Articles | Volume 22, issue 8
https://doi.org/10.5194/cp-22-1441-2026
https://doi.org/10.5194/cp-22-1441-2026
Research article
 | 
04 Aug 2026
Research article |  | 04 Aug 2026

Atmospheric pressure and anemological conditions in south-western Greenland in the second half of the 18th century

Konrad Chmist, Garima Singh, Andrzej Araźny, Rajmund Przybylak, and Przemysław Wyszyński

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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-2025-5657', Anonymous Referee #1, 06 Jan 2026
    • AC1: 'Reply on RC1', Konrad Chmist, 26 Feb 2026
  • RC2: 'Comment on egusphere-2025-5657', Anonymous Referee #2, 18 Jan 2026
    • AC2: 'Reply on RC2', Konrad Chmist, 26 Feb 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (16 Mar 2026) by Julie Loisel
AR by Konrad Chmist on behalf of the Authors (02 Apr 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (21 Apr 2026) by Julie Loisel
RR by Anonymous Referee #2 (20 May 2026)
RR by Anonymous Referee #1 (26 May 2026)
ED: Publish subject to technical corrections (07 Jun 2026) by Julie Loisel
AR by Konrad Chmist on behalf of the Authors (09 Jun 2026)  Author's response   Manuscript 
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Short summary
The currently observed climate changes are most intense in the Arctic region. This study utilized some of the oldest existing meteorological measurement series in this region. Atmospheric pressure and anemological conditions were analysed and then compared with contemporary measurements. This showed that the weakest low and strongest high systems occur in the same months. Prevailing wind directions have also remained unchanged, while the northerly wind carries less frigid air than in the past.
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