NCL Home> Application examples> Non-uniform grids || Data files for some examples

Example pages containing: tips | resources | functions/procedures

NCL: Equivalent Latitudes

Equivalent latitude is often used when analyzing potential vorticity (PV) and polar vortex behavior. The edge of the vortex is defined as the maximum first derivative of PV with respect to equivalent latitude. You can use NCL's triangular mesh capability to directly contour equivalent latitudes which are function of time and longitude.

Bodecker Scientific provides a tutorial of how to compute equivalent latitude from potential vorticity.

For more information on non-uniform grids that NCL can handle, see the document "Non-uniform grids that NCL can contour."

equiv_lat_1.ncl: The file looks like

        double time(time) ;
                time:units = "days as %Y%m%d.%f" ;
        double lat(lat) ;
                lat:long_name = "latitude" ;
                lat:units = "degrees_north" ;
                lat:standard_name = "latitude" ;
        double lon(lon) ;
                lon:long_name = "longitude" ;
                lon:units = "degrees_east" ;
                lon:standard_name = "longitude" ;

        float vortpot_0600K(time, lat, lon) ;
                vortpot_0600K:long_name = "potential vorticity on 0600K surfaceP" ;
                vortpot_0600K:units = "K m2 kg-1 s-1" ;

        float eqlat_0600K(time, lat, lon) ;
                eqlat_0600K:long_name = "equivalent latitude on 0600K surfaceP" ;
                eqlat_0600K:units = "degrees_north" ;

The eqlat_0600K variable is a function of (time, lat, lon). The lat/lon information must be provided by setting the resources sfXArray and sfYArray. Further, the data array must be one-dimensional (use ndtooned).