Articles | Volume 17, issue 1
https://doi.org/10.5194/tc-17-175-2023
https://doi.org/10.5194/tc-17-175-2023
Research article
 | 
16 Jan 2023
Research article |  | 16 Jan 2023

Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radar

Jilu Li, Fernando Rodriguez-Morales, Xavier Fettweis, Oluwanisola Ibikunle, Carl Leuschen, John Paden, Daniel Gomez-Garcia, and Emily Arnold

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-368', William D. Harcourt, 06 Aug 2022
    • AC1: 'Reply on RC1', Jilu Li, 21 Oct 2022
  • RC2: 'Comment on egusphere-2022-368', HP Marshall, 19 Sep 2022
    • AC2: 'Reply on RC2', Jilu Li, 21 Oct 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (09 Nov 2022) by Melody Sandells
AR by Jilu Li on behalf of the Authors (14 Nov 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (08 Dec 2022) by Melody Sandells
AR by Jilu Li on behalf of the Authors (16 Dec 2022)  Manuscript 
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Short summary
Alaskan glaciers' loss of ice mass contributes significantly to ocean surface rise. It is important to know how deeply and how much snow accumulates on these glaciers to comprehend and analyze the glacial mass loss process. We reported the observed seasonal snow depth distribution from our radar data taken in Alaska in 2018 and 2021, developed a method to estimate the annual snow accumulation rate at Mt. Wrangell caldera, and identified transition zones from wet-snow zones to ablation zones.