Slow and Intraseasonal Modes of the Boreal Winter Atmospheric Circulation Simulated by CMIP5 Models  | 
	
|   Figure 1   a-c The leading three slow REOFs rotated empirical orthogonal function of the 20CR NH Northern Hemisphere 500 hPa geopotential height for DJF 1951-2000. d-f Slow SST-height covariance with HadISST The Hadley Centre Global Sea Ice and Sea Surface Temperature for the leading three slow REOFs. The estimated standard deviation m and variance explained % are given to the left of each REOF.  | 
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