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        <p>Our next speaker in the<span> </span><span data-markjs="true" class="markysf22eeiy" data-ogac="" data-ogab="" data-ogsc="" data-ogsb="" style="margin: 0px">EOAS</span><span> </span><span data-markjs="true" class="markmhgzrwsdl" data-ogac="" data-ogab="" data-ogsc="" data-ogsb="" style="margin: 0px">Colloquium</span><span>
            TODAY</span> at 3:30 pm will be<br>
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        <p><font size="+2">Dr. Shineng Hu </font>of the Columbia
          University / Duke University</p>
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        <p class="x_MsoNormal" style="margin: 0in; font-size: 12pt;
          font-family: Times"><font size="+2">Global climate impacts of
            Indian Ocean warming</font></p>
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        The tropical Indian Ocean (TIO) has warmed by 1°C since the
        1950s, at a faster rate than the other tropical oceans. In this
        talk, I will discuss how this warming can affect the Atlantic
        Ocean via atmospheric and oceanic teleconnections. Specifically,
        by reorganizing the atmospheric Walker circulation in the
        equatorial band, this warming can reduce precipitation in the
        tropical Atlantic, resulting in pronounced surface salinity
        anomalies. On multidecadal timescales, these anomalies are
        advected to northern high latitudes and strengthen the Atlantic
        meridional overturning circulation (AMOC). The resultant AMOC
        changes lead to a stronger hemispheric
        <div>asymmetry and a northward shifted intertropical convergence
          zone (ITCZ). On shorter timescales, Indian Ocean warming
          generates a train of atmospheric planetary waves, which reach
          the subpolar North Atlantic, strengthen surface westerly winds
          there, and cool the underlying ocean within a few months to
          years. This mechanism could potentially explain the suppressed
          warming in the subpolar North Atlantic (known as the "warming
          hole") seen in the observational record. Further, I will
          discuss the implications for past and future climate changes
          and ocean interbasin teleconnections.</div>
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        <p class="x_MsoNormal" style="margin: 0in; font-size: 12pt;
          font-family: Times">Via Zoom:</p>
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        <p class="x_MsoNormal" style="margin: 0in; font-size: 12pt;
          font-family: Times"><font size="+2"><a href="https://fsu.zoom.us/j/92556866443?pwd=bTFlc1Rnc0QrUG84UFlvN1MxdzdlUT09" id="LPlnk" moz-do-not-send="true">https://fsu.zoom.us/j/92556866443?pwd=bTFlc1Rnc0QrUG84UFlvN1MxdzdlUT09</a></font></p>
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            !important">The informal virtual chat will start at 3:00 PM
            through the same zoom link. </span>Please contact Dr Zhaohua
          Wu if you would like to meet privately with the speaker in
          that day.
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        <p class="x_MsoNormal" style="margin: 0in; font-size: 12pt;
          font-family: Times">The more detailed zoom meeting information
          is appended</p>
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        <p class="x_MsoNormal" style="margin: 0in; font-size: 12pt;
          font-family: Times">==========================</p>
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          Zhaohua Wu is inviting you to a scheduled Zoom meeting.
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          <div>Topic: EOAS Colloquium, Oct. 9</div>
          <div>Time: Oct 9, 2020 03:00 PM Eastern Time (US and Canada)</div>
          <div><br>
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          <div>Join Zoom Meeting</div>
          <div><a class="moz-txt-link-freetext" href="https://fsu.zoom.us/j/92556866443?pwd=bTFlc1Rnc0QrUG84UFlvN1MxdzdlUT09">https://fsu.zoom.us/j/92556866443?pwd=bTFlc1Rnc0QrUG84UFlvN1MxdzdlUT09</a></div>
          <div><br>
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          <div><b>Meeting ID: 925 5686 6443</b></div>
          <div><b>Passcode: 451688</b></div>
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          <div>Dial by your location</div>
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          <div>Meeting ID: 925 5686 6443</div>
          <div>Find your local number: <a class="moz-txt-link-freetext" href="https://fsu.zoom.us/u/al1Y5u3NL">https://fsu.zoom.us/u/al1Y5u3NL</a></div>
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          <div>Meeting ID: 925 5686 6443</div>
          <div>Passcode: 451688</div>
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