Slide 1Developing a new general circulation model for planetary atmospheres - how (and why!) Claire Newman Kliegel Planetary Science Seminar March 1st 2005 Slide 2 Overview…
Slide 1www.met.reading.ac.uk/~sws98slg Sting Jets in severe Northern European Windstorms Suzanne Gray, Oscar Martinez-Alvarado, Laura Baker (Univ. of Reading), Peter Clark…
Slide 1How do the clouds form? Slide 2 Water Vapor Basics (names of different phase changes, latent heat) Humidity indices (there are 6 total). Saturation vapor pressure…
Slide 1Severe Weather Part II: The Synoptic Scale Sets the Table Lab 11 Anthony R. Lupo Atms 4310 / 7310 Slide 2 Severe Weather Part II: The Synoptic Scale Sets the Table…
Slide 1The freeze-drying of ensembles of air parcels in determining stratospheric water Department of Environmental Sciences Institute of Environmental and Natural Sciences…
Slide 1Chapter 11 Imbalance and Vertical Motion Slide 2 (1) Wind-Parallel Accelerations In order for wind to flow in a cyclonically curved manner, (an acceleration) it has…
Slide 1 Updates on NOAA MM5 Assessment Where we left off Buoy assessment Temperature problems Solar radiation assessment Z T simulation Analysis nudging Where next? Slide…
Slide 1 Chapter 4 Atmospheric Circulation Slide 2 Earth Regions near the equator receive light at 90 o High latitudes receive light at low angles Slide 3 Earth Regions near…