Changes between Version 1 and Version 2 of 2017WP/NOC-2_JamesH-SCO_ISF
- Timestamp:
- 2017-05-18T04:08:29+02:00 (7 years ago)
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2017WP/NOC-2_JamesH-SCO_ISF
v1 v2 24 24 == Summary #summary 25 25 26 || '''Action''' || NOC-2_JamesH-SCO_ISF ||27 || '''PI(S)''' || James Harle ||26 || '''Action''' || NOC-2_JamesH-SCO_ISF || 27 || '''PI(S)''' || James Harle || 28 28 {{{#!td 29 29 '''Digest''' 30 30 }}} 31 31 {{{#!td 32 The simulation of dense water cascading from the shelf has been shown to benefit from the use of S-coordinate and mixed S-coordinate/partial step vertical grids in Arctic simulations. To gain maximum benefit in Antarctic simulations will require the under Ice-ShelF component to be adapted to work with the alternative vertical coordinates. This work will address this issue and will fully test solutions in a 'PERIANT' type model of the Southern Ocean being developed under the UK 'ORCHESTRA' project. 32 The simulation of dense water cascading from the shelf has been shown to benefit from the use of S-coordinate and mixed S-coordinate/partial step vertical grids in Arctic simulations.\\ 33 To gain maximum benefit in Antarctic simulations will require the under Ice-ShelF component to be adapted to work with the alternative vertical coordinates.\\ 34 This work will address this issue and will fully test solutions in a 'PERIANT' type model of the Southern Ocean being developed under the UK 'ORCHESTRA' project. 33 35 }}} 34 36 |-