EGU General Assembly 2008
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  Oral Programme - CR21 Sea ice, ice-ocean interactions and glaciology of Antarctica (co-listed in OS)

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Convener: Morales Maqueda, M.
Co-Convener: Feltham, D., Kulessa, B.

Tuesday, 15 April 2008

Lecture Room: Lecture Room 30

Chairperson: MORALES MAQUEDA, M. A.

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13:30 - 14:00
EGU2008-A-01301;  CR21-1TU3O-001
Fichefet, T.; Vancoppenolle, M.; Goosse, H.; Bouillon, S.; Madec, G.; Morales Maqueda, M.A.
Simulating the mass balance and salinity of Arctic and Antarctic sea ice with LIM3-OPA9 (solicited)

14:00 - 14:15
EGU2008-A-00120;  CR21-1TU3O-002
Girard, L.; Weiss, J.; Molines, J.M.
How realistic are sea ice models in terms of sea ice dynamics and associated scaling properties?

14:15 - 14:30
EGU2008-A-05553;  CR21-1TU3O-003
Yakovlev, N.
On the implementation of the FEMAO (Finite Element Model of the Arctic Ocean) with tides the dynamical ice-ocean coupling in a case of thick ice

14:30 - 14:45
EGU2008-A-09789;  CR21-1TU3O-004
Maksym, T
Antarctic sea ice surface processes: a comparison of field results with a thermodynamic-hydraulic model

14:45 - 15:15
EGU2008-A-00578;  CR21-1TU3O-006
Thomas, D
Sea ice biogeochemistry - some key issues for modellers (solicited)


Chairperson: KULESSA, B.

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15:30 - 15:45
EGU2008-A-00711;  CR21-1TU4O-002
Tedesco, L.; Vichi, M.; Haapala, J.; Stipa, T.
SIM2: a numerical model of sea-ice halo-thermodynamics for biogeochemical studies

15:45 - 16:00
EGU2008-A-00773;  CR21-1TU4O-003
Brabant, F.; Carnat, G.; Ackley, S.F.; Tison, J.-L.
DMS and DMSP dynamics in Antarctic early spring sea ice (Bellingshausen Sea, September-October 2007)

16:00 - 16:30
EGU2008-A-10903;  CR21-1TU4O-004
Shuman, C. ; Hulbe, C. ; Scambos, T.
Crane Glacier in the Larsen B Embayment: Faster, Slower, Higher, Lower after Ice Shelf Loss (solicited)

16:30 - 16:45
EGU2008-A-07225;  CR21-1TU4O-005
Jenkins, A; Jacobs, S
Circulation and melting beneath George VI Ice Shelf, Antarctica

16:45 - 17:00
EGU2008-A-08526;  CR21-1TU4O-006
Shoosmith, D. R.; Jenkins, A.; Brandon, M. A.
Oceanography of the Bellingshausen Sea and implications for West Antarctic Peninsula ice shelves


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