Effects of stochastic ice strength perturbation on Arctic finite element sea ice modeling
The ice strength parameter P* is a key parameter in dynamic/thermodynamic sea ice models that cannot be measured directly. Stochastically perturbing P* in the Finite Element Sea Ice–Ocean Model (FESOM) of the Alfred Wegener Institute aims at investigating the effect of uncertainty pertaining to this...
Main Authors: | Juricke, S, Lemke, P, Timmermann, R, Rackow, T |
---|---|
Format: | Journal article |
Published: |
American Meteorological Society
2013
|
Similar Items
-
Potential sea ice predictability and the role of stochastic sea ice strength perturbations
by: Juricke, S, et al.
Published: (2014) -
Improved teleconnection between Arctic sea ice and the North Atlantic Oscillation through stochastic process representation
by: K. Strommen, et al.
Published: (2022-08-01) -
Influence of stochastic sea ice parametrization on climate and the role of atmosphere-sea ice-ocean interaction
by: Juricke, S, et al.
Published: (2014) -
Evaluation of Arctic Sea Ice Thickness from a Parameter-Optimized Arctic Sea Ice–Ocean Model
by: Qiaoqiao Zhang, et al.
Published: (2023-05-01) -
A stochastic model for the turbulent ocean heat flux under Arctic sea ice
by: Toppaladoddi, S, et al.
Published: (2021)