LU Peng, YU Miao, WANG Lei, Bin CHENG, WANG Qingkai & LI Zhijun
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The study of Arctic sea ice has traditionally been focused on large-scale such as reductions of ice coverage, thickness, volumes and sea ice regime shift. Research has primarily concentrated on the impact of large-scale external factors such as atmospheric and oceanic circulations, and solar radiation. Additionally, Arctic sea ice also undergoes rapid micro-scale evolution such as gas bubbles formation, brine pockets migration and massive formation of surface scattering layer. Field studies like CHINARE (2008–2018) and MOSAiC (2019–2020) have confirmed these observations, yet the full understanding of those changes remain insufficient and superficial. In order to cope better with the rapidly changing Arctic Ocean, this study reviews the recent advances in the microstructure of Arctic sea ice in both field observations and laboratory experiments, and looks forward to the future objectives on the microscale processes of sea ice. The significant porosity and the cyclical annual and seasonal shifts likely modify the ice’s thermal, optical, and mechanical characteristics, impacting its energy dynamics and mass balance. Current thermodynamic models, both single-phase and dual-phase, fail to accurately capture these microstructural changes in sea ice, leading to uncertainties in the results. The discrepancy between model predictions and actual observations strongly motivates the parameterization on the evolution in ice microstructure and development of next-generation sea ice models, accounting for changes in ice crystals, brine pockets, and gas bubbles under the background of global warming. It helps to finally achieve a thorough comprehension of Arctic sea ice changes, encompassing both macro and micro perspectives, as well as external and internal factors.
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