscellaneous  
Subjects

Bedrock

Dome C

EPICA

reflectivity

radio-echo sounding (...

data analysis

Abstract
Abstract—Geophysical surveys have played a fundamental role in glaciology, climatology, and geology studies conducted at and around the site of the EPICA Dome C Ice Core (Antarctica).
Analysis of radio-echo sounding (RES) data collected during the 2009 and 2011 Italian Antarctic Expeditions, in the immediate vicinity (2 km) of the Core site, reveals the presence of small-scale bedrock structures. Data acquired during the 2011 campaign, which applied the latest updates of our instrument, show double echoes from the ice bottom separated by very small time intervals. These reflections are distributed close to the topographic dome and do not always correspond to particular features of the bedrock structure, but instead may correspond to small-scale subglacial water storage. The unprecedented spatial resolution of the basal environment for Dome C from these recent surveys allows us to
identify this and other features that have been missed by previous larger scale RES surveys of this area.
Type
article
File(s)
Loading...
Thumbnail Image
Name

IEEE_2014_articolo_doppie.pdf

Description
main article
Size

6.84 MB

Format

Adobe PDF

Checksum (MD5)

ff5b2b443a4f9ca79e0ce409de19a201

rome library|catania library|milano library|napoli library|pisa library|palermo library
Explore By
  • Research Outputs
  • Researchers
  • Organizations
Info
  • Earth-Prints Open Archive Brochure
  • Earth-Prints Archive Policy
  • Why should you use Earth-prints?
Earth-prints working group
⚬Anna Grazia Chiodetti (Project Leader)
⚬Gabriele Ferrara (Technical and Editorial Assistant)
⚬Massimiliano Cascone
⚬Francesca Leone
⚬Salvatore Barba
⚬Emmanuel Baroux
⚬Roberto Basili
⚬Paolo Marco De Martini

Built with DSpace-CRIS software - Extension maintained and optimized by 4Science

  • Privacy policy
  • End User Agreement
  • Send Feedback