Articles | Volume 10, issue 2
Geosci. Model Dev., 10, 765–789, 2017
Geosci. Model Dev., 10, 765–789, 2017

Model description paper 17 Feb 2017

Model description paper | 17 Feb 2017

The Finite-volumE Sea ice–Ocean Model (FESOM2)

Sergey Danilov et al.


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 Sergey Danilov on behalf of the Authors (20 Dec 2016)  Author's response    Manuscript
ED: Publish as is (21 Dec 2016) by David Ham
Short summary
Numerical models of global ocean circulation are used to learn about future climate. The ocean circulation is characterized by processes on different spatial scales which are still beyond the reach of present computers. We describe a new model setup that allows one to vary a model's spatial resolution and hence focus the computational power on regional dynamics, reaching a better description of local processes in areas of interest.