Articles | Volume 14, issue 8
https://doi.org/10.5194/tc-14-2673-2020
https://doi.org/10.5194/tc-14-2673-2020
Research article
 | 
21 Aug 2020
Research article |  | 21 Aug 2020

Clouds damp the radiative impacts of polar sea ice loss

Ramdane Alkama, Patrick C. Taylor, Lorea Garcia-San Martin, Herve Douville, Gregory Duveiller, Giovanni Forzieri, Didier Swingedouw, and Alessandro Cescatti

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
ED: Reconsider after major revisions (further review by editor and referees) (23 Apr 2020) by Dirk Notz
AR by Ramdane Alkama on behalf of the Authors (24 Apr 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (14 May 2020) by Dirk Notz
RR by Anonymous Referee #2 (26 May 2020)
ED: Publish subject to minor revisions (review by editor) (15 Jun 2020) by Dirk Notz
AR by Ramdane Alkama on behalf of the Authors (19 Jun 2020)
ED: Publish as is (06 Jul 2020) by Dirk Notz
AR by Ramdane Alkama on behalf of the Authors (09 Jul 2020)
Download
Short summary
The amount of solar energy absorbed by Earth is believed to strongly depend on clouds. Here, we investigate this relationship using satellite data and 32 climate models, showing that this relationship holds everywhere except over polar seas, where an increased reflection by clouds corresponds to an increase in absorbed solar radiation at the surface. This interplay between clouds and sea ice reduces by half the increase of net radiation at the surface that follows the sea ice retreat.