Attributes {
    T {
        Float32 pointwidth 1.0;
        String calendar "standard";
        String standard_name "time";
        Int32 gridtype 0;
        String units "julian_day";
    }
    Y {
        String standard_name "latitude";
        Float32 pointwidth 2.5;
        String long_name "latitude";
        Int32 gridtype 0;
        String units "degree_north";
    }
    X {
        String standard_name "longitude";
        Float32 pointwidth 2.5;
        String long_name "longitude";
        Int32 gridtype 1;
        String units "degree_east";
    }
    PNA_index {
        Float32 missing_value 9.99999962E35;
        String long_name "PNA Index";
        String units "unitless";
    }
    PNA_pattern {
        Float32 missing_value 9.99999962E35;
        String long_name "PNA Loading Pattern";
        String units "m";
    }
NC_GLOBAL {
    String Conventions "IRIDL";
    String comment "The loading patterns of NAO and PNA are obtained using a rotated EOF (REOF) analysis following Barnston and Livezey (1987). The REOF is conducted for the monthly mean 500-hPa geopotential height anomalies over the Northern Hemisphere (20-90N) using the NCEP/NCAR reanalyses from 1951 to 2010. Monthly mean anomalies for all 12 calendar months and 10 rotated varimax spatial patterns are used. Since the NAO and PNA variability has the largest variance in the cold season, the patterns are thus dominated by characteristics in winter. Similar definition was used in Johansson (2007), Lin et al. (2009), and Frederiksen and Lin (2013). Analysis provided courtesy of Hai Lin (hai.lin@canada.ca) of Environment Canada.";
    String references "Barnston_Livezey1987 Frederiksen_Lin2013 Johansson2007 Lin_etal2009";
    String description "Pacific/North American";
}
}