Geofizički seminar 11.04.2018. u 13:15h

As an introduction, I will give a review of recent studies on the lead-lag interactions of Arctic and the midlatitudes with respect to sea ice, atmospheric processes, and surface climate. My own previous studies are about how November Barents sea ice anomaly is associated with lagged troposphere and surface climate later in the winter, as well as how climate conditions before November affect the November Barents sea ice. I will also show some ongoing investigation of the dominant coupled modes of sea ice-atmosphere using Maximum Covariance Analysis. Selected GCMs are also analysed similarly. It was found that the models generally overestimate the covariance for the first modes.