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X-WR-CALNAME;VALUE=TEXT:ClimaTea Journal Club
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SUMMARY:ClimaTea Journal Club
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 style='NewRoman";mso-ansi-language:EN-US;mso-fareast-language:EN-US;mso-bidi-language:AR-SA'><span style="mso-spacerun:yes"> </span>Stephen </span><span style='NewRoman";mso-ansi-language:EN-US;mso-fareast-language:EN-US;mso-bidi-language:AR-SA'>Bourguet</span>			</p>			<p>				<span style="color:black">Stephen will lead a discussion<strong> </strong>on the paper titled</span> <strong> <em>"<span style='NewRoman";mso-ansi-language:EN-US;mso-fareast-language:EN-US;mso-bidi-language:AR-SA'>Indian Ocean Warming Trend Reduces Pacific WarmingResponse to Anthropogenic Greenhouse Gases: An Interbasin Thermostat Mechanism"</span></em></strong>			</p>			<p>				<strong>Abstract: </strong><span><span>A greater warming trend of sea surface temperature in the tropical Indian Ocean than in the tropical Paci</span></span><span><span>fi</span></span><span><span>c is a robust feature found in various observational data sets. Yet this interbasin warming contrast is not present in climate models. Here we investigate the impact of tropical Indian Ocean warming on the tropical Paci</span></span><span><span>fi</span></span><span><span>c response to anthropogenic greenhouse gas warming by analyzing results from coupled model pacemaker experiments. We </span></span><span><span>fi</span></span><span><span>nd that warming in the Indian Ocean induces local negative sea level pressure anomalies, which extend to the western tropical Paci</span></span><span><span>fi</span></span><span><span>c, strengthening the zonal sea level pressure gradient and easterly trades in the tropical Paci</span></span><span><span>fi</span></span><span><span>c. The enhanced trade winds reduce sea surface temperature in the eastern tropical Paci</span></span><span><span>fi</span></span><span><span>c by increasing equatorial upwelling and evaporative cooling, which offset the greenhouse gas warming. This result suggests an interbasin thermostat mechanism, through which the Indian Ocean exerts its in</span></span><span><span>fl</span></span><span><span>uence on the Paci</span></span><span><span>fi</span></span><span><span>c response to anthropogenic greenhouse gas warming. </span></span>			</p>		</div>	</div></div>
LOCATION:HUCE Seminar Room MCZ 429
STATUS:CONFIRMED
DTSTART:20191112T200000Z
DTEND:20191112T200000Z
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