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Good morning all,</div>
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This is a reminder for the COAPS didactics today. </div>
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There will be a slight delay of 15 minutes requested by Dr. Caroline Muller. So we
<b>will begin at 10:15 AM</b> and end at 11 AM.</div>
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<u>The talk will be recorded</u> and uploaded to COAPS youtube channel. I'll share the link soon!</div>
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<div id="x_divRplyFwdMsg" dir="ltr"><font face="Calibri, sans-serif" color="#000000" style="font-size:11pt"><b>From:</b> Keshav Raja <kraja@fsu.edu><br>
<b>Sent:</b> Thursday, January 12, 2023 11:00<br>
<b>To:</b> eoas-seminar@lists.fsu.edu <eoas-seminar@lists.fsu.edu>; JESfwd-fsu-sc-4th-floor <4th-floor@sc.fsu.edu><br>
<b>Subject:</b> COAPS didactics - Dr. Caroline Muller</font>
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We are starting a new seminar series this year at COAPS! The goals of these <i>didactic sessions</i> are to get an overview on a topic, learn something new and start a discussion, in the hopes that these would lead to novel ideas and collaborations. </div>
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For the month of January, Dr. Caroline Muller (Assistant Professor, Institute of Science and Technology Austria; CNRS researcher) will be speaking about Spontaneous Aggregation of Convective Storms. </div>
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<div class="x_x_x_ContentPasted0" style="text-align:center">Time: <span style="font-size:12pt">
<b>Jan 24, 2023 10:15 AM EST</b></span></div>
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<div style="text-align:center">Join from anywhere on Zoom: <a href="https://urldefense.com/v3/__https://fsu.zoom.us/j/9206782375__;!!PhOWcWs!xDSz5b-B5uF6c8cd5PhpQSnbc-rzeq428TpTZNB2nNcZFpdjTm4LFNQLw4sM0MAmeKlqj_eqqD8JPQ$" data-auth="NotApplicable" id="LPNoLPOWALinkPreview">https://fsu.zoom.us/j/9206782375</a></div>
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<div class="x_x_x_ContentPasted0">Meeting ID: 920 678 2375<br>
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<div style="text-align:center"><span style="color:rgb(23,78,134); font-size:18pt"><b>Spontaneous Aggregation of Convective Storms</b><br>
</span><span style="color:rgb(0,36,81); font-size:14pt">Dr. Caroline Muller</span></div>
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<div style="text-align:left"><span style="color:rgb(36,36,36); font-size:15px">Idealized simulations of the tropical atmosphere have predicted that clouds can spontaneously clump together in space, despite perfectly homogeneous settings. This phenomenon has
been called self-aggregation, and it results in a state where a moist cloudy region with intense deep convective storms is surrounded by extremely dry subsiding air devoid of deep clouds. Here we review the main findings from theoretical work and idealized
models of this phenomenon, highlighting the physical processes believed to play a key role in convective self-aggregation. We also review the growing literature on the importance and implications of this phenomenon for the tropical atmosphere, notably, for
the hydrological cycle and for precipitation extremes, in our current and in a warming climate.</span></div>
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<div style="text-align:left">Best,</div>
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<div><span style="font-family:Calibri,Arial,Helvetica,sans-serif; font-size:12pt">Keshav J Raja</span></div>
<div style="font-family:Calibri,Arial,Helvetica,sans-serif; font-size:12pt">Assistant Research Scientist</div>
<div style="font-family:Calibri,Arial,Helvetica,sans-serif; font-size:12pt">Center for Ocean-Atmospheric Prediction Studies (COAPS)</div>
<span style="font-family:Calibri,Arial,Helvetica,sans-serif; font-size:12pt">Florida State University</span></div>
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