Articles | Volume 19, issue 7
Atmos. Chem. Phys., 19, 4659–4683, 2019
https://doi.org/10.5194/acp-19-4659-2019
Atmos. Chem. Phys., 19, 4659–4683, 2019
https://doi.org/10.5194/acp-19-4659-2019

Research article 08 Apr 2019

Research article | 08 Apr 2019

On the fine vertical structure of the low troposphere over the coastal margins of East Antarctica

Étienne Vignon et al.

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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 Étienne Vignon on behalf of the Authors (28 Feb 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (13 Mar 2019) by Jayanarayanan Kuttippurath
ED: Publish subject to minor revisions (review by editor) (25 Mar 2019) by Jayanarayanan Kuttippurath
AR by Étienne Vignon on behalf of the Authors (25 Mar 2019)  Author's response    Manuscript
ED: Publish as is (26 Mar 2019) by Jayanarayanan Kuttippurath
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Short summary
The future sea-level rise will depend on how much the Antarctic ice sheet gain – via precipitation – or loose mass. The simulation of precipitation by numerical models used for projections depends on the representation of the atmospheric circulation over and around Antarctica. Using daily measurements from balloon soundings at nine Antarctic stations, this study characterizes the structure of the atmosphere over the Antarctic coast and its representation in atmospheric simulations.
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