Articles | Volume 5, issue 1
https://doi.org/10.5194/wcd-5-1-2024
https://doi.org/10.5194/wcd-5-1-2024
Research article
 | 
10 Jan 2024
Research article |  | 10 Jan 2024

Seasonally dependent increases in subweekly temperature variability over Southern Hemisphere landmasses detected in multiple reanalyses

Patrick Martineau, Swadhin K. Behera, Masami Nonaka, Hisashi Nakamura, and Yu Kosaka

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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-2023-1137', Anonymous Referee #1, 11 Jul 2023
  • RC2: 'Comment on egusphere-2023-1137', Anonymous Referee #2, 23 Jul 2023
  • AC1: 'Final author comments on egusphere-2023-1137', Patrick Martineau, 21 Aug 2023
    • EC1: 'Reply on AC1', Tim Woollings, 24 Aug 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Patrick Martineau on behalf of the Authors (03 Oct 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (17 Oct 2023) by Tim Woollings
AR by Patrick Martineau on behalf of the Authors (23 Oct 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (25 Oct 2023) by Tim Woollings
AR by Patrick Martineau on behalf of the Authors (31 Oct 2023)

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Patrick Martineau on behalf of the Authors (08 Jan 2024)   Author's adjustment   Manuscript
EA: Adjustments approved (08 Jan 2024) by Tim Woollings
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Short summary
The representation of subweekly near-surface temperature variability trends over the Southern Hemisphere landmasses is compared across multiple atmospheric reanalyses. It is found that there is generally a good agreement concerning the positive trends affecting South Africa and Australia in the spring, and South America in the summer. A more efficient generation of subweekly temperature variance by horizontal temperature fluxes contributes to the observed rise.