<html><head>
<meta http-equiv="Content-Type" content="text/html; charset=utf-8">
</head>
<body text="#000000" bgcolor="#FFFFFF">
<font face="Times New Roman, Times, serif">These talks are usually
scheduled for the first Monday of each month. The first talk
normally starts at 11:00AM. Each talk is typically 12 minutes
long (similar to many professional meetings), with 8 minutes for
questions.</font><br>
<p><font face="Times New Roman, Times, serif">These talks will be
presented via Zoom, with the following connection information:</font><br>
</p>
<font face="Times New Roman, Times, serif"> </font><a class="moz-txt-link-freetext" href="https://fsu.zoom.us/j/98491660566?pwd=NzBxNzN4LzdsbSs4R3B6RzliOGhhdz09" moz-do-not-send="true">https://fsu.zoom.us/j/98491660566?pwd=NzBxNzN4LzdsbSs4R3B6RzliOGhhdz09</a><br>
<br>
Meeting ID: 984 9166 0566<br>
<p> Passcode: 478314</p>
Nov. 7th
<p>Joanna Rodgers: <span style="color:black;
font-family:Calibri,Arial,Helvetica,sans-serif; font-size:12pt">Monitoring
the onset and demise of rainfall over Central America using
IMERG rainfall.</span></p>
<p><span style="font-family: Calibri, sans-serif; font-weight: 400;">Using
IMERG rainfall data, the onset and the demise of the rainy
season over Central America will be characterized. Methods to be
used include those developed by Dr. Misra </span><span style="font-family: Calibri, sans-serif; font-weight: 400;">and
outlined in his previous papers but will be applied to the
Central America region. By characterizing the typical season,
trends in early or late onset dates may reveal </span><span style="font-family: Calibri, sans-serif; font-weight: 400;">significant
insights into what to expect for the following rainy season.</span><span style="color:black;
font-family:Calibri,Arial,Helvetica,sans-serif; font-size:12pt"></span></p>
<p>Tony Freveletti: Characterizing the diurnal variability of
convectively available potential energy and convective inhibition
in the Southeastern United States</p>
<p>10 years of CAPE and CIN values have been computed every day at
3-hour intervals from the FLAReS1.0 dataset. Using these values an
empirical ensemble mode decomposition (EEMD) analysis will be done
to characterize diurnal variability on the diurnal, semi-diurnal,
and seasonal scales.<font style="font-size:11pt" face="Calibri,
sans-serif" color="#000000"> </font></p>
<p>Dec. 5th</p>
<p>Carly Narotsky: TBA</p>
<p>TBA: TBA</p>
<p>Shawn Smith: The MarineFlux project<br>
</p>
<p> </p>
<p> </p>
</body>
</html>