Impact of satellite thickness data assimilation on bias reduction in Arctic sea ice concentration

• Published in: NPJ climate and atmospheric science 2023-06, Vol.6 (1), p.73-12, Article 73
• Main Authors: Lee, Jeong-Gil, Ham, Yoo-Geun
• Format: Article
• Language: English
• Subjects: 704/106/125; 704/106/829/2737; Albedo; Atmospheric Protection/Air Quality Control/Air Pollution; Atmospheric Sciences; Bias; Climate Change/Climate Change Impacts; Climatology; Control simulation; Data assimilation; Data collection; Earth and Environmental Science; Earth Sciences; Enthalpy; Growing season; Ice cover; Ice thickness; Interpolation; Melting; Salinity; Salinity effects; Sea ice; Seasons; Thickness
• ISSN: 2397-3722; 2397-3722
• DOI: 10.1038/s41612-023-00402-6

The impact of assimilating satellite-retrieved Arctic sea ice thickness (SIT) on simulating sea ice concentration (SIC) climatology in CICE5 is examined using a data assimilation (DA) system based on the ensemble optimal interpolation. The DA of the SIT satellite data of CryoSat-2 and SMOS during 2011–2019 significantly reduces the climatological bias of SIC and SIT in both sea ice melting and growing seasons. Moreover, the response of SIC to SIT change is strongly dependent on the seasons and latitudinal locations. The SIT in the inner ice zone thickens due to the SIT DA during the boreal winter wherein the SIT observation is available; the ice melting throughout the subsequent seasons is attenuated to increase SIC during the boreal summer to reduce the simultaneous SIC bias. In marginal ice zones, the positive SIT bias depicted in the control simulation is significantly reduced by SIT DA, which reduces the positive SIC bias. The idealized experiments of reducing the SIT show that the enhanced ice bottom melting process plays a crucial role in reducing the SIC; the prescribed SIT thinning increases the ice bulk salinity due to the weak gravity drainage of brine and increases the ice bulk temperature due to the decrease of the sea ice albedo. The augmentation of the ice salinity and temperature contributes to the shrinkage of the ice enthalpy, boosting the bottom melting process, which leads to SIC decrease.