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<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>
Passcode: 478314<br>
<p>Mark Bourassa<br>
</p>
<font face="Times New Roman, Times, serif"> </font> <font face="Times New Roman, Times, serif"> April 5th </font><br>
<p><font face="Times New Roman, Times, serif">Parker Beasley: </font><font face="Times New Roman, Times, serif">Validation of IMERG
rainfall to monitor onset and demise of the rainy season over
Peninsular Florida</font></p>
<p><font face="Times New Roman, Times, serif">Description: </font><font face="Times New Roman, Times, serif">This study was motivated to
assess the fidelity of gridded, remotely sensed rainfall
analysis for real time monitoring of the wet season over the
five water management districts (WMDs) of Florida. All five WMDs
have a significant fraction of the annual rainfall occurring in
the wet season. Therefore, monitoring and anticipating its
variations from year to year would be critical to manage water
resources in the WMDs. In this study we analyzed the fidelity
of the Integrated Multi-Satellite Retrievals for Global
Precipitation Mission version 6 (IMERG) late run at 12-hour
latency and final run at 3.5-month latency with respect to the
rain gauge based analysis from the National Oceanic and
Atmospheric Administration (NOAA) Climate Prediction Center
(CPC). The 3.5-month latency product ingests a larger volume of
data for analysis and uses a more rigorous analysis technique,
which would lead to the anticipation of a better rainfall
analysis than the former 12-hour latency product.</font></p>
<p><font face="Times New Roman, Times, serif">John Uehling: TBA</font></p>
<p><font face="Times New Roman, Times, serif">Description: TBA</font></p>
<p><font face="Times New Roman, Times, serif">Yang Wang: </font><font face="Times New Roman, Times, serif">Barotropic vorticity
balance of the Ross gyre in B-SOSE data</font></p>
<p><font face="Times New Roman, Times, serif"> Description: </font><font face="Times New Roman, Times, serif">The aim of this study is to
investigate the dynamics of the Ross Gyre by analyzing the
barotropic vorticity balance. </font></p>
<p><font face="Times New Roman, Times, serif"><br>
</font></p>
<p><font face="Times New Roman, Times, serif">May 3rd<br>
</font></p>
<p><font face="Times New Roman, Times, serif">Daneisha Blair: TBA<br>
</font></p>
<p><font face="Times New Roman, Times, serif">Description: TBA<br>
</font></p>
<p><font face="Times New Roman, Times, serif">Renee Richardson: <i>A
Newly Developed Form Drag Derived from Sea Spray Influenced
Surface Wind Stress at Hurricane Force Winds</i></font> </p>
<p><font face="Times New Roman, Times, serif"> Description: Drag, or
momentum transfer, at the air-sea interface is one of the major
physical processes impacting hurricane intensity. Sea spray is
suspected of playing a major role on the drag under hurricane
wind conditions. In this study, we investigate the impact of a
newly parameterized sea spray generation mechanism on drag, as
well as total surface stress, under hurricane force winds. I
will be discussing our findings on the spray influenced surface
stresses. <br>
</font></p>
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