设雾 Hadley Cell Role of eddies* Numerical solutions: Vallis,2006, axisymmetric numerical results from idealized GCM 0.0 40 um n uo 0.5 20 us 0 1.0 Narrower but stronger 0.0 Hadley cell 3-D flow.with eddies 40 1化m E Upper jet shifts with weakeruo 0.5 20 maximum leuoz Stronger surface winds 0 Us 1.0 60 -30 0 30 60 -60 -30 0 30 60 Latitude Latitude授课教师：张洋 10 Hadley Cell : Role of eddies* ! Numerical solutions: axisymmetric 3-D flow, with eddies Vallis, 2006, numerical results from idealized GCM Narrower but stronger Hadley cell Upper jet shifts with weaker maximum Stronger surface winds