Articles | Volume 12, issue 4
The Cryosphere, 12, 1293–1306, 2018
https://doi.org/10.5194/tc-12-1293-2018

Special issue: The World Meteorological Organization Solid Precipitation...

The Cryosphere, 12, 1293–1306, 2018
https://doi.org/10.5194/tc-12-1293-2018

Research article 12 Apr 2018

Research article | 12 Apr 2018

Estimating the snow water equivalent on a glacierized high elevation site (Forni Glacier, Italy)

Antonella Senese et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by A. Senese on behalf of the Authors (22 Nov 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (04 Dec 2017) by Mareile Wolff
RR by Craig Smith (13 Dec 2017)
RR by Anonymous Referee #2 (18 Dec 2017)
ED: Publish subject to minor revisions (review by editor) (09 Feb 2018) by Mareile Wolff
AR by A. Senese on behalf of the Authors (16 Feb 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (07 Mar 2018) by Mareile Wolff
AR by A. Senese on behalf of the Authors (15 Mar 2018)  Author's response    Manuscript
Download
Short summary
We present and compare 11 years of snow data measured by an automatic weather station and corroborated by data from field campaigns on the Forni Glacier in Italy. The methodology we present is interesting for remote locations such as glaciers or high alpine regions, as it makes it possible to estimate the total snow water equivalent (SWE) using a relatively inexpensive, low-power, low-maintenance, and reliable instrument such as the sonic ranger.