设雾 Hadley Cell Moisture effect* 10 Q=QRAD +QLh +QB 30 -1.2 0.8 NET RADIATIVE HEATING b DJF 27 (deg day-1) -0.2- 20 24F -0.8 30 21 50 qw 0.2 QRAD 18H 70 100 15 Radiative cooling, 0.8 weaker meridional variation -1.2 0 C12 400 500 -2.0 -1.61 700 0.8 850 1000 LATENT HEAT RELEASE C QLH (deg day-1) 0 100 Heating,strong meridional 0.4 150 and vertical variation 12 200 9 300 (qw] 0.8- 0.4 400 6 2.0 500 0.4- 1.61.2 2.0 700 QB c0.82 850 0 1000 500 3anss3ad BOUNDARY LAYER HEATING ò Heating,strongest at (deg day-1) 700 midlatitudes -0.4 20620.80.4 0.8. 0 X25 850 (Newell et al,1970) 0 1000 90N8070605040302010N010s2030405060708090授课教师：张洋 Q = QRAD + QLH + QB QRAD QLH QB 18 Hadley Cell : Moisture effect* http://www.adultpdf.com Created by Image To PDF trial version, to remove this mark, please register this software. Radiative cooling, weaker meridional variation Heating, strong meridional and vertical variation Heating, strongest at midlatitudes DJF (Newell et al, 1970)