Articles | Volume 3, issue 4
https://doi.org/10.5194/wcd-3-1341-2022
https://doi.org/10.5194/wcd-3-1341-2022
Research article
 | 
18 Nov 2022
Research article |  | 18 Nov 2022

Non-linear intensification of monsoon low-pressure systems by the BSISO

Kieran M. R. Hunt and Andrew G. Turner

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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 wcd-2022-31', Anonymous Referee #1, 14 Jul 2022
  • RC2: 'Comment on wcd-2022-31', Anonymous Referee #2, 14 Sep 2022
  • RC3: 'Comment on wcd-2022-31', Anonymous Referee #3, 14 Sep 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Kieran Hunt on behalf of the Authors (28 Sep 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (29 Sep 2022) by Juliane Schwendike
RR by Anonymous Referee #1 (30 Sep 2022)
RR by Anonymous Referee #3 (10 Oct 2022)
RR by Anonymous Referee #2 (11 Oct 2022)
ED: Publish as is (19 Oct 2022) by Juliane Schwendike
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Short summary
More than half of India's summer monsoon rainfall arises from low-pressure systems: storms originating over the Bay of Bengal. In observation-based data, we examine how the generation and pathway of these storms are changed by the boreal summer intraseasonal oscillation – the chief means of large-scale control on the monsoon at timescales of a few weeks. Our study offers new insights for useful prediction of these storms, important for both water resources planning and disaster early warning.