Slide 1 SYNOPTIC STRUCTURE AND EVOLUTION OF A KONA LOW Steven Businger and Ian Morrison University of Hawaii Slide 2 Kona Low Kona lows are subtropical cyclones that occur…
QG Theory & Weather Systems Team 2 Alyssa Halm Matt Sanders The 850mb temperature advection corresponds quite well with the cloud pattern at 0Z. There is strong waa in…
Atmosphere Shallow Meridional Circulations: A New Mechanism for ITCZ-Cold Tongue Interaction Chidong Zhang RSMAS, University of Miami Miami, FL Equator ITCZ 1 km 10-12 km…
Andy Josh Team 5 3/31/2005 On the plots that we made we can see broad area of vertical motion caused by absolute vorticity advectionand temperature advection. Where there…
Anomalous Reintensification of (Sub)Tropical Storm Allison (2001) over Land Kwan-yin Kong and Stanley David Gedzelman EAS Department and NOAA CREST Center City College of…