E-P flux in the real atmosphere *01Ik F三-u*v*]j+f0e/ap F=cgA E-P FLUX 1 TRANSIENT EDDIES (a) 5×1015 () -+1.25×1015 DJF JJA 2 2 -1 3 A 1u. 1-4 6 5tN11:: 6 7 -2111N+, 11111 9 8 9 10 10 10 1020 30 40 5060 7080N 10 20 30 4050 60 70 80N 授课教师：张洋8
http://www.adultpdf.com Created by Image To PDF trial version, to remove this mark, please register this software. 授课教师：张洋 8 F ⌘ [u⇤v⇤] j + f [v⇤✓⇤] @✓s/@p k E-P flux - in the real atmosphere F ~ = c ~ gA
E-P flux in the real atmosphere u*91k 下≡-u**]j+f0e/n 于=cgA E-P FLUX TRANSIENT EDDIES (a) 5×1015 () -+1.25×1015 DJF JJA Vertical component 2 2 is dominant. -1 3 1-4 5 人 ,51t1141: 6 7 -2111H+, 11111 9 8 9 10 10 10 1020 30 40 5060 7080N 1020 3040 50 60 70 80N 授课教师：张洋8
http://www.adultpdf.com Created by Image To PDF trial version, to remove this mark, please register this software. 授课教师：张洋 8 F ⌘ [u⇤v⇤] j + f [v⇤✓⇤] @✓s/@p k E-P flux - in the real atmosphere F ~ = c ~ gA Vertical component is dominant
E-P flux in the real atmosphere U*01k 下≡-u**1j+f∂0e/p F=CgA E-P FLUX TRANSIENT EDDIES (a) 5×1015 () +1.25×1015 DJF JJA Vertical component 2 is dominant. ×<\111-1 3 3 EP divergence in 旦 、1，. 1-4 the lower layers; 5 convergence in the 人 511Nt11,: 6 upper layers. -211N1+, 8 9 9 10 a10 10 1020 30 40 50607080N 1020 304050 60 70 80N 授课教师：张洋8
http://www.adultpdf.com Created by Image To PDF trial version, to remove this mark, please register this software. 授课教师：张洋 8 F ⌘ [u⇤v⇤] j + f [v⇤✓⇤] @✓s/@p k E-P flux - in the real atmosphere F ~ = c ~ gA Vertical component is dominant. EP divergence in the lower layers; convergence in the upper layers
及金乐 E-P flux and the eddy-driven jet -summary *01k 下=-w产*]j+fo0./p 子=cgA =f网+V.F+E 授课教师：张洋9
授课教师：张洋 9 F ~ = c ~ gA @[u] @t = f ˜[v] + r · F + [Fx] F ⌘ [u⇤v⇤] j + f [v⇤✓⇤] @✓s/@p k E-P flux and the eddy-driven jet -summary
E-P flux and the eddy-driven jet -summary *01k 下=-[w**1j+fa0a/p F=CgA Numerical results and observations:eddies generate in the lower level, propagate upwards and away from the eddy source region. olu=fF) at 授课教师：张洋9
授课教师：张洋 9 F ~ = c ~ gA @[u] @t = f ˜[v] + r · F + [Fx] F ⌘ [u⇤v⇤] j + f [v⇤✓⇤] @✓s/@p k E-P flux and the eddy-driven jet -summary • Numerical results and observations: eddies generate in the lower level, propagate upwards and away from the eddy source region