Articles | Volume 16, issue 13
Atmos. Chem. Phys., 16, 8193–8204, 2016
https://doi.org/10.5194/acp-16-8193-2016
Atmos. Chem. Phys., 16, 8193–8204, 2016
https://doi.org/10.5194/acp-16-8193-2016

Research article 07 Jul 2016

Research article | 07 Jul 2016

Hybrid ensemble 4DVar assimilation of stratospheric ozone using a global shallow water model

Douglas R. Allen et al.

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 Douglas Allen on behalf of the Authors (09 Jun 2016)  Author's response    Manuscript
ED: Publish subject to technical corrections (18 Jun 2016) by William Lahoz (deceased)
Download
Short summary
This study examines the extraction of wind information from assimilation of ozone observations in a simplified model of the atmosphere. Understanding this process is important for the stratosphere (10–50 km altitude), where wind observations are sparse. A key aspect is using multiple forecasts (ensembles) to determine the error correlations between ozone and wind. Experiments using different ensemble sizes show that ozone benefits winds more when ensemble information is blended into the system.
Altmetrics
Final-revised paper
Preprint