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<b><u><span style="margin:0px; font-family:"Monotype Corsiva"; font-size:26pt">Meteorology<span class="Apple-converted-space"> </span><span class="markys8emuxhh" style="margin:0px">Seminar</span></span></u></b><span style="margin:0px; font-size:10pt"></span></p>
<div style="text-align:center"><font color="#201f1e" face="Monotype Corsiva"><span style="font-size:37.33333206176758px"><b>Lindsay Lawrence</b></span></font></div>
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<span style="margin:0px; font-family:"Monotype Corsiva"; font-size:28pt">M. S. Meteorology Candidate</span><span style="margin:0px; font-size:10pt"></span></p>
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<b><u><span style="margin:0px; font-family:SimSun; font-size:14pt; text-transform:uppercase">TITLE</span></u></b><b><span style="margin:0px; font-family:SimSun; text-transform:uppercase">:</span></b><span style="margin:0px; font-family:SimSun; text-transform:uppercase">
The influence of enso and the iod on atmospheric fronts and frontal precipitation across australia</span></p>
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<b><u><span style="margin:0px; font-size:14pt">Major Professor</span></u></b><b><span style="margin:0px; font-size:14pt">: Dr. Parfitt</span></b></p>
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<b><u><span style="margin:0px; font-size:14pt">Date</span></u></b><b><span style="margin:0px; font-size:14pt">:</span></b><span style="margin:0px; font-size:14pt"> November 5th, 2021 <b><u>Time</u>: 10:30 AM</b></span></p>
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<b><span style="margin:0px; font-size:10pt"> </span></b><span style="margin:0px; font-family:"Times New Roman",serif; font-size:10pt"></span></p>
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<b><u><span style="margin:0px; font-size:14pt">Location</span></u></b><b><span style="margin:0px; font-size:14pt">: Room 2061 EOA or via </span></b><span style="margin:0px; font-size:14pt"><b>Zoom:</b></span><span style="margin:0px; font-size:14pt; line-height:normal"><b style="line-height:normal"> </b></span><span style="margin:0px; font-size:14pt"><a href="https://fsu.zoom.us/j/98673761097" id="LPNoLPOWALinkPreview" style="font-family:"Helvetica Neue"; font-size:13px; font-style:normal; font-variant-caps:normal"><span style="font-size:14pt; line-height:normal">https://fsu.zoom.us/j/98673761097</span></a><b></b></span></p>
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<b>ABSTRACT</b></p>
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<span style="font-size:12pt; font-family:TimesNewRomanPSMT">Over the past few decades, Southeast Australia has experienced severe regional climatic events, including devastating floods and some of the most extreme droughts on record, linked in part to influences
from both the El Niņo Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD). In this manuscript, the extent to which ENSO-IOD driven rainfall anomalies are communicated specifically through variations in atmospheric fronts is quantified. Consistent
with previous studies, the most extreme wet (dry) conditions result from the co-occurrence of La Niņa-Negative IOD (El Niņo-Positive IOD). With maximum anomalous wet and dry conditions in southeast Australia during Austral winter, it is found that most of
these precipitation anomalies result from changes to the frontal precipitation associated with the passing of atmospheric fronts. These anomalies accompany changes in both the frequency of atmospheric fronts as well as the precipitation rate associated with
those fronts. Interestingly, the distribution in the dynamic strength of individual fronts remains relatively unchanged. Instead, the variability in atmospheric fronts and their associated precipitation appears to be related to latitudinal fluctuations in
the eddy-driven jet.</span></p>
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