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Volume 16, issue 10
Atmos. Chem. Phys., 16, 6091–6105, 2016
https://doi.org/10.5194/acp-16-6091-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 16, 6091–6105, 2016
https://doi.org/10.5194/acp-16-6091-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 19 May 2016

Research article | 19 May 2016

Changes in the shape of cloud ice water content vertical structure due to aerosol variations

Steven T. Massie et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Steven Massie on behalf of the Authors (22 Apr 2016)  Author's response    Manuscript
ED: Publish as is (01 May 2016) by Qiang Fu
Publications Copernicus
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Short summary
Changes in cloud vertical structure (i.e. the shape of cloud ice water content (IWC) vertical structure) due to variations in aerosol, observed by three different satellite experiments (MODIS, OMI, and MLS) are calculated in the Tropics during 2007–2010. This topic is of interest because aerosol-cloud interactions are the largest source of uncertainty in climate models. Analysis of the effects of MODIS aerosol, OMI absorptive aerosol, and MLS CO (an absorptive aerosol proxy) upon deep convective
Changes in cloud vertical structure (i.e. the shape of cloud ice water content (IWC) vertical...
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