<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>August 1st:</p>
<p><!--[if gte mso 9]><xml>
<o:OfficeDocumentSettings>
<o:AllowPNG/>
</o:OfficeDocumentSettings>
</xml><![endif]--></p>
<p><!--[if gte mso 9]><xml>
<w:WordDocument>
<w:View>Normal</w:View>
<w:Zoom>0</w:Zoom>
<w:TrackMoves/>
<w:TrackFormatting/>
<w:PunctuationKerning/>
<w:ValidateAgainstSchemas/>
<w:SaveIfXMLInvalid>false</w:SaveIfXMLInvalid>
<w:IgnoreMixedContent>false</w:IgnoreMixedContent>
<w:AlwaysShowPlaceholderText>false</w:AlwaysShowPlaceholderText>
<w:DoNotPromoteQF/>
<w:LidThemeOther>EN-ID</w:LidThemeOther>
<w:LidThemeAsian>X-NONE</w:LidThemeAsian>
<w:LidThemeComplexScript>X-NONE</w:LidThemeComplexScript>
<w:Compatibility>
<w:BreakWrappedTables/>
<w:SnapToGridInCell/>
<w:WrapTextWithPunct/>
<w:UseAsianBreakRules/>
<w:DontGrowAutofit/>
<w:SplitPgBreakAndParaMark/>
<w:EnableOpenTypeKerning/>
<w:DontFlipMirrorIndents/>
<w:OverrideTableStyleHps/>
</w:Compatibility>
<m:mathPr>
<m:mathFont m:val="Cambria Math"/>
<m:brkBin m:val="before"/>
<m:brkBinSub m:val="--"/>
<m:smallFrac m:val="off"/>
<m:dispDef/>
<m:lMargin m:val="0"/>
<m:rMargin m:val="0"/>
<m:defJc m:val="centerGroup"/>
<m:wrapIndent m:val="1440"/>
<m:intLim m:val="subSup"/>
<m:naryLim m:val="undOvr"/>
</m:mathPr></w:WordDocument>
</xml><![endif]--></p>
<p>Elok Wulandari:Characteristics of low level wind shear and wind
profiler based alerting in Bali, Indonesia<br>
</p>
<p>We review and analyze wind shear warnings given by Wind Profiler
data and find the characteristic of wind shear in International
Airport Ngurah Rai Bali. Using at least the Bulk Richardson
number, we will try to find the pattern before the wind shear
event happens. Preliminary result shows that most of the wind
shear happened between value -0.25 – 0.25.</p>
<p><!--[if gte mso 10]>
<style>
/* Style Definitions */
table.MsoNormalTable
{mso-style-name:"Table Normal";
mso-tstyle-rowband-size:0;
mso-tstyle-colband-size:0;
mso-style-noshow:yes;
mso-style-priority:99;
mso-style-parent:"";
mso-padding-alt:0in 5.4pt 0in 5.4pt;
mso-para-margin-top:0in;
mso-para-margin-right:0in;
mso-para-margin-bottom:8.0pt;
mso-para-margin-left:0in;
line-height:107%;
mso-pagination:widow-orphan;
font-size:11.0pt;
font-family:"Calibri",sans-serif;
mso-ascii-font-family:Calibri;
mso-ascii-theme-font:minor-latin;
mso-hansi-font-family:Calibri;
mso-hansi-theme-font:minor-latin;
mso-bidi-font-family:"Times New Roman";
mso-bidi-theme-font:minor-bidi;
mso-ansi-language:EN-ID;}
</style>
<![endif]--></p>
<p>Opeyemi Kehinde: Lateral advection of Particulate organic carbon
in the eastern Indian Ocean</p>
<p>A small oligotrophic Agro basin, near Java and northwest of
Australia in the eastern Indian is the only known spawning region
for Southern Bluefin Tuna (SBT). Nutrients supports Phytoplankton
at the base of the ecosystem, that indirectly supports SBT larvae
growth and development. Therefore, much attention must be paid to
the nutrient supply and how they are been supplied, into this
oligotrophic region. This talk will discuss how much Lateral
advection is contributing to the total new production of
Particulate organic Carbon that supports this ecosystem.</p>
<p> </p>
<p> Keshav J Raja: Wind-generated near-inertial waves in global
ocean simulations</p>
<p>Surface winds in oceans excite near-inertial oscillations with
clockwise (anticlockwise) rotational motion in the Northern
(Southern) Hemisphere. These oscillations cause vertical motions
at the base of the mixed layer and generate near-inertial internal
waves in the ocean interior. It is thought that near-inertial
waves contribute about 25% of the energy for global ocean mixing
through turbulence resulting from their strong vertical shear and
breaking in the upper ocean. In this talk, we use global HYCOM
simulations to examine how much energy is transferred from winds
to surface near-inertial motions, how this energy propagates
horizontally, and where do they dissipate in the global ocean.</p>
<p><br>
</p>
<p> </p>
<p> </p>
</body>
</html>