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<font face="arial, sans-serif" class="">Dear all, </font></div>
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<font face="arial, sans-serif" class=""><span style="color: windowtext; white-space: pre-wrap;" class="">I</span><span style="caret-color: rgba(0, 0, 0, 0.847059); color: rgba(0, 0, 0, 0.847059); white-space: pre-wrap;" class="">’</span><span style="color: windowtext; white-space: pre-wrap;" class="">m
not sure why the formatting of the abstract was so weird. Here is another attempt:</span></font></div>
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<b class=""><font face="arial, sans-serif" class=""><span lang="EN-US" class="gmail-SCXW122769022 gmail-TextRun gmail-BCX0" style="margin: 0px; padding: 0px; line-height: 20.5042px; font-variant-ligatures: none;"><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;"><br class="">
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<b class=""><font face="arial, sans-serif" class=""><span lang="EN-US" class="gmail-SCXW122769022 gmail-TextRun gmail-BCX0" style="margin: 0px; padding: 0px; line-height: 20.5042px; font-variant-ligatures: none;"><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">TITLE:
</span></span></font></b><span style="color: windowtext;" class=""><font face="arial, sans-serif" class=""><span lang="EN-US" class="gmail-SCXW122769022 gmail-TextRun gmail-BCX0" style="margin: 0px; padding: 0px; line-height: 20.5042px; font-variant-ligatures: none;"><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">How
and Why Does Tropical Cyclone Precipitation Respond to Climate Change?</span></span><span class="gmail-EOP gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px; line-height: 20.5042px;"> </span></font></span></div>
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<font face="arial, sans-serif" class=""><b class="">ABSTRACT:</b></font></div>
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<span style="caret-color: rgba(0, 0, 0, 0.847059); color: rgba(0, 0, 0, 0.847059); white-space: pre-wrap;" class="">Tropical cyclone (TC) precipitation can create dangerous hazards and cause millions of dollars in damages. While previous 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). In this talk, various
methodologies and datasets are utilized to disentangle the interwoven factors that impact the response of TC precipitation to warming, including TC intensity, outer size, landfall frequency, and increases in atmospheric moisture. Results are first presented
for the North Atlantic and eastern United States specifically and then generalized globally using idealized aquaplanet model simulations. The idealized simulations are compared to more realistic global model simulations and satellite observations of TC precipitation.
Finally, proposed high-resolution (~1 km) limited-domain idealized simulations with the goal of exploring changes in three-dimensional TC precipitation structures as sea surface temperatures warm are discussed. </span></div>
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Allison Wing, Ph.D.<br class="">
Werner A. and Shirley B. Baum Professor<br class="">
Associate Professor, Department of Earth, Ocean and Atmospheric Science<br class="">
Florida State University<br class="">
<a href="mailto:awing@fsu.edu" class="">awing@fsu.edu</a></div>
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<div class="">On Apr 3, 2023, at 8:50 AM, eoas-seminar--- via Eoas-seminar <<a href="mailto:eoas-seminar@lists.fsu.edu" class="">eoas-seminar@lists.fsu.edu</a>> wrote:</div>
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Dear all,
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<div class="">Please join us this <b class="">Thursday April 6</b> for a Meteorology seminar, given by Dr. Alyssa Stansfield from Colorado State University. Dr. Stansfield will speak about “<i class="">How and Why Does Tropical Cyclone Precipitation Respond
to Climate Change?</i>" (abstract below).<br class="">
<br class="">
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" class="">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 class="">
<br class="">
<b style="font-size: inherit; font-family: Helvetica, Arial;" class="">If you are interested in meeting with the speaker, please contact Allison Wing.
</b><span style="font-size: inherit; font-family: Helvetica, Arial;" class="">She is available for virtual meetings between 11 AM and 3 PM.</span><br class="">
<br class="">
<b class="">DATE:</b> Thursday April 6<br class="">
<b class="">SEMINAR TIME:</b> Refreshments at 3 PM, Talk 3:15 PM - 4:15 PM. <br class="">
<b class="">SEMINAR LOCATION:</b> EOA 1044 (Speaker remote)<br class="">
<b class="">SPEAKER: </b>Dr. Alyssa Stansfield<br class="">
<br class="">
<b class="">TITLE: </b><i class="">How and Why Does Tropical Cyclone Precipitation Respond to Climate Change?</i><br class="">
<br class="">
<b class="">ABSTRACT</b><br class="">
<span lang="EN-US" class="gmail-SCXW122769022 gmail-TextRun gmail-BCX0" style="caret-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="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">Tropical
cyclone (TC) precipitation can create dangerous hazards and cause millions of dollars in
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">damages</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">.</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">
While </span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">previous</span><span class="gmail-SCXW122769022 gmail-NormalTextRun 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="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">In this talk, v</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">arious methodologies and datasets
are </span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">utilized</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;"> to disentangle the interwoven
factors that </span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">impact</span><span class="gmail-SCXW122769022 gmail-NormalTextRun 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="gmail-SCXW122769022 gmail-NormalTextRun 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="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">globally</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;"> using idealized
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">aquaplanet</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">model simulations. The idealized</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">simulations are compared to more realistic
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">global
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">model simulations and
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">satellite observations of
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">TC
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">precipitation.
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">Finally,
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">proposed</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;"> high-resolution (~1 km) limited-domain
idealized simulations </span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">with the goal of
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">explor</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">ing</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">
changes in three-dimensional </span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">TC
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">precipitation structures
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">as
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">sea surface temperatures</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">warm
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">are</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-SCXW122769022 gmail-NormalTextRun gmail-BCX0" style="margin: 0px; padding: 0px;">discussed.</span></span><span class="gmail-EOP gmail-SCXW122769022 gmail-BCX0" style="caret-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>
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<div class="">We look forward to seeing you there! </div>
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Allison Wing, Ph.D.<br class="">
Werner A. and Shirley B. Baum Professor<br class="">
Associate Professor, Department of Earth, Ocean and Atmospheric Science<br class="">
Florida State University<br class="">
<a href="mailto:awing@fsu.edu" class="">awing@fsu.edu</a></div>
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