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Dear all, </div>
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This is a friendly reminder of today's MET seminar, given by Dr. Alyssa Stansfield from Colorado State University on "<i>How and Why Does Tropical Cyclone Precipitation Respond to Climate Change?". </i></div>
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Snacks at 3, talk at 3:15 in 1044 (speaker remote). </div>
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See you there!</div>
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Cheers, </div>
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Allison</div>
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<div id="divRplyFwdMsg" dir="ltr"><font face="Calibri, sans-serif" style="font-size:11pt" color="#000000"><b>From:</b> Eoas-seminar <eoas-seminar-bounces@lists.fsu.edu> on behalf of eoas-seminar--- via Eoas-seminar <eoas-seminar@lists.fsu.edu><br>
<b>Sent:</b> Monday, April 3, 2023 8:50 AM<br>
<b>To:</b> eoas-seminar--- via Eoas-seminar <eoas-seminar@lists.fsu.edu><br>
<b>Subject:</b> [Eoas-seminar] MET Seminar - This Thursday April 6 - Dr. Alyssa Stansfield (Colorado State University)</font>
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<div dir="auto" style="word-wrap:break-word; line-break:after-white-space">Dear all,
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<div>Please join us this <b>Thursday April 6</b> for a Meteorology seminar, given by Dr. Alyssa Stansfield from Colorado State University. Dr. Stansfield will speak about “<i>How and Why Does Tropical Cyclone Precipitation Respond to Climate Change?</i>" (abstract
below).<br>
<br>
Dr. Stansfield will be joining us virtually but we will gather in EOA 1044 to participate in the seminar. If you cannot attend in person due to a medical reason or approved work out of town, please contact Allison Wing (<a href="mailto:awing@fsu.edu">awing@fsu.edu</a>)
for remote access. Otherwise, we look forward to seeing everyone in 1044! Please join us for refreshments prior to the beginning of the talk at 3:15 PM. <br>
<br>
<b style="font-size:inherit; font-family:Helvetica,Arial">If you are interested in meeting with the speaker, please contact Allison Wing.
</b><span style="font-size:inherit; font-family:Helvetica,Arial">She is available for virtual meetings between 11 AM and 3 PM.</span><br>
<br>
<b>DATE:</b> Thursday April 6<br>
<b>SEMINAR TIME:</b> Refreshments at 3 PM, Talk 3:15 PM - 4:15 PM. <br>
<b>SEMINAR LOCATION:</b> EOA 1044 (Speaker remote)<br>
<b>SPEAKER: </b>Dr. Alyssa Stansfield<br>
<br>
<b>TITLE: </b><i>How and Why Does Tropical Cyclone Precipitation Respond to Climate Change?</i><br>
<br>
<b>ABSTRACT</b><br>
<span lang="EN-US" class="x_gmail-TextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="color:rgba(0,0,0,0.847059); font-family:arial,sans-serif; white-space:pre-wrap; margin:0px; padding:0px; line-height:20.5042px; font-variant-ligatures:none"><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">Tropical
cyclone (TC) precipitation can create dangerous hazards and cause millions of dollars in
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">damages</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">.</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">
While </span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">previous</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px"> literature agrees that
future TC precipitation will increase due to rising global temperatures, the estimates of how much it will increase vary, ranging from around 3 to 20% per °C of warming, or three times the Clausius-Clapeyron scaling (about 7% per °C).</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">In this talk, v</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">arious methodologies and
datasets are </span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">utilized</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px"> to disentangle
the interwoven factors that </span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">impact</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px"> the
response of TC precipitation to warming, including TC intensity, outer size, landfall frequency, and increases in atmospheric moisture.
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">Results are first presented for the North Atlantic and eastern United States specifically and then generalized
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">globally</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px"> using idealized
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">aquaplanet</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">model simulations. The idealized</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">simulations are compared to more realistic
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">global
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">model simulations and
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">satellite observations of
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">TC
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">precipitation.
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">Finally,
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">proposed</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px"> high-resolution (~1 km) limited-domain
idealized simulations </span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">with the goal of
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">explor</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">ing</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">
changes in three-dimensional </span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">TC
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">precipitation structures
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">as
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">sea surface temperatures</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">warm
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">are</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">
</span><span class="x_gmail-NormalTextRun x_gmail-SCXW122769022 x_gmail-BCX0" style="margin:0px; padding:0px">discussed.</span></span><span class="x_gmail-EOP x_gmail-SCXW122769022 x_gmail-BCX0" style="color:rgba(0,0,0,0.847059); font-family:arial,sans-serif; white-space:pre-wrap; margin:0px; padding:0px; line-height:20.5042px"> </span></div>
<div><br>
</div>
<div>We look forward to seeing you there! </div>
<div><br>
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Allison Wing, Ph.D.<br>
Werner A. and Shirley B. Baum Professor<br>
Associate Professor, Department of Earth, Ocean and Atmospheric Science<br>
Florida State University<br>
awing@fsu.edu</div>
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