The PNA pattern significantly influences the temperature, precipitation, and circulation across the Northeast during the winter. Correlation coefficients range from -0.34 (Maine) to -0.64 (West Virginia) between observational mean temperature and PNA for December 1958-2000. Correlations between precipitation and PNA typically are more variable, ranging from -0.11 (Maine) to -0.65 (Michigan). The observational data therefore suggests that a positive phase of PNA typically coincides with cooler and drier conditions across the Northeast, particularly in the western side of the model domain. The SUNYA ReCM was run for ten Decembers during 1980-1999, five with the most positive PNA and five with the most negative PNA. These simulations are being composited to determine the impact of PNA on the winter climate. The results will be compared to the observational study while also gaining further insight at the regional scale.
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