Changes between Version 1 and Version 2 of 2017WP/NOC-2_JamesH-SCO_ISF


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Timestamp:
2017-05-18T04:08:29+02:00 (3 years ago)
Author:
nicolasmartin
Comment:

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  • 2017WP/NOC-2_JamesH-SCO_ISF

    v1 v2  
    2424== Summary #summary 
    2525 
    26 || '''Action'''       || NOC-2_JamesH-SCO_ISF           || 
    27 || '''PI(S)'''        || James Harle                            || 
     26|| '''Action'''       || NOC-2_JamesH-SCO_ISF                                                       || 
     27|| '''PI(S)'''        || James Harle                                                                || 
    2828{{{#!td 
    2929'''Digest''' 
    3030}}} 
    3131{{{#!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. 
     32The 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.\\ 
     33To gain maximum benefit in Antarctic simulations will require the under Ice-ShelF component to be adapted to work with the alternative vertical coordinates.\\ 
     34This 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. 
    3335}}} 
    3436|-