No anomalous supersaturation in ultracold  cirrus laboratory experiments

Clouser, Benjamin W.; Lamb, Kara D.; Sarkozy, Laszlo C.; Habig, Jan; Ebert, Volker; Saathoff, Harald; Möhler, Ottmar; Moyer, Elisabeth J.

doi:https://doi.org/10.5194/acp-20-1089-2020

Articles | Volume 20, issue 2

https://doi.org/10.5194/acp-20-1089-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-20-1089-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 20, issue 2

Research article

|

28 Jan 2020

Research article |

| 28 Jan 2020

No anomalous supersaturation in ultracold cirrus laboratory experiments

Benjamin W. Clouser, Kara D. Lamb, Laszlo C. Sarkozy, Jan Habig, Volker Ebert, Harald Saathoff, Ottmar Möhler, and Elisabeth J. Moyer

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Final revised paper (published on 28 Jan 2020)
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Preprint (discussion started on 01 Apr 2019)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Review of manuscript acp-2019-150', Anonymous Referee #2, 06 May 2019
RC2: 'Review of Clouser et al.', Anonymous Referee #1, 25 Jun 2019
AC1: 'Replies to Referee Comments', Benjamin Clouser, 25 Nov 2019

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Benjamin Clouser on behalf of the Authors (26 Nov 2019) Author's response Manuscript

ED: Publish as is (11 Dec 2019) by Hang Su

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Short summary

Previous measurements of water vapor in the upper troposphere and lower stratosphere (UT/LS) have shown unexpectedly high concentrations of water vapor in ice clouds, which may be due to an incomplete understanding of the structure of ice and the behavior of ice growth in this part of the atmosphere. Water vapor measurements during the 2013 IsoCloud campaign at the AIDA cloud chamber show no evidence of this anomalous supersaturation in conditions similar to the real atmosphere.