Articles | Volume 18, issue 9
https://doi.org/10.5194/acp-18-6493-2018
https://doi.org/10.5194/acp-18-6493-2018
Research article
 | 
08 May 2018
Research article |  | 08 May 2018

Microphysical variability of Amazonian deep convective cores observed by CloudSat and simulated by a multi-scale modeling framework

J. Brant Dodson, Patrick C. Taylor, and Mark Branson

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Jason Dodson on behalf of the Authors (21 Dec 2017)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (23 Feb 2018) by Philip Stier
AR by Jason Dodson on behalf of the Authors (05 Mar 2018)  Author's response   Manuscript 
ED: Publish as is (12 Mar 2018) by Philip Stier
AR by Jason Dodson on behalf of the Authors (22 Mar 2018)
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Short summary
The vertical profiles of convection in the Amazon are sampled using CloudSat, with particular emphasis on day–night contrast. Focusing on vigorous deep convective cores reveals a distinct, previously unreported double-arc reflectivity feature in the contoured frequency by altitude diagram, likely corresponding with two modes of ice hydrometeor phase: snow versus graupel/hail. Replicating this feature in cloud-resolving models requires further improvements in the microphysical parameterization.
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