Arctic sea ice is a crucial component of the climate system. The radiation balance and the dynamics of the atmosphere and ocean have strong interactions with sea ice. Observations show that the extent of Arctic Sea ice has been declining over the last few decades. This could have a significant impact on the climate, ecosystems and human activities and highlights the need for improved sea ice prediction.
Tag: Model
4DEnVar Data Assimilation Technique
Land surface models are paramount to the climate modelling community in that they provide ‘boundary conditions’ — a quantification of the water, carbon and energy fluxes between the land and atmosphere at the Earth’s surface. Arguably the biggest problem for land surface modellers is the selection of parameter values for use in their land surface model.