The sensitivity of parameterization schemes in thermodynamic modeling of the landfast sea ice in Prydz Bay, East Antarctica

• Published in: Journal of Glaciology
• Main Authors: Changwei Liu, Guanghua Hao, Yubin Li, Jiechen Zhao, Ruibo Lei, Bin Cheng, Zhiqiu Gao, Qinghua Yang
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press 2022
• Subjects: Antarctic landfast sea ice; oceanic heat flux; parameterization schemes; sensitivity tests; thermodynamically modeling; Environmental sciences; GE1-350; Meteorology. Climatology; QC851-999; Antarctic; East Antarctica; Prydz Bay; Antarc*; Antarctica; Journal of Glaciology; Sea ice
• Online Access: https://doi.org/10.1017/jog.2022.8; https://doaj.org/article/e7abf1df85684181abad0aec6192c903

Based on the measurements conducted over the landfast sea ice in Prydz Bay, East Antarctica during the sea-ice growth season in 2016, various parameterization schemes in the high-resolution thermodynamic snow/ice model HIGHTSI are evaluated. The parameterization scheme of turbulent fluxes produces the largest errors compared with the parameterization schemes for other surface heat fluxes. However, the sea-ice thickness simulation is most sensitive to the differences in upward longwave radiation at the surface. In addition, the sea-ice thickness simulation during the growth season is highly sensitive to the oceanic heat flux, and a new oceanic heat flux parameterization scheme based on the bulk method is proposed. The new parameterization scheme is tested in a second year, and it significantly improves the model performance relative to the standard configuration when compared against observations. Finally, the seasonal variation in the heat budget and its influence on the sea-ice thickness variation are analyzed. The net shortwave radiation, sensible heat flux and conductive heat flux (the net longwave radiation and latent heat flux) are found to be the surface heat sources (heat sinks) during the growth season. The larger conductive heat flux and the smaller oceanic heat flux can intensify the growth of sea ice.