Articles | Volume 25, issue 7
https://doi.org/10.5194/hess-25-4025-2021
https://doi.org/10.5194/hess-25-4025-2021
Research article
 | 
09 Jul 2021
Research article |  | 09 Jul 2021

Microphysical features of typhoon and non-typhoon rainfall observed in Taiwan, an island in the northwestern Pacific

Jayalakshmi Janapati, Balaji Kumar Seela, Pay-Liam Lin, Meng-Tze Lee, and Everette Joseph

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (13 Nov 2020) by Carlo De Michele
AR by Jayalakshmi J on behalf of the Authors (16 Nov 2020)  Author's response   Manuscript 
ED: Reconsider after major revisions (further review by editor and referees) (16 Nov 2020) by Carlo De Michele
ED: Referee Nomination & Report Request started (16 Nov 2020) by Carlo De Michele
RR by Anonymous Referee #3 (15 Dec 2020)
RR by Anonymous Referee #2 (18 Jan 2021)
ED: Publish subject to revisions (further review by editor and referees) (19 Feb 2021) by Carlo De Michele
AR by Jayalakshmi J on behalf of the Authors (19 Mar 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (12 Apr 2021) by Carlo De Michele
RR by Anonymous Referee #3 (30 Apr 2021)
RR by Anonymous Referee #2 (06 May 2021)
ED: Publish subject to technical corrections (26 May 2021) by Carlo De Michele
AR by Jayalakshmi J on behalf of the Authors (01 Jun 2021)  Author's response   Manuscript 
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Short summary
Typhoon (TY) and non-typhoon (NTY) rainy days in northern Taiwan summer seasons showed more large drops on NTY than TY rainy days. Relatively higher convective activity and drier conditions in NTY than TY lead to variations in microphysical characteristics between TY and NTY rainy days. The raindrop size distribution and kinetic energy relations assessed for TY and NTY rainfall can be useful for evaluating the radar rainfall estimation algorithms, cloud modeling, and rainfall erosivity studies.