Articles | Volume 12, issue 1
https://doi.org/10.5194/tc-12-325-2018
https://doi.org/10.5194/tc-12-325-2018
Research article
 | 
26 Jan 2018
Research article |  | 26 Jan 2018

Surface formation, preservation, and history of low-porosity crusts at the WAIS Divide site, West Antarctica

John M. Fegyveresi, Richard B. Alley, Atsuhiro Muto, Anaïs J. Orsi, and Matthew K. Spencer

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by John Fegyveresi on behalf of the Authors (26 Jul 2017)
ED: Reconsider after major revisions (31 Jul 2017) by Catherine Ritz
AR by John Fegyveresi on behalf of the Authors (12 Sep 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (16 Sep 2017) by Catherine Ritz
RR by Martin Schneebeli (27 Oct 2017)
ED: Publish subject to minor revisions (review by editor) (04 Nov 2017) by Catherine Ritz
AR by John Fegyveresi on behalf of the Authors (11 Nov 2017)  Author's response   Manuscript 
ED: Publish as is (28 Nov 2017) by Catherine Ritz
AR by John Fegyveresi on behalf of the Authors (01 Dec 2017)  Manuscript 
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Short summary
Observations at the WAIS Divide site in West Antarctica show that near-surface snow is strongly altered by weather-related processes, such as strong winds and temperature fluctuations, producing features that are recognizable within the WDC06A ice core. Specifically, over 10 000 prominent crusts were observed in the upper 560 m of the core. We show that these crusts develop more often in summers, during relatively low-wind, low-humidity, clear-sky periods with intense daytime sunshine.