Prsentation PowerPoint - PowerPoint PPT Presentation

1 / 8
About This Presentation
Title:

Prsentation PowerPoint

Description:

Improvement of model configurations ORCA025, NATL12, NATL4-AGRIF ... Role of katabatic winds and polynia on the production of AABW (MAR) ... – PowerPoint PPT presentation

Number of Views:42
Avg rating:3.0/5.0
Slides: 9
Provided by: Barn99
Category:

less

Transcript and Presenter's Notes

Title: Prsentation PowerPoint


1
DRAKKAR PLANED ACTIVITIES 2007-2010
LEGI/LPO/LOCEAN
Improvement of model configurations ORCA025,
NATL12, NATL4-AGRIF Variability of the subpolar
Atlantic (ORCA025, NATL12, NATL4) Variability
of the Southern Ocean (ORCA025, PERIANT025, AGRIF)
2
 
  • Improvement of model configurations ORCA025,
    NATL12, NATL4-AGRIF
  • 1 - Internal parameterisations
  • Sensitivity to the vertical resolution (64
    levels?)
  • Parameterisation of subgridscale at ¼ resolution
  • Parameterisation of the vertical mixing (tidal
    mixing in the Indonesian throughflow)
  • Values of several key sea-ice parameters
  •  
  • 2 - Improvement of atmospheric forcing
  • space/time resolution of satellite winds,
  • freshwater forcing,
  • diurnal cycle in solar heat flux,
  • accuracy of the atmospheric surface variables on
    recent periods (1990s and 2000s).

3
  • 3 - Eddy-resolving resolution
  • Further develop NATL12 configuration local
    AGRIF refinement in NATL4 (AMEN)
  • Validate in application studies on the role of
    the ocean mesoscale turbulence on water mass
    formation and cross-front transports.  
  • 4 - Development of validation tools
  • Development of statistical tools for a systematic
    quantitative model-observation comparisons with
    global observational databases (ENACT/ENSEMBLES
    AVISO).

4
  • Variability of the subpolar Atlantic
  • (ORCA025, NATL12, NATL4)
  • 1 - Mode water variability (AMEN) (Virginie
    Thierry, A.M. Treguier, collaboration with Eric
    de Boisséson and the OVIDE team)
  • Identify the formation areas of subpolar mode
    water in the Eastern North Atlantic
  • understand the mechanisms that set up its
    properties and its variability
  • investigate the way mode water ventilates the
    interior of the gyres
  • 2 - Characterisation of the boundary currents
    variability from high frequency to the decadal
    scale, and forcing mechanisms (A.M. Treguier, C.
    Guiavarch (post doc in 2007), a PhD student to
    start in 2007 at LPO, Gaelle Hervieux, PhD
    student at LEGI (2007), B. Barnier, T. Penduff,
    A. Wirth)
  • Connexion between the Greenland-Iceland-Scotland
    overflow and the deep boundary current (2007)
  • Interannual to decadal variability of the DWBC
    from the overflows to the subtropical gyre
    (2007-2008)
  • High frequency variability of the boundary
    currents in the North Atlantic (2007)
  • Wind-forced variability of the boundary current
    in the Irminger Sea (2007-2010)
  • Variability modes and local processes
    (2007-2009)
  • Exchanges between the boundary current and the
    interior (2008-2010)

5
  • 3 - Variability modes and local processes
    (2007-2009) Participants T. Penduff (LEGI), A.
    Lecointre (PhD starting in 2006, LEGI), A.M.
    Treguier (LPO), PhD student to start in 2008/2009
    (LPO), B. Barnier (LEGI).
  • to characterize and study the transports of
    properties (especially mass, heat, salt) and
    their low-frequency fluctuations across the
    selected sections (48N, 36N, 24.5N, 52W,
    66W, WOCE A1E/AR7E Greeland-Ireland transect,
    OVIDE).
  • to relate these 2D structure with basin-scale
    modes of variability, using observed, reanalyzed,
    and simulated data.
  • 4 - Exchanges between the boundary current and
    the interior (2008-2010)
  • Participants A.M. Treguier, T. Penduff, B.
    Barnier, J. Le Sommer, G. Madec, PhD student at
    LPO. Collaboration with the OVIDE team and Bruno
    Blanke.
  • mass exchanges between the boundary current, the
    overflows, and the interior of the gyres
  • water mass formation and transformation, by
    atmospheric forcing and mixing processes on the
    basin scale (including the boundary current).

6
  • Variability of the Southern Ocean
  • (ORCA025, PERIANT025, AGRIF)
  • 1 - Dynamics and variability of the Antarctic
    Circumpolar Current
  • - Role of eddies in the density balance of the
    ACC
  • Participants A.M. Treguier at LPO. Cooperation
    with S. Rintoul from CSIRO and M. England from
    UNSW in Australia.
  •  
  • - Role of eddies in the momentum balance of the
    ACC
  • Participants J. Le Sommer at LEGI, A.M. Treguier
    at LPO and B. Barnier at LEGI. Ongoing discussion
    with C. Wilson at University of Liverpool.
  • Is the geographical distribution of eddy
    vorticity forcing in the model simulations
    consistent with direct observations?
  • What is the vertical structure of the eddy
    vorticity forcing?
  • How is the eddy vorticity forcing related to
    topographic steering?

7
  • 2 - Life-cycle of Antarctic Bottom Water
  •  
  • - Role of katabatic winds and polynia on the
    production of AABW (MAR). Participants Pierre
    Mathiot (PhD student at LEGI), with contributions
    from B. Barnier, J. Le Sommer and J. M. Molines
    at LEGI, H. Gallée LGGE, A. M. Treguier at LPO.
    Cooperation with S. Rintoul and M. England from
    CSIRO in Australia. Ongoing discussion with A. de
    Montety et H. Goose for a possible cooperation
    with UC Louvain la Neuve.
  • What is the impact of the katabatic winds on the
    local ocean circulation and sea-ice cover?
  • What is the contribution of Antarcticas Coastal
    polynyas to the formation of Antarctic Bottom
    Water (AABW), a major component of the world
    ocean meridional circulation?
  • 3 - Life-cycle of Mode Waters (SAMW and AAIW)
  •  
  • - Semi-annual variability of Intermediate waters.
    Participants  J. Le Sommer (LEGI), collaboration
    M. England (UNSW)
  •  
  • Does the SAO force the variability of water mass
    properties observed by Sun and Watts, 2002?
  • Does the modulation of properties correspond to
    a variability of formation rates?
  • Is the oceanic response dependent on the
    mechanical forcing (Ekman/subduction) or rather
    the thermodynamic forcing (heat and freshwater
    fluxes)?

8
4 - Variability of cross frontal exchanges.
Participants A.M. Treguier, J. Le Sommer and G.
Madec, collaborations with M. England, S.
Rintoul, S. Speich and M. Arhan. One post-doc or
PhD student sought for 2008. GOODHOPE project.
Write a Comment
User Comments (0)
About PowerShow.com