<html>
<head>
<meta http-equiv="Content-Type" content="text/html; charset=utf-8">
</head>
<body style="overflow-wrap: break-word; -webkit-nbsp-mode: space; line-break: after-white-space;">
<div dir="auto" style="word-wrap: break-word; -webkit-nbsp-mode: space; line-break: after-white-space;">
Dear all,
<div><br>
</div>
<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="gmail-TextRun gmail-SCXW122769022 gmail-BCX0" style="caret-color: rgba(0, 0, 0, 0.847059); 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-NormalTextRun gmail-SCXW122769022 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-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">damages</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">.</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">
While </span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">previous</span><span class="gmail-NormalTextRun gmail-SCXW122769022 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-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">In this talk, v</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">arious methodologies and datasets
are </span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">utilized</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;"> to disentangle the interwoven
factors that </span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">impact</span><span class="gmail-NormalTextRun gmail-SCXW122769022 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-NormalTextRun gmail-SCXW122769022 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-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">globally</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;"> using idealized
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">aquaplanet</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">model simulations. The idealized</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">simulations are compared to more realistic
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">global
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">model simulations and
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">satellite observations of
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">TC
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">precipitation.
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">Finally,
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">proposed</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;"> high-resolution (~1 km) limited-domain
idealized simulations </span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">with the goal of
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">explor</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">ing</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">
changes in three-dimensional </span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">TC
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">precipitation structures
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">as
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">sea surface temperatures</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">warm
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">are</span><span class="gmail-NormalTextRun gmail-SCXW122769022 gmail-BCX0" style="margin: 0px; padding: 0px;">
</span><span class="gmail-NormalTextRun gmail-SCXW122769022 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); 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>
<div>
<div dir="auto" style="caret-color: rgb(0, 0, 0); color: rgb(0, 0, 0); letter-spacing: normal; text-align: start; text-indent: 0px; text-transform: none; white-space: normal; word-spacing: 0px; -webkit-text-stroke-width: 0px; text-decoration: none; word-wrap: break-word; -webkit-nbsp-mode: space; line-break: after-white-space;">
<div style="word-wrap: break-word; -webkit-nbsp-mode: space; line-break: after-white-space;">
<div style="color: rgb(0, 0, 0); font-family: Helvetica; font-size: 12px; font-style: normal; font-variant-caps: normal; font-weight: normal; letter-spacing: normal; text-align: start; text-indent: 0px; text-transform: none; white-space: normal; word-spacing: 0px; -webkit-text-stroke-width: 0px;">
——————————————————</div>
<div style="color: rgb(0, 0, 0); font-family: Helvetica; font-size: 12px; font-style: normal; font-variant-caps: normal; font-weight: normal; letter-spacing: normal; text-align: start; text-indent: 0px; text-transform: none; white-space: normal; word-spacing: 0px; -webkit-text-stroke-width: 0px;">
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>
<div style="color: rgb(0, 0, 0); font-family: Helvetica; font-size: 12px; font-style: normal; font-variant-caps: normal; font-weight: normal; letter-spacing: normal; text-align: start; text-indent: 0px; text-transform: none; white-space: normal; word-spacing: 0px; -webkit-text-stroke-width: 0px;">
<br>
</div>
<br class="Apple-interchange-newline">
</div>
</div>
<br class="Apple-interchange-newline">
<br class="Apple-interchange-newline">
</div>
<br>
</div>
</div>
</body>
</html>