Explore atmosphere-ocean-ice interactions over seasonal to centennial timescales.
Establish the role of sea ice on Antarctic surface mass balance (SMB) over seasonal to centennial timescales.
Quantify the role of winds and atmospheric circulation on SMB variability.
Key deliverables:
Improve existing SMB reconstructions as well as its drivers, using a combination of new paleo records and data-assimilation approaches.
Initiate new data compilations, based on isotope and chemical data from high-resolution paleo-archives (ice core, marine sediments, peat…) to reconstruct past sea ice and atmospheric circulation.
Refine the interpretation and the estimate of the uncertainty of existing records.
Test the compatibility between the signal reconstructed from different records, in particular between the oceanic and continental records, and between models and observations.
Understand the atmosphere-ocean-ice interactions over seasonal to centennial timescales.