2008/12/27 by I. Eisenman, J. S. Wettlaufer · 1 citation
Physics and Astronomy · #physics.geo-ph #physics.ao-ph
paper · pdf · doi:10.1073/pnas.0806887106
published as Proc.Natl.Acad.Sci.USA 106 (2009) 28-32 · 11 pages with 8 figures, includes Article plus Supporting Information in a single file
arxiv created 2008/12/27 · arxiv updated 2009/12/01
In light of the rapid recent retreat of Arctic sea ice, a number of studies have discussed the possibility of a critical threshold (or "tipping point") beyond which the ice-albedo feedback causes the ice cover to melt away in an irreversible process. The focus has typically been centered on the annual minimum (September) ice cover, which is often seen as particularly susceptible to destabilization by the ice-albedo feedback. Here we examine the central physical processes associated with the transition from ice-covered to ice-free Arctic Ocean conditions. We show that while the ice-albedo feedback promotes the existence of multiple ice cover states, the stabilizing thermodynamic effects of sea ice mitigate this when the Arctic Ocean is ice-covered during a sufficiently large fraction of the year. These results suggest that critical threshold behavior is unlikely during the approach from current perennial sea ice conditions to seasonally ice-free conditions. In a further warmed climate, however, we find that a critical threshold associated with the sudden loss of the remaining wintertime-only sea ice cover may be likely.