Document Type

Conference Proceeding

Publication Title

Annals of Glaciology

Publication Date

2005

First Page

10

Last Page

16

Volume Number

41

Abstract/ Summary

We have recorded reflection profiles of firn through large areas of West Antarctica and part of the East Antarctic plateau using 400 MHz short-pulse radar. The locations show accumulation rates that vary from well above to well below the vertical radar resolution. Most reflection horizons have extensive lateral continuity, and are composed of distinctive wavelets with a consistent phase polarity sequence within their successive half-cycles. We modeled these waveforms, and conclude that they arise from thin, double layers of ice over hoar, which is consistent with the standard model of firn stratification. In addition, we conclude that ice/hoar layers are extensive throughout West Antarctica and also present (although more sparsely) beneath the Antarctic Plateau.

Citation/Publisher Attribution

Arcone, SA, Spikes, VB, and Hamilton, GS, 2005, Phase Structure of Radar Stratigraphic Horizons Within Antarctic Firn: Annals of Glaciology, Vol 41 2005, v. 41, p. 10-16. Available on publisher's site at: http://www.ingentaconnect.com/content/igsoc/agl/2005/00000041/00000001/art00003

Publisher Statement

© Copyright 2005 by the International Glaciological Society

DOI

10.3189/172756405781813267

Version

publisher's version of the published document

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