Extremes of summer Arctic sea ice reduction investigated with a rare event algorithm

TL;DR

This study uses a rare event algorithm with a climate model to statistically analyze extreme Arctic sea ice reductions, revealing key preconditioning processes and improving understanding of these rare but impactful events.

Contribution

The paper applies a rare event sampling technique to a climate model to estimate the frequency and dynamics of extreme Arctic sea ice loss, overcoming computational limitations of direct sampling.

Findings

Extreme sea ice reductions are linked to winter preconditioning.

Enhanced spring atmospheric moisture and heat fluxes contribute to sea ice loss.

Sea ice-albedo feedback amplifies summer sea ice anomalies.

Abstract

Various studies identified possible drivers of extremes of Arctic sea ice reduction, such as observed in the summers of 2007 and 2012, including preconditioning, local feedback mechanisms, oceanic heat transport and the synoptic- and large-scale atmospheric circulations. However, a robust quantitative statistical analysis of extremes of sea ice reduction is hindered by the small number of events that can be sampled in observations and numerical simulations with computationally expensive climate models. Recent studies tackled the problem of sampling climate extremes by using rare event algorithms, i.e., computational techniques developed in statistical physics to reduce the computational cost required to sample rare events in numerical simulations. Here we apply a rare event algorithm to ensemble simulations with the intermediate complexity coupled climate model PlaSim-LSG to investigate extreme negative summer pan-Arctic sea ice area anomalies under pre-industrial greenhouse gas conditions. Owing to the algorithm, we estimate return times of extremes orders of magnitude larger than feasible with direct sampling, and we compute statistically significant composite maps of dynamical quantities conditional on the occurrence of these extremes. We find that extremely low sea ice summers in PlaSim-LSG are associated with preconditioning through the winter sea ice-ocean state, with enhanced downward longwave radiation due to an anomalously moist and warm spring Arctic atmosphere and with enhanced downward sensible heat fluxes during the spring-summer transition. As a consequence of these three processes, the sea ice-albedo feedback becomes active in spring and leads to an amplification of pre-existing sea ice area anomalies during summer.