Changes between Version 29 and Version 30 of 2015WP/2015Action_institutions_CNRS
- Timestamp:
- 2014-10-14T18:38:50+02:00 (10 years ago)
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2015WP/2015Action_institutions_CNRS
v29 v30 92 92 93 93 === '''CNRS-16 - '''LIM3, FCT4 advection scheme === 94 ''' Motivation: ''' Rachid, using a classical test case of advection of a passive tracer, have shown that a 4th order Flux Corrected Transport (FCT4) ha vea behavior very close to the one of a Pather scheme, i.e. the one used in LIM. It is much cheaper as you don't have to advect second order moments in addition to the field itself. [[BR]] ''' Status :''' The FCT4 scheme has been coded and tested as part of a 3D advection scheme for ocean tracers. [[BR]] ''' Main tasks :''' adapt to LIM3 and test it. If it performs as expected, implement it is the current version of LIM3 [[BR]] ''' Science Reviewer:''' Martin Vancoppenolle [[BR]] ''' System Reviewer:''' [[BR]] ''' Deadline:''' [[BR]] ''' Priority:''' [[BR]] ''' Depends on:''' [[BR]] ''' Principal Investigator : ''' Clément Rousset, Gurvan Madec94 ''' Motivation: ''' Rachid, using a classical test case of advection of a passive tracer, have shown that a 4th order Flux Corrected Transport (FCT4) had a behavior very close to the one of a Pather scheme, i.e. the one used in LIM. It is much cheaper as you don't have to advect second order moments in addition to the field itself. [[BR]] ''' Status :''' The FCT4 scheme has been coded and tested as part of a 3D advection scheme for ocean tracers. [[BR]] ''' Main tasks :''' adapt to LIM3 and test it. If it performs as expected, implement it is the current version of LIM3 [[BR]] ''' Science Reviewer:''' Martin Vancoppenolle [[BR]] ''' System Reviewer:''' [[BR]] ''' Deadline:''' [[BR]] ''' Priority:''' [[BR]] ''' Depends on:''' [[BR]] ''' Principal Investigator : ''' Clément Rousset, Gurvan Madec 95 95 96 96 === '''CNRS-17 - '''Vertical redistribution of salt rejection due to ice formation ===