Download presentation
Presentation is loading. Please wait.
1
500 hPa height , surface pressure
2011 Feb 1 12Z Smaller scale features less evident in middle/upper troposphere
2
850 hPa , Feb 04-06 Feb 05 Feb 06 Feb 04 Svnoptic scale cyclones can develop rapidly (1-2 d.) and move generally eastward
3
02/02/2009 sfc 500 hPa Upper level trough westward of surface frontal low pressure
4
Feb Z Feb Z
5
Feb Z Feb Z
6
Jan 500 hPa climatology Quasi-stationary planetary-scale waves
7
Jan 850/500/300 hPa climatology little if any phase shift with height (in the troposphere)
8
Observed zonal mean u, T DJF JJA
9
Observed zonal mean u, T DJF tropopause JJA
10
Observed zonal mean u, T DJF JJA cold winter polar stratosphere
high, cold, tropical tropopause JJA very flat T contours in tropics
11
Observed zonal mean u, T DJF main tropospheric (subtropical) jets JJA
12
Observed zonal mean u, T DJF JJA midlatitude surface westerlies
tropical easterlies
13
Observed zonal mean u, T DJF JJA
polar night jets in winter stratosphere JJA summertime stratospheric easterlies
14
Mean meridional circulation DJF
V ~ 1 m/s
15
Mean meridional circulation DJF
Hadley cells Ferrell cells
16
Seasonal variation of the Hadley circulation
17
Different averaging approaches (Townsend & Johnson, JAS, 1985)
mass streamfunction Average at fixed p Average at fixed θ
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.