A regime view of northern hemisphere atmospheric variability and change under global warming

The leading mode of wintertime variability in Northern Hemisphere sea level pressure (SLP) is the Arctic Oscillation (AO). It is usually obtained usin g linear principal component analysis, which produces the optimal, although somewhat restrictive, linear approximation to the SLP data. Here we use a recently introduced nonlinear principal component analysis to find the opti mal nonlinear approximation to SLP data produced by a 1001 year integration of the CCCma coupled general circulation model (CGCM1). This approximation 's associated time series is strongly bimodal and partitions the data into two distinct regimes. The first and more persistent regime describes a stan ding oscillation whose signature in the mid-troposphere is alternating ampl ification and attenuation of the climatological ridge over Northern Europe; with associated decreasing and increasing daily variance over Northern Eur asia. The second and more episodic regime describes a split-flow south of G reenland with much enhanced daily variance in the Arctic. In a 500 year int egration with atmospheric CO2 stabilized at concentrations projected for ye ar 2100, the occupation statistics of these preferred modes of variability change, such that the episodic split-flow regime occurs less frequently whi le the standing oscillation regime occurs more frequently.