Articles | Volume 15, issue 10
https://doi.org/10.5194/tc-15-4981-2021
https://doi.org/10.5194/tc-15-4981-2021
Research article
 | 
28 Oct 2021
Research article |  | 28 Oct 2021

The influence of snow on sea ice as assessed from simulations of CESM2

Marika M. Holland, David Clemens-Sewall, Laura Landrum, Bonnie Light, Donald Perovich, Chris Polashenski, Madison Smith, and Melinda Webster

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on tc-2021-174', Anonymous Referee #1, 09 Jul 2021
    • AC1: 'Reply on RC1', Marika Holland, 01 Sep 2021
  • RC2: 'Comment on tc-2021-174', Anonymous Referee #2, 12 Jul 2021
    • AC2: 'Reply on RC2', Marika Holland, 01 Sep 2021
  • RC3: 'Comment on tc-2021-174', Anonymous Referee #3, 15 Jul 2021
    • AC3: 'Reply on RC3', Marika Holland, 01 Sep 2021

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) (14 Sep 2021) by John Yackel
AR by Marika Holland on behalf of the Authors (17 Sep 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (20 Sep 2021) by John Yackel
AR by Marika Holland on behalf of the Authors (27 Sep 2021)

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Marika Holland on behalf of the Authors (21 Oct 2021)   Author's adjustment   Manuscript
EA: Adjustments approved (24 Oct 2021) by John Yackel
Download
Short summary
As the most reflective and most insulative natural material, snow has important climate effects. For snow on sea ice, its high reflectivity reduces ice melt. However, its high insulating capacity limits ice growth. These counteracting effects make its net influence on sea ice uncertain. We find that with increasing snow, sea ice in both hemispheres is thicker and more extensive. However, the drivers of this response are different in the two hemispheres due to different climate conditions.