Loading the field values of a variable into a vector T which dimension varies with the spatial extension of the field (e.g. model level or volume field), the field RMSE and PCC are respectively defined by,
RMSE º   æ
Ö

(Tf- ^
T
 
)T (Tf- ^
T
 
)
 
= ||Tf- ^
T
 
||2 ,     (1)
PCC =
(Tf-Tb)T ( ^
T
 
-Tb)

||Tf-Tb||2  || ^
T
 
-Tb||2
     (2)
where T (hat) denotes the true ocean, Tf its forecast, Tb a background field vector (e.g. large-scale field, climatological field), and || ·||2 the vector l2 norm.


File translated from TEX by TTH, version 2.51.
On 13 Jun 2001, 22:37.