Articles | Volume 21, issue 3
https://doi.org/10.5194/acp-21-2191-2021
https://doi.org/10.5194/acp-21-2191-2021
Research article
 | 
15 Feb 2021
Research article |  | 15 Feb 2021

Ice injected into the tropopause by deep convection – Part 2: Over the Maritime Continent

Iris-Amata Dion, Cyrille Dallet, Philippe Ricaud, Fabien Carminati, Thibaut Dauhut, and Peter Haynes

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Iris-Amata Dion on behalf of the Authors (20 Feb 2020)  Manuscript 
ED: Referee Nomination & Report Request started (21 Feb 2020) by Geraint Vaughan
RR by Anonymous Referee #2 (12 Mar 2020)
RR by Michelle Santee (12 Apr 2020)
ED: Reconsider after major revisions (17 Apr 2020) by Geraint Vaughan
AR by Iris-Amata Dion on behalf of the Authors (28 May 2020)  Manuscript 
ED: Referee Nomination & Report Request started (16 Jun 2020) by Geraint Vaughan
RR by Michelle Santee (07 Jul 2020)
ED: Reconsider after major revisions (07 Jul 2020) by Geraint Vaughan
AR by Iris-Amata Dion on behalf of the Authors (13 Oct 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (16 Oct 2020) by Geraint Vaughan
RR by Michelle Santee (24 Oct 2020)
ED: Publish subject to minor revisions (review by editor) (24 Oct 2020) by Geraint Vaughan
AR by Iris-Amata Dion on behalf of the Authors (17 Nov 2020)  Manuscript 
ED: Publish subject to minor revisions (review by editor) (21 Nov 2020) by Geraint Vaughan
AR by Iris-Amata Dion on behalf of the Authors (26 Nov 2020)  Author's response   Manuscript 
ED: Publish as is (27 Nov 2020) by Geraint Vaughan
AR by Iris-Amata Dion on behalf of the Authors (14 Dec 2020)  Manuscript 
Short summary
Ice in the tropopause has a strong radiative effect on climate. The amount of ice injected (∆IWC) up to the tropical tropopause layer has been shown to be the highest over the Maritime Continent (MC), a region that includes Indonesia. ∆IWC is studied over islands and sea of the MC. Space-borne observations of ice, precipitation and lightning are used to estimate ∆IWC and are compared to ∆IWC estimated from the ERA5 reanalyses. It is shown that Java is the area of the greatest ∆IWC over the MC.
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