[Eoas-seminar] TODAY: 3 PM - Baum Lecture by Dr. Kerry Emanuel (MIT)

[eoas-seminar at lists.fsu.edu]

Just a final reminder of the Baum lecture today at 3 pm in EOA 1050!

If you need a Zoom link contact Allison Wing (awing at fsu.edu<mailto:awing at fsu.edu>) before 12:30 pm. Otherwise, see you in 1050!

Cheers,

Allison

--------------------------------------------
Allison A. Wing, Ph.D.
Werner A. and Shirley B. Baum Professor
Associate Professor, Department of Earth, Ocean, and Atmospheric Science
Florida State University
awing at fsu.edu

On Nov 27, 2023, at 8:03 AM, eoas-seminar--- via Eoas-seminar <eoas-seminar at lists.fsu.edu> wrote:

Dear all,

This is a reminder to please join us for the Werner A. Baum Lecture this Friday December 1 at 3 PM in EOA 1050, to be given by distinguished climate scientist Dr. Kerry Emanuel<https://emanuel.mit.edu/>, professor emeritus at MIT. See the attached flyer for more information.

Dr. Emanuel will present “What Sets the Climatology of Severe Thunderstorms” (abstract below).

While this is intended as an in-person event, if you have a medical excuse or approved work off campus, please contact Allison Wing (awing at fsu.edu<mailto:awing at fsu.edu>) for a Zoom link.

DATE: Friday December 1
TIME: 3-4 PM
LOCATION: EOA 1050
SPEAKER: Dr. Kerry Emanuel (MIT)<https://emanuel.mit.edu/>

TITLE: What Sets the Climatology of Severe Thunderstorms

ABSTRACT: Severe convective storms are a significant source of weather-related losses and injury, worldwide. Yet very little is known about what sets their climatology in the current climate, and why climate models generally indicate increased severe storm activity as the climate warms. In this talk, I will focus on one of the main ingredients in severe convective storms: Convective Available Potential Energy (CAPE). The global climatology of CAPE differs significantly from that of deep convection in general; for example, high CAPE values are quite rare over the ocean. Using both an observational analysis and a 1-D model coupled to a model of soil and vegetation, I will argue that high CAPE results when air masses that have been significantly modified by passage over dry, lightly vegetated soils are advected over moist soils with moderate to extensive vegetation. This suggests that widespread agricultural practices may significantly modify the climatology of severe convection and points to how climate change might affect the prevalence and intensity of severe convective storms.

--------------------------------------------
Allison A. Wing, Ph.D.
Werner A. and Shirley B. Baum Professor
Associate Professor, Department of Earth, Ocean, and Atmospheric Science
Florida State University
awing at fsu.edu
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