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X-WR-CALNAME;VALUE=TEXT:Special ClimaTea
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UID:event_1635847_0
SUMMARY:Special ClimaTea
DESCRIPTION:<div class="field field-name-body field-type-text-with-summary field-label-hidden view-mode-full">	<div class="field-items">		<div class="field-item even">			<p>				<strong>Speaker:</strong> <span class="cf0">Professor Geoffrey </span><span class="cf0">Vallis </span><a href="https://emps.exeter.ac.uk/mathematics/staff/gv219" title="">from University of Exeter </a>			</p>			<p>				<strong>Title:</strong><span><span style="color:black"> <em><strong>"Trying to Demystify Hothouse Climates"</strong></em></span></span><em><span><span style="color:black"> </span></span></em>			</p>			<p>				<span><span style="color:black"><strong>Abstract:</strong> </span></span><span><span style="color:black">Earth has gone through various periods with very warm climates and may again in the future. Although the overall temperature increases are most likely caused by very high levels of greenhouse gases, difficulties remain in understanding changes on regional and seasonal scales. In particular, the apparently very low equator-pole temperature gradient of the Eocene, and the very warm winters at high latitudes even over land surfaces, bring into question our understanding of the climate feedbacks and general circulation itself. Here we show, using an idealized numerical model in conjunction with basic physical arguments, that many of these features can be explained with plausible, known, physical processes. Although we cannot yet be certain which of these processes is dominant, and a full agreement with proxy data is elusive, it seems that we may be getting closer to a reasonable understanding. (Joint work with Matthew Henry.)</span></span>			</p>		</div>	</div></div>
LOCATION:HUCE seminar room MCZ 440
STATUS:CONFIRMED
DTSTART:20220412T160000Z
DTEND:20220412T160000Z
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