This talk is presented as a Zoom Webinar and requires a passcode. For anyone outside the department; If you would like to attend, email [email protected]

Assessing the predictability and probability of a summer ice-free Arctic

How predictable are future changes in Arctic sea ice, and in particular the occurrence of ice-free conditions in the summer? I will answer this question using ensemble simulations from the Community Earth System Model (CESM) forced by a range of emission pathways, resulting in global temperature changes of 1.5°C to 4.5°C above pre-industrial by the year 2100. I will show that after 2045, scenario uncertainty dominates over internal-variability uncertainty for projections of Arctic September sea ice extent. This means that for the next several decades, the sea ice evolution will be determined primarily by internal variability, superimposed upon a trend of steadily declining sea ice. At the same time, this also means that the world’s emission choices over the next few decades will have a clearly detectable effect upon the mid-to-late 21^st century Arctic sea ice cover. In particular, I will show that only by limiting warming to 1.5°C above pre-industrial, any occurrence of an ice-free Arctic in September can potentially be avoided before 2100. Warming of 4.5°C, on the other hand, will lead to ice-free summers that are four months long each year in the late 21^st century. The timing of the first occurrence of ice-free conditions, however, cannot be predicted with a range of less than 20 years due to internal variability alone, and is not sensitive to the future emission pathway as it will likely occur before scenario impacts begin to emerge.

Webinar link: https://psu.zoom.us/j/98361613108?pwd=WHNrVVBqUFpERUxraHhpVTdDTVRDQT09