'Deep moist convection' presentation slideshows

4.4 Theory

4.4 Theory. 4.4 Theory (structures). African Easterly Wave trough. Peak rainfall ahead of trough. 2-3000km Wavelength. 11-12 o N. Relative Vorticity 700hPa (10 -5 s -1 ). Average precipitation rate (mm/day). 4.4 Theory (structures). Note distinctive horizontal tilts.

601 views • 46 slides

Paper by Charles A. Doswell III Powerpoint by Christopher J. Stumpf

The Distinction between Large-Scale and Mesoscale Contribution to Severe Convection: A Case Study Example. Paper by Charles A. Doswell III Powerpoint by Christopher J. Stumpf. The May 6 th 1983 Topeka, KS Tornado. A Squall line moved through on the evening of the 6 th

369 views • 30 slides

NROW XII Wednesday , 3 November 2010 Albany, NY

The Influence of the Elevated Mixed Layer on Record High Temperatures and Severe Weather Over the Northeast US in April and May 2010. Jason M. Cordeira + , Thomas J. Galarneau, Jr .*, and Lance F. Bosart + + Department of Atmospheric and Environmental Sciences

503 views • 24 slides

Paper by Charles A. Doswell III Powerpoint by Christopher J. Stumpf

The Distinction between Large-Scale and Mesoscale Contribution to Severe Convection: A Case Study Example. Paper by Charles A. Doswell III Powerpoint by Christopher J. Stumpf. Differences between Large-Scale and Mesoscale definitions and terms. Large-Scale Processes

328 views • 22 slides

Flash Flood Forecasting: An Ingredients Based Methodology

Flash Flood Forecasting: An Ingredients Based Methodology. Charles A. Doswell III, Harold E. Brooks, and Robert A. Maddox . Introduction.

399 views • 21 slides

434 views • 21 slides

Recognition of Negative Mesoscale Factors for Severe-Weather Potential- A Case Study

Recognition of Negative Mesoscale Factors for Severe-Weather Potential- A Case Study. Article By: Charles Doswell III Donald V Baker Charles A Liles Presentation By: Jason Tiffany. Introduction.

343 views • 20 slides