Articles | Volume 18, issue 20
https://doi.org/10.5194/acp-18-14799-2018
https://doi.org/10.5194/acp-18-14799-2018
Research article
 | 
16 Oct 2018
Research article |  | 16 Oct 2018

A new model of meteoric calcium in the mesosphere and lower thermosphere

John M. C. Plane, Wuhu Feng, Juan Carlos Gómez Martín, Michael Gerding, and Shikha Raizada

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by John Plane on behalf of the Authors (29 Sep 2018)  Manuscript 
ED: Publish as is (04 Oct 2018) by Andreas Engel
AR by John Plane on behalf of the Authors (04 Oct 2018)
Download
Short summary
Meteoric ablation creates layers of metal atoms in the atmosphere around 90 km. Although Ca and Na have similar elemental abundances in most minerals found in the solar system, surprisingly the Ca abundance in the atmosphere is less than 1 % that of Na. This study uses a detailed chemistry model of Ca, largely based on laboratory kinetics measurements, in a whole-atmosphere model to show that the depletion is caused by inefficient ablation of Ca and the formation of stable molecular reservoirs.
Altmetrics
Final-revised paper
Preprint