Articles | Volume 22, issue 6
https://doi.org/10.5194/nhess-22-1795-2022
https://doi.org/10.5194/nhess-22-1795-2022
Research article
 | 
02 Jun 2022
Research article |  | 02 Jun 2022

Idealized simulations of Mei-yu rainfall in Taiwan under uniform southwesterly flow using a cloud-resolving model

Chung-Chieh Wang, Pi-Yu Chuang, Shi-Ting Chen, Dong-In Lee, and Kazuhisa Tsuboki

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (19 Dec 2021) by Joaquim G. Pinto
AR by Pi-Yu Chuang on behalf of the Authors (21 Dec 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (10 Jan 2022) by Joaquim G. Pinto
RR by Anonymous Referee #2 (20 Jan 2022)
RR by Anonymous Referee #3 (28 Mar 2022)
ED: Publish subject to minor revisions (review by editor) (28 Mar 2022) by Joaquim G. Pinto
AR by Pi-Yu Chuang on behalf of the Authors (31 Mar 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (08 Apr 2022) by Joaquim G. Pinto
AR by Pi-Yu Chuang on behalf of the Authors (10 Apr 2022)  Manuscript 
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Short summary
In this study, cloud-resolving simulations are performed under idealized and uniform southwesterly flow direction and speed to investigate the rainfall regimes in the Mei-yu season and the role of complex mesoscale topography on rainfall without the influence of unwanted disturbances, including a low-Froude number regime where the thermodynamic effects and island circulation dominate, a high-Froude number regime where topographic rainfall in a flow-over scenario prevails, and a mixed regime.
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