Adjoint-based simultaneous state and parameter estimation in an Arctic Sea Ice-Ocean Model using MITgcm (c63m)
Year: 2025
Type: article
Abstract: . Parameters in sea ice-ocean coupled models greatly affect the simulated ocean and sea ice evolution, and are normally tunned to bring the model state close to the observations. Using an adjoint method, spatiotemporally varying parameters of Arctic sea ice-ocean coupled model are optimized simultaneously with the initial condition and the atmospheric forcing by assimilating satellite and in-situ observations. The assimilation results show that the joint state and parameter estimation (SPE) substantially improves the sea ice concentration simulation. Particularly in October when the ocean surface starts to refreeze, SPE reduces the lead closing parameter Ho, which determines the minimum ice thickness formed in the open water, to increase the lateral sea ice growth and facilitate the seasonal rapid sea ice recovery in the Pacific sector. Comparisons with sea ice thickness observations from the moored upward looking sonars and Ice Mass Balance buoys demonstrate that the inclusion of model parameters in the optimization also leads to better sea ice thickness estimation. Overall, the adjoint-based SPE scheme has the potential to better reproduce the Arctic ocean and sea ice state and will be applied to reproduce a new Arctic sea ice-ocean reanalysis.
Source: Geoscientific model development
Language: English
Subfield: Atmospheric Science
Field: Earth and Planetary Sciences
Domain: Physical Sciences
SDG: Life below water
Open Access status: gold
Estimated APC paid: $1,725
Funders: Université Catholique de Louvain, Dartmouth College, Met Office, National Natural Science Foundation of China, European Organization for the Exploitation of Meteorological Satellites, National Key Research and Development Program of China, Program of Shanghai Academic Research Leader, Cold Regions Research and Engineering Laboratory
Awards: G6614079204, G710596693, G7294735235
OpenAlex ID: W4416945350
