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Heavy Banded Snow
System Relative Flow / Conveyor Belts
System-Relative Flow on Isentropic Surfaces
System-Relative Flow: How can it be used?
Conveyor Belts Associated with Cyclogenesis: Standard Model
Dry Conveyor Belt
Some New Thoughts on the Conveyor Belts Associated with Cyclogenesis
Conveyor Belts Associated with a Mid-Tropospheric, Open-Wave, Weak Surface System
Conveyor Belts Associated with a Mid-Tropospheric, Closed Low, Strong Surface System
The TROWAL
What is a TROWAL
TROWAL Characteristics
TROWAL Structure
Conceptual Model of a TROWAL Associated with a Warm-Type Occlusion
Conceptual Model of a TROWAL Associated with a Cold-Type Occlusion
But...The plot thickens (or at least the clouds)
Two-Dimensional Frontogensis Function
Frontogenetical Circulation
Frontogenetical Circulation (cont.)
Emanuel's Conceptual Model of CSI-Associated Vertical Circulation
Equivalent Potential Vorticity (EPV)
Three-Dimensional Form of EPV Equation
Equivalent Potential Vorticity (EPV)
EPV Tendency Equation from Nicosia and Grumm (1999)
Nicosia and Grumm Model for EPV Reduction Near Extratropical Cyclones
A Conceptual Model: Plan View of Key Processes
A Conceptual model: Cross-sectional View of Key Processes
Southern Missouri and Illinois, 13-14 March 1999
Radar Loop
Satellite IR Loop
Satellite Water Vapor
Snowfall Totals
Surface Observations and MSL Loop
700-hPa Theta-e Loop
700-hPa Frontogenesis
600-hPa HEPV using Theta-es
13 March, Ground-Relative Streamlines and Pressure
13 March, System-Relative Streamlines and Pressure
14 March, Ground-Relative Streamlines and Pressure
14 March, System-Relative Streamlines and Pressure
Surface-500-hPa Mean Relative Humidity
Upper Midwest, 26-27 November 2001
26-27 November 2001 Snowfall Amounts
Satellite IR Loop
Surface Analysis
600-hPa Theta-e Loop
Frontogenesis at 700 and 600 hPa
600-hPa EPV and 700-500-hPa RH and Winds
Satellite Water Vapor Loop
Ground-and-System-Relative Streamlines and Pressure on 296K Surface
Ground-and-System-Relative Omega on 296K Surface
Ground-and-System-Relative Moisture Transport on 296K Surface
Satellite IR with Overlays
600-hPa Theta-e, 800h-Pa EPV, 800-600-hPa Frontogenesis, 296K S-R Streamlines
Vis5D 306K Theta-e
Summary
Conclusions
Contributors
Bibliography
System-Relative Flow on Isentropic Surfaces
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