<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>
<p>June 6th<br>
</p>
<p>Shuhang (Thea) Xue: Model forecast errors in Rossby wave breaking</p>
<p>Description: Using 15-year ECMWF data, we found that there are
year-on-year and month-on-month forecast errors in global Rossby
wave breaking extents. Conditional composites show that the model
world introduces more significant errors in cyclonic wave breaking
than in anticyclonic ones globally. Results also show that the
differences between model and observation are largest around the
Pacific.
</p>
<p>Carly Narotsky: Characterizing the diurnal cycle in Florida</p>
<p>Description: Late afternoon thunderstorms are an almost-daily
occurrence in Florida summers. These routine thunderstorms
typically result from the afternoon sea breezes, a feature of the
diurnal cycle. To improve our understanding of this pattern, I aim
to characterize the phase and amplitude of the diurnal cycle
variations of 7 surface meteorology variables at 31 observational
stations in the Florida Automated Weather Network (FAWN). In this
presentation, I show preliminary results from a few FAWN stations.
The diurnal cycle analysis employs Ensemble Empirical Mode
Decomposition (EEMD) to isolate the diurnal mode of variability.
Preliminary results consistently show the famous late-afternoon
maximum in precipitation during the summer months.</p>
<br>
<p><br>
</p>
<p> </p>
<p> </p>
</body>
</html>