Articles | Volume 17, issue 12
https://doi.org/10.5194/tc-17-5007-2023
https://doi.org/10.5194/tc-17-5007-2023
Research article
 | 
29 Nov 2023
Research article |  | 29 Nov 2023

Evaluation of snow cover properties in ERA5 and ERA5-Land with several satellite-based datasets in the Northern Hemisphere in spring 1982–2018

Kerttu Kouki, Kari Luojus, and Aku Riihelä

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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 tc-2023-53', Anonymous Referee #1, 20 May 2023
    • AC1: 'Reply on RC1', Kerttu Kouki, 27 Jun 2023
  • RC2: 'Comment on tc-2023-53', Anonymous Referee #2, 22 May 2023
    • AC2: 'Reply on RC2', Kerttu Kouki, 27 Jun 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (05 Jul 2023) by Stephen Howell
AR by Kerttu Kouki on behalf of the Authors (29 Aug 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to revisions (further review by editor and referees) (07 Sep 2023) by Stephen Howell
ED: Referee Nomination & Report Request started (12 Sep 2023) by Stephen Howell
RR by Anonymous Referee #2 (25 Sep 2023)
RR by Anonymous Referee #1 (28 Sep 2023)
ED: Publish subject to minor revisions (review by editor) (05 Oct 2023) by Stephen Howell
AR by Kerttu Kouki on behalf of the Authors (12 Oct 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (12 Oct 2023) by Stephen Howell
AR by Kerttu Kouki on behalf of the Authors (17 Oct 2023)
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Short summary
We evaluated snow cover properties in state-of-the-art reanalyses (ERA5 and ERA5-Land) with satellite-based datasets. Both ERA5 and ERA5-Land overestimate snow mass, whereas albedo estimates are more consistent between the datasets. Snow cover extent (SCE) is accurately described in ERA5-Land, while ERA5 shows larger SCE than the satellite-based datasets. The trends in snow mass, SCE, and albedo are mostly negative in 1982–2018, and the negative trends become more apparent when spring advances.