EGU2020-8075
https://doi.org/10.5194/egusphere-egu2020-8075
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Investigating the climate variability in the Totten area using NEMO-LIM regional model.

Guillian Van Achter, Charles Pelletier, and Thierry Fichefet
Guillian Van Achter et al.
  • Université Catholique de Louvain, Earth and Life Institute, Earth and Climate, Belgium (guillian.vanachter@uclouvain.be)

The Totten ice shelf drains over 570 000 km² of East Antarctica. Most of the ice sheet that drains through the Totten ice-shelf is from Aurora Subglacial Basin and is marine based making the region potentially vulnerable to rapid ice sheet colapse.
Understanding how the changes in ocean circulation and properties are causing increased basal melt of Antarctic ice shelves is crucial for predicting future sea level rise.
In the context of the The PARAMOUR project (decadal predictability and variability of polar climate: the role of atmosphere-ocean-cryosphere multiscale interaction), we use a high resolution NEMO-LIM 3.6 regional model to investigate the variability and the predictability of the coupled climate system over the Totten area in East Antarctica.
In this poster, we will present our on-going work about the impact of landfast ice over the variability of the system. Landfast ice is sea ice that is fastened to the coastline, to the sea floor along shoals or to grouded icebergs. Current sea ice models are unable to represent very crudely the formation, maintenance and decay of coastal landfast ice. We applyed several parameterization for modeling landfast ice over the Totten ice shelf area.

How to cite: Van Achter, G., Pelletier, C., and Fichefet, T.: Investigating the climate variability in the Totten area using NEMO-LIM regional model., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8075, https://doi.org/10.5194/egusphere-egu2020-8075, 2020

This abstract will not be presented.