Forcing Fields Derived from Arctic Surface Biases in CAM3 Richard Grojahn and Linlin Pan Dept. of LAWR, Univ. of California, Davis With assistance from.
The first 2 terms on the RHS are nonlinear terms in the bias. The group labeled THF are transient heat advection bias. Q^ is the bias in diabatic heating.
Forcing Fields Derived from Arctic Surface Biases in CAM3
Linear Stationary Wave ( LSW ) Model
Arctic Surface DJF Biases in CAM3 Viewed As Forcing Fields Richard Grojahn and Linlin Pan Dept. of LAWR, Univ. of California, Davis With assistance from.
