Understanding model spread in sea ice volume by attribution of model differences in seasonal ice growth and melt

• Published in: The Cryosphere
• Main Authors: West, Alex, Blockley, Edward, Collins, Matthew
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: article; Verlagsveröffentlichung; Arctic; albedo; Sea ice; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-16-4013-2022; https://noa.gwlb.de/receive/cop_mods_00062811; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00061984/tc-16-4013-2022.pdf; https://tc.copernicus.org/articles/16/4013/2022/tc-16-4013-2022.pdf

Arctic sea ice is declining rapidly, but predictions of its future loss are made difficult by the large spread both in present-day and in future sea ice area and volume; hence, there is a need to better understand the drivers of model spread in sea ice state. Here we present a framework for understanding differences between modelled sea ice simulations based on attributing seasonal ice growth and melt differences. In the method presented, the net downward surface flux is treated as the principal driver of seasonal sea ice growth and melt. An energy balance approach is used to estimate the pointwise effect of model differences in key Arctic climate variables on this surface flux and hence on seasonal sea ice growth and melt. We compare three models with very different historical sea ice simulations: HadGEM2-ES, HadGEM3-GC3.1 and UKESM1.0. The largest driver of differences in ice growth and melt between these models is shown to be the ice area in summer (representing the surface albedo feedback) and the ice thickness distribution in winter (the thickness–growth feedback). Differences in snow and melt pond cover during the early summer exert a smaller effect on the seasonal growth and melt, hence representing the drivers of model differences in both this and in the sea ice volume. In particular, the direct impacts on sea ice growth and melt of differing model parameterisations of snow area and of melt ponds are shown to be small but non-negligible.