Articles | Volume 12, issue 6
Geosci. Model Dev., 12, 2255–2283, 2019
https://doi.org/10.5194/gmd-12-2255-2019
Geosci. Model Dev., 12, 2255–2283, 2019
https://doi.org/10.5194/gmd-12-2255-2019

Model experiment description paper 12 Jun 2019

Model experiment description paper | 12 Jun 2019

Assessment of sub-shelf melting parameterisations using the ocean–ice-sheet coupled model NEMO(v3.6)–Elmer/Ice(v8.3)

Lionel Favier 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 Lionel Favier on behalf of the Authors (26 Apr 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (01 May 2019) by Alexander Robel
RR by Anonymous Referee #2 (10 May 2019)
RR by Anonymous Referee #1 (17 May 2019)
ED: Publish subject to technical corrections (17 May 2019) by Alexander Robel
AR by Lionel Favier on behalf of the Authors (22 May 2019)  Author's response    Manuscript
Download
Short summary
The melting at the base of floating ice shelves is the main driver of the Antarctic ice sheet current retreat. Here, we use an ideal set-up to assess a wide range of melting parameterisations depending on oceanic properties with regard to a new ocean–ice-sheet coupled model, published here for the first time. A parameterisation that depends quadratically on thermal forcing in both a local and a non-local way yields the best results and needs to be further assessed with more realistic set-ups.