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<p class="HTMLBody" align="center" style="text-align:center"><b><u><span style="font-size:26.0pt;font-family:"Monotype Corsiva"">Meteorology Seminar<o:p></o:p></span></u></b></p>
<p class="HTMLBody" align="center" style="text-align:center"><b><span style="font-size:28.0pt;font-family:"Monotype Corsiva""><o:p> </o:p></span></b></p>
<p class="HTMLBody" align="center" style="text-align:center"><b><span style="font-size:28.0pt;font-family:"Monotype Corsiva"">Jiangmei Li</span></b><span style="font-size:28.0pt;font-family:"Monotype Corsiva""><o:p></o:p></span></p>
<p class="HTMLBody" align="center" style="text-align:center"><span style="font-size:28.0pt;font-family:"Monotype Corsiva"">M.S. Meteorology Candidate<o:p></o:p></span></p>
<p class="HTMLBody"><span style="font-size:14.0pt"><o:p> </o:p></span></p>
<p class="doublespacedcaps" align="left" style="text-align:left;line-height:normal">
<b><u><span style="font-size:14.0pt">Title</span></u>:</b> C<span style="mso-fareast-language:ZH-CN">lassification of rain clouds based on the relationship between microwave emission and scattering signals</span><span style="font-size:14.0pt;mso-fareast-language:ZH-CN"><o:p></o:p></span></p>
<p class="MsoNormal"><span style="font-size:14.0pt"><o:p> </o:p></span></p>
<p class="MsoNormal"><b><u><span style="font-size:14.0pt">Major Professor</span></u></b><b><span style="font-size:14.0pt">: Guosheng Liu</span></b><b><u><span style="font-size:14.0pt;font-family:Times"><o:p></o:p></span></u></b></p>
<p class="MsoNormal"><span style="font-size:10.0pt;font-family:"Tahoma",sans-serif;color:black"><o:p> </o:p></span></p>
<p class="MsoNormal"><b><u><span style="font-size:14.0pt">Date</span></u></b><b><span style="font-size:14.0pt">:</span></b><span style="font-size:14.0pt">
<b>March 5, 2019</b> <b><u>Time</u>: 3:30 – 5:00 PM</b></span><span style="font-size:14.0pt;font-family:"Times New Roman",serif"><o:p></o:p></span></p>
<p class="HTMLBody"><b><o:p> </o:p></b></p>
<p class="HTMLBody"><b><u><span style="font-size:14.0pt">Location</span></u></b><b><span style="font-size:14.0pt">:
</span></b><span style="font-size:14.0pt">Werner A. Baum Seminar Room (353 </span>
<span style="font-size:14.0pt">Love Building)<b><o:p></o:p></b></span></p>
<p class="MsoNormal"><b>(Please join us for refreshments served outside room 353 Love @ 3:00 PM)</b><b><span style="font-size:12.0pt"><o:p></o:p></span></b></p>
<p class="HTMLBody" style="text-autospace:ideograph-other"><span style="font-size:9.0pt"><o:p> </o:p></span></p>
<p class="MsoNormal" align="center" style="text-align:center"><b><span style="font-size:12.0pt"><o:p> </o:p></span></b></p>
<p class="MsoNormal" align="center" style="text-align:center"><b>ABSTRACT<o:p></o:p></b></p>
<p class="MsoNormal" align="center" style="text-align:center"><b><o:p> </o:p></b></p>
<p class="MsoNormal" style="text-align:justify;text-indent:20.9pt"><a name="OLE_LINK571"></a><a name="OLE_LINK2"></a><a name="OLE_LINK1"></a><a name="OLE_LINK363"></a><a name="OLE_LINK161"></a><a name="OLE_LINK160"></a><a name="OLE_LINK429"></a><a name="OLE_LINK427"></a><a name="OLE_LINK762"></a><a name="OLE_LINK761"></a><a name="OLE_LINK296"></a><a name="OLE_LINK287"></a><a name="OLE_LINK119"></a><a name="OLE_LINK120"><span style="mso-bookmark:OLE_LINK119"><span style="mso-bookmark:OLE_LINK287"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK571">In
this thesis, we introduce a new approach to classify rain clouds based on the relationship between the emission signal and scattering signal<i>
</i>derived from microwave brightness temperature data.</span></span></span></span></span></span></span></span></span></span></span></span></span></a><a name="OLE_LINK215"></a><a name="OLE_LINK216"><span style="mso-bookmark:OLE_LINK215"><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK287">
</span></span></span></span></span></span></span></span></span></span></span></span></span></a><a name="OLE_LINK368"></a><a name="OLE_LINK369"><span style="mso-bookmark:OLE_LINK368"><span style="mso-bookmark:OLE_LINK287"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK215"><span style="mso-bookmark:OLE_LINK216">Two
parameters are used as indicators of emission signal and scattering signal respectively:</span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></a><a name="OLE_LINK585"></a><a name="OLE_LINK586"><span style="mso-bookmark:OLE_LINK585"><span style="mso-bookmark:OLE_LINK216"><span style="mso-bookmark:OLE_LINK215"><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK287"><span style="mso-bookmark:OLE_LINK368"><span style="mso-bookmark:OLE_LINK369">
</span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></a><a name="OLE_LINK584"></a><a name="OLE_LINK583"><span style="mso-bookmark:OLE_LINK584"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK368"><span style="mso-bookmark:OLE_LINK287"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK215"><span style="mso-bookmark:OLE_LINK216"><span style="mso-bookmark:OLE_LINK585"><span style="mso-bookmark:OLE_LINK586">one
is </span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></a><a name="OLE_LINK983"></a><a name="OLE_LINK984"><span style="mso-bookmark:OLE_LINK983"><span style="mso-bookmark:OLE_LINK586"><span style="mso-bookmark:OLE_LINK585"><span style="mso-bookmark:OLE_LINK216"><span style="mso-bookmark:OLE_LINK215"><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK287"><span style="mso-bookmark:OLE_LINK368"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK584"><span style="mso-bookmark:OLE_LINK583">the
polarization difference (<i>D</i>)</span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></a><span style="mso-bookmark:OLE_LINK586"><span style="mso-bookmark:OLE_LINK585"><span style="mso-bookmark:OLE_LINK216"><span style="mso-bookmark:OLE_LINK215"><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK287"><span style="mso-bookmark:OLE_LINK368"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK584"><span style="mso-bookmark:OLE_LINK583">
at 19 GHz, and the other one is <a name="OLE_LINK985"></a><a name="OLE_LINK986"><span style="mso-bookmark:OLE_LINK985">the polarization-corrected temperature</span></a> (<i>PCT</i>) at high-frequencies channels.</span></span>
</span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK287"><span style="mso-bookmark:OLE_LINK368"><span style="mso-bookmark:OLE_LINK369"><i>D</i>
</span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK296"><span style="mso-bookmark:OLE_LINK287"><span style="mso-bookmark:OLE_LINK368"><span style="mso-bookmark:OLE_LINK369">is
related to the emission of liquid hydrometeors, and <i>PCT</i> mainly reflects the brightness temperature depression due to the scattering by ice particles. Both
<i>D</i> and <i>PCT</i> decrease with increasing precipitation rate. </span></span></span></span><a name="OLE_LINK297"></a><a name="OLE_LINK300"></a><a name="OLE_LINK351"></a><a name="OLE_LINK426"></a><a name="OLE_LINK217"></a><a name="OLE_LINK218"></a><a name="OLE_LINK284"></a><a name="OLE_LINK285"></a><a name="OLE_LINK286"><span style="mso-bookmark:OLE_LINK285"><span style="mso-bookmark:OLE_LINK284"><span style="mso-bookmark:OLE_LINK218"><span style="mso-bookmark:OLE_LINK217"><span style="mso-bookmark:OLE_LINK426"><span style="mso-bookmark:OLE_LINK351"><span style="mso-bookmark:OLE_LINK300"><span style="mso-bookmark:OLE_LINK297"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK368">Therefore,
certain combinations of <i>D</i> and <i>PCT</i> can be regarded as the representatives of cloud hydrometeor structures.</span></span></span></span></span></span></span></span></span></span></a><span style="mso-bookmark:OLE_LINK284"><span style="mso-bookmark:OLE_LINK218"><span style="mso-bookmark:OLE_LINK217"><span style="mso-bookmark:OLE_LINK426"><span style="mso-bookmark:OLE_LINK351"><span style="mso-bookmark:OLE_LINK300"><span style="mso-bookmark:OLE_LINK297"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK368">
</span></span></span></span></span></span></span></span></span><span style="mso-bookmark:OLE_LINK426"><span style="mso-bookmark:OLE_LINK351"><span style="mso-bookmark:OLE_LINK300"><span style="mso-bookmark:OLE_LINK297"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK368">Based
on the <i>D</i>-<i>PCT</i> relationship investigated in this study, we classified the observed rain clouds into five categories—non-precipitating, light-precipitating, liquid-dominant precipitating, well-mix precipitating, and ice-dominant precipitating cloud.</span></span></span></span></span></span><span style="mso-bookmark:OLE_LINK300"><span style="mso-bookmark:OLE_LINK297"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK368">
</span></span></span></span></span></span></span></span></span></span></span></span></span></span><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK762"><span style="mso-bookmark:OLE_LINK761"><span style="mso-bookmark:OLE_LINK300"><span style="mso-bookmark:OLE_LINK297"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK368"><span style="font-family:SimSun"><o:p></o:p></span></span></span></span></span></span></span></span></span></span></span></span></span></span></span></p>
<span style="mso-bookmark:OLE_LINK761"></span><span style="mso-bookmark:OLE_LINK762"></span>
<p class="MsoNormal" style="text-align:justify;text-indent:20.9pt"><span style="mso-bookmark:OLE_LINK571"><span style="mso-bookmark:OLE_LINK2"><span style="mso-bookmark:OLE_LINK1"><span style="mso-bookmark:OLE_LINK363"><span style="mso-bookmark:OLE_LINK161"><span style="mso-bookmark:OLE_LINK160"><span style="mso-bookmark:OLE_LINK429"><span style="mso-bookmark:OLE_LINK427"><span style="mso-bookmark:OLE_LINK300"><span style="mso-bookmark:OLE_LINK297"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK368"><a name="OLE_LINK763"></a><a name="OLE_LINK565"></a><a name="OLE_LINK430"></a><a name="OLE_LINK566"></a><a name="OLE_LINK576"><span style="mso-bookmark:OLE_LINK566"><span style="mso-bookmark:OLE_LINK430"><span style="mso-bookmark:OLE_LINK565"><span style="mso-bookmark:OLE_LINK763">We
verified the results of the classification of different precipitation cases over tropical regions.
</span></span></span></span></a></span></span></span></span></span></span><span style="mso-bookmark:OLE_LINK300"><span style="mso-bookmark:OLE_LINK297"><span style="mso-bookmark:OLE_LINK369"><span style="mso-bookmark:OLE_LINK368"><span style="mso-bookmark:OLE_LINK430"><span style="mso-bookmark:OLE_LINK565"><span style="mso-bookmark:OLE_LINK763">For
both the hurricane and front cases, the results show that the distributions of categorized cloud pixels can reflect the horizontal structure of the weather systems.
</span></span></span></span></span><a name="OLE_LINK352"></a><a name="OLE_LINK353"><span style="mso-bookmark:OLE_LINK352"><span style="mso-bookmark:OLE_LINK763"><span style="mso-bookmark:OLE_LINK565"><span style="mso-bookmark:OLE_LINK430">The monthly gridded
mean frequencies of categorized precipitating clouds are used to analyze the relationship between the seasonal and interannual cycles of tropical precipitation and clouds’ hydrometeor components.</span></span></span></span></a></span></span><span style="mso-bookmark:OLE_LINK353"><span style="mso-bookmark:OLE_LINK352"><span style="mso-bookmark:OLE_LINK763"><span style="mso-bookmark:OLE_LINK565"><span style="mso-bookmark:OLE_LINK430">
<a name="OLE_LINK356"></a><a name="OLE_LINK357"></a><a name="OLE_LINK358"></a><a name="OLE_LINK359"></a><a name="OLE_LINK360"></a><a name="OLE_LINK354"></a><a name="OLE_LINK355"><span style="mso-bookmark:OLE_LINK354"><span style="mso-bookmark:OLE_LINK360"><span style="mso-bookmark:OLE_LINK359"><span style="mso-bookmark:OLE_LINK358"><span style="mso-bookmark:OLE_LINK357"><span style="mso-bookmark:OLE_LINK356">Moreover,
the results indicated that in an annual cycle or an ENSO cycle, when the local precipitation frequencies increase, the occurrence frequencies of all kinds of rain clouds will increase. However, among those precipitating systems, the proportions of ice-dominant
and well-mixed clouds increases while that of water-dominant clouds decrease as the local precipitation increas</span></span></span></span></span></span></a><span style="mso-bookmark:OLE_LINK360"><span style="mso-bookmark:OLE_LINK359"><span style="mso-bookmark:OLE_LINK358"><span style="mso-bookmark:OLE_LINK357"><span style="mso-bookmark:OLE_LINK356">es.</span></span></span></span></span><span style="mso-bookmark:OLE_LINK357"><span style="mso-bookmark:OLE_LINK356">
Anomalies of the opposite sign tend to accompany the decreasing precipitations situations.</span></span></span></span></span></span></span></span></span></span><span style="mso-bookmark:OLE_LINK763"><span style="mso-bookmark:OLE_LINK565"><span style="mso-bookmark:OLE_LINK430">
</span></span></span><a name="OLE_LINK579"></a><a name="OLE_LINK580"></a><a name="OLE_LINK587"></a><a name="OLE_LINK588"><span style="mso-bookmark:OLE_LINK587"><span style="mso-bookmark:OLE_LINK580"><span style="mso-bookmark:OLE_LINK579">Overall, the classification
method proves to be useful to extract objective information from observed emission and scattering signals.
</span></span></span></a></span></span></span><span style="mso-bookmark:OLE_LINK579"></span><span style="mso-bookmark:OLE_LINK580"></span><span style="mso-bookmark:OLE_LINK587"></span><span style="mso-bookmark:OLE_LINK588"></span><span style="mso-bookmark:OLE_LINK1"></span><span style="mso-bookmark:OLE_LINK2"></span><span style="mso-bookmark:OLE_LINK571"></span><span style="font-family:"Times New Roman",serif"><o:p></o:p></span></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal">Shel McGuire<o:p></o:p></p>
<p class="MsoNormal">Florida State University<o:p></o:p></p>
<p class="MsoNormal">Academic Program Specialist<o:p></o:p></p>
<p class="MsoNormal">Department of Earth, Ocean, & Atmospheric Science<o:p></o:p></p>
<p class="MsoNormal">1017 Academic Way, 410 Love Building (Meteorology)<o:p></o:p></p>
<p class="MsoNormal">Tallahassee, FL 32306<o:p></o:p></p>
<p class="MsoNormal">850-644-8582<o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
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