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X-WR-CALNAME;VALUE=TEXT:Special ClimaTea 
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SUMMARY:Special ClimaTea 
DESCRIPTION:<p>	Speaker: <a data-url="https://uwpcc.ocean.washington.edu/person/Lucas_Vargas_Zeppetello" href="https://uwpcc.ocean.washington.edu/person/Lucas_Vargas_Zeppetello" title="">Lucas Vargas Zeppetello</a></p><p>	Title: <strong><em>"<span class="gmail-s1"><span style="New">Simple Models of Land Surface Evaporation: Theory and Applications</span></span>"</em></strong></p><p>	Abstract: <span class="gmail-s1"><span style="New">Observations show the relationship between evaporation and soil moisture generally conforms to a “two regime” framework; namely that evaporation is limited by available soil moisture in dry climates and by radiation in wet climates.</span></span><span class="gmail-apple-converted-space"><span style="New">  </span></span><span class="gmail-s1"><span style="New">Despite its common acceptance as a pedagogical tool to understand soil moisture’s impact on evaporation, no globally uniform value of soil moisture at which a transition between the two regimes occurs has been observed.</span></span><span class="gmail-apple-converted-space"><span style="New">  </span></span><span class="gmail-s1"><span style="New">Guided by output from a simple model of the land-atmosphere interface, we derive expressions for evaporative cooling anomalies and vapor pressure deficit that demonstrate the non-linear impact of soil moisture perturbations.</span></span><span class="gmail-apple-converted-space"><span style="New">  </span></span><span class="gmail-s1"><span style="New">These equations show that a negative feedback between evaporation and surface temperature gives rise to the two apparent regimes without requiring a critical value of soil moisture at which the transition occurs.</span></span><span class="gmail-apple-converted-space"><span style="New">  </span></span><span class="gmail-s1"><span style="New">As an application of these simple expressions, we present a diagnostic equation for summertime temperature variance as a function of radiation and precipitation, the two primary evaporation forcing agents.</span></span><span class="gmail-apple-converted-space"><span style="New">  </span></span><span class="gmail-s1"><span style="New">This equation can be used to accurately model contemporary summertime temperature variance and make predictions about how variance will evolve under various climate change scenarios. </span></span><a data-fid="3822940" href="/file_url/616">Reference paper</a></p>
LOCATION:TBD 
STATUS:CONFIRMED
DTSTART:20200129T170000Z
DTEND:20200129T170000Z
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