Changes between Version 5 and Version 6 of 2012WP/2012Action_institutions_NOC
- Timestamp:
- 2011-11-17T18:14:26+01:00 (12 years ago)
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2012WP/2012Action_institutions_NOC
v5 v6 74 74 ''' Motivation:''' An improvement in the numerical treatment of vertical diffusion can be achieved by replacing the fully implicit scheme with a Crank-Nicholson scheme. This approach is widely used in other ocean models (e.g. ROMS, MARS...) and can be implemented relatively simply.[[BR]] ''' Main task:''' (1 wk) [[BR]] (1) The replacement scheme will be implemented and its performance tested. [[BR]] ''' Principal Investigator :''' Andrew Coward (acc@noc.soton.ac.uk) [[BR]] ''' Deadline :''' 18th February 2011 [[BR]] ''' Priority: ''' Medium[[BR]] ''' Science Reviewer : ''' Mercator (TBC)[[BR]] ''' System Reviewer : ''' Paris (TBC) 75 75 76 === '''NOCS.09 — Implementation of spectral nudging''' ===76 === '''NOCS.09 — Stand alone surface module''' === 77 77 78 ''' Motivation:''' Work by our Canadian colleagues has demonstrated the potential benefits of spectral nudging techniques to restore large scale gradients without suppressing meso-scale activity. [[BR]] ''' Status: ''' Coded in v3.2. Requires porting to and testing and documenting in v3.4[[BR]] ''' Main task''' (3 wk)[[BR]] ''' Deadline :''' 22nd April 2011 [[BR]] ''' Priority: ''' High[[BR]] ''' Science Reviewer :''' Mercator (TBC)[[BR]] ''' System Reviewer : ''' Paris (TBC)[[BR]] ''' Principal Investigator :''' Jeff Blundell (jeff@noc.soton.ac.uk) 79 78 ''' Motivation:''' A standalone surface module is proposed which will allow surface elements such as sea-ice, iceberg drift and surface fluxes to be run using prescribed model state fields. [[BR]] ''' Status: ''' [[BR]] ''' Main task''' (3 wk)[[BR]] ''' Deadline :''' 22nd April 2011 [[BR]] ''' Priority: ''' High[[BR]] ''' Science Reviewer :''' [[BR]] ''' System Reviewer : ''' Paris (TBC)[[BR]] ''' Principal Investigator :''' Steve Alderson (sga@noc.ac.uk) 80 79 81 80 === '''NOCL.01 — Wetting and Drying''' ===