Articles | Volume 16, issue 22
https://doi.org/10.5194/acp-16-14249-2016
https://doi.org/10.5194/acp-16-14249-2016
Research article
 | 
16 Nov 2016
Research article |  | 16 Nov 2016

Large-scale vertical velocity, diabatic heating and drying profiles associated with seasonal and diurnal variations of convective systems observed in the GoAmazon2014/5 experiment

Shuaiqi Tang, Shaocheng Xie, Yunyan Zhang, Minghua Zhang, Courtney Schumacher, Hannah Upton, Michael P. Jensen, Karen L. Johnson, Meng Wang, Maike Ahlgrimm, Zhe Feng, Patrick Minnis, and Mandana Thieman

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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 Shuaiqi Tang on behalf of the Authors (17 Oct 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (18 Oct 2016) by Maria Assuncao Silva Dias
RR by Alan K. Betts (19 Oct 2016)
RR by Enio Souza (28 Oct 2016)
ED: Publish subject to technical corrections (28 Oct 2016) by Maria Assuncao Silva Dias
AR by Shuaiqi Tang on behalf of the Authors (29 Oct 2016)  Manuscript 
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Short summary
Data observed during the Green Ocean Amazon (GoAmazon2014/5) experiment are used to derive the large-scale fields in this study. The morning propagating convective systems are active during the wet season but rare during the dry season. The afternoon convections are active in both seasons, with heating and moistening in the lower level corresponding to the vertical convergence of eddy fluxes. Case study shows distinguish large-scale environments for three types of convective systems in Amazonia.
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