'Level moisture' presentation slideshows

859 views • 63 slides

Richard H. Johnson Paul E. Ciesielski James H. Ruppert , Jr. Colorado State University

Moistening Processes for the October-November 2011 MJO Events. Richard H. Johnson Paul E. Ciesielski James H. Ruppert , Jr. Colorado State University Masaki Katsumata JAMSTEC, Japan Zhe Feng PNNL. Owen Shieh.

337 views • 17 slides

The Distinction Between Large-Scale and Mesoscale Contribution to Severe Convection : A Case Study Example

The Distinction Between Large-Scale and Mesoscale Contribution to Severe Convection : A Case Study Example. What Case Do We Study?. May 6 th , 1983 Event: Tornadic Severe Thunderstorm at Topeka, Kansas. What So Special about it?. F3 Tornado

372 views • 13 slides

Aerosol Impacts on Deep Convection

Aerosol Impacts on Deep Convection. Severe Storms and Tropical Cyclones. Rainfall . Having more aerosols in the atmosphere does not result in a net increase in rainfall Can lead to convective decoupling Therefore leading to a decrease in rainfall

185 views • 5 slides

Some Characteristics of Developing and Non-Developing Vorticity Maxima:

Some Characteristics of Developing and Non-Developing Vorticity Maxima: East Pacific Versus Atlantic. Brandon W. Kerns, Kantave M. Greene, Chuntao Liu, and Edward J. Zipser University of Utah, Department of Meteorology. 2. Two vorticity maxima properties that matter for each region:.

140 views • 1 slides