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X-WR-CALNAME;VALUE=TEXT:Harvard Climate Seminar
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SUMMARY:Harvard Climate Seminar
DESCRIPTION:<div>	<div>		<span style="caret-color:#000000"><span style="color:#000000"><font color="#000000"><span style="font-variant-caps:small-caps"><strong>Inez Fung</strong></span></font></span></span>	</div>	<div>		<span style="caret-color:#000000"><span style="color:#000000">Professor of Atmospheric Science</span></span>	</div>	<div>		<span style="caret-color:#000000"><span style="color:#000000">Univeristy of California, Berkeley</span></span>	</div>	<div>		 	</div>	<div>		<span style="caret-color:#000000"><span style="color:#000000"><strong><em>The Tibetan Plateau and East Asian Banded Precipitation</em></strong></span></span>	</div>	<div>		<p>			<span style="caret-color:#000000"><span style="color:#000000">The concept of the “Asian monsoon” masks the existence of two separate summer rainfall regimes: convective storms over India, Bangladesh and Nepal (the South Asian monsoon) and banded rainfall over China, Japan and Korea (East Asian monsoon). Here we focus on the East Asian summer monsoon, and present analysis of its precipitation variability over the past 50 years. Emphasis will be placed on the deflection of the jet stream downstream of the Tibetan Plateau and its role in changing precipitation patterns.</span></span>		</p>	</div></div>
LOCATION:HUCE MCZ 440
STATUS:CONFIRMED
DTSTART:20200115T170000Z
DTEND:20200115T170000Z
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