《Table 2.Selected anomalous years based on the (a) Nino4 and (b) LE-SIC indices under different PDO

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《Subseasonal Reversal of East Asian Surface Temperature Variability in Winter 2014/15》

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Five datasets are used in this study:（1）NCEP atmospheric reanalysis data at a resolution of 2.5?（Kalnay et al.，1996），including sea level pressure（SLP），SAT，850-h Pa zonal and meridional wind（UV850），500-h Pa geopotential height（GPH500），and 200-h Pa zonal wind（U200）；（2）ERA-Interim data at a resolution of 2.5?（Simmons et al.，2006），including 300-h Pa zonal wind（U300）and SST；（3）ERSST.v3data at a resolution of 2.0?（Smith et al.，2008）；（4）Had ISST1data at a resolution of 1.0?（Rayner et al.，2003）；and（5）six and five models from phase 5 of the Coupled Model Intercomparison Project（CMIP5）（Table 1） ，according to the availability of output data from the historical simulations.In this paper，the observed anomalies in 2014/15 are relative to the climatology of 1979/80–2014/15.