Session 6 |
| Midlatitude Dynamics |
| Chair: Terry Nathan, University of California, Davis, Davis, CA
|
| 10:00 AM | 6.1 | Why is there Mid-Winter Minimum of Storm Tracks? Yi Deng, Univ of Illinois, Urbana, IL; and M. Mak |
| 10:15 AM | 6.2 | Midwinter suppression and interannual variability of the Pacific storm track: Examples of eddy-mean flow coupling? Jeffrey H. Yin, NOAA/ERL/CDC, Boulder, CO; and P. D. Sardeshmukh |
| 10:30 AM | 6.3 | Dynamics and predictability of anomalous storm tracks Prashant D. Sardeshmukh, NOAA/CIRES/CDC, Boulder, CO; and G. P. Compo |
| 10:45 AM | 6.4 | Eddy-driven jets from a mean-flow perspective Walter A. Robinson, University of Illinois, Urbana, IL |
| 11:00 AM | 6.5 | Implications of the Shape of Atmospheric Eddies Ming Cai, University of Maryland, College Park, MD; and S. Yang, H. M. van den Dool, and V. E. Kousky |
| 11:15 AM | 6.6 | The baroclinic growth/barotropic decay paradigm -- application to growth and decay of wave packets Edmund K. M. Chang, SUNY, Stony Brook, NY |