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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>Jan. 10th<br>
</p>
<p>John Paul Irving: Quantifying the sequestration time of
remineralized carbon dioxide in the California current ecosystem
for different carbon flux plathways</p>
<div>
<div>Description: <span style="caret-color: rgb(255, 255, 255);
font-family: Calibri, Arial, Helvetica, sans-serif; display:
inline !important;">Within the California Current Ecosystem
particulate organic carbon (POC) vertically migrates based on
different export pathways; sinking, subduction, and active
transport. These various export pathways influence the depth
of remineralization, a process in which heterotrophic
zooplankton and bacteria utilize POC and release CO2 as a
product of respiration. To quantify the sequestration time of
this CO2 within the ocean a lagrangian patricle tracking
simulation was conducted using the MITgcm Floats Package and
HYCOM reanalysis data. Magnitudes of sequestration are then
calculated for the different carbon flux pathways based on
sequestration time scales and remineralization rates of the
different export flux pathways.</span></div>
<br>
</div>
<p>Shawn Smith: The MarineFlux Project.<br>
</p>
<p>Description: TBD<br>
</p>
<p>Mark Bourassa: <i></i>Butterfly - a NASA proposal to measure
air-sea fluxes. <br>
</p>
<p>Description: Butterfly is a proposed NASA satellite-based mission
to more accurate determine air-sea turbulent heat fluxes at
relatively fine resolution. The mission concept will be outlined.
<br>
</p>
<p> </p>
<p> </p>
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