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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://www.researchgate.net/scientific-contributions/2031316853_Faycal_Lamraoui" href="https://www.researchgate.net/scientific-contributions/2031316853_Faycal_Lamraoui" title="">Dr. Faycal Lamraoui from CCNY </a></p><p>	Tilte: <strong><em>"<span><span style="line-height:107%"><span>Post-Cold Frontal Clouds: Relationship Between Upper-level and Boundary Layer Properties"</span></span></span></em></strong></p><p>	<span><span style="line-height:107%"><span>Abstract: </span></span>Using cloud and environment observations from the Atmospheric Radiation Measurement program (DOE-ARM) Eastern North Atlantic (ENA) site in the Azores Islands and Weather Research and Forecasting Model (WRF) simulations, cloud properties in post</span><span style='Math",serif'>‐</span><span>cold front (PCF) periods are examined and compared to similar conditions of subsidence (non</span><span style='Math",serif'>‐</span><span>PCF). Also, we investigate how distinct pairs of planetary boundary layer (PBL) and convection parameterization schemes represent cloud fraction in the PCF and their interaction with upper-level. Low</span><span style='Math",serif'>‐</span><span>level clouds are predominant and are found to have higher cloud</span><span style='Math",serif'>‐</span><span>base and top heights, colder cloud</span><span style='Math",serif'>‐</span><span>top temperature, as well as greater vertical extent and liquid water path during PCF than non</span><span style='Math",serif'>‐</span><span>PCF periods. The environmental metric that is best correlated with cloud boundaries for both PCF and non</span><span style='Math",serif'>‐</span><span>PCF periods is the difference in potential temperature between the sea surface and 800 hPa, a parameter used to locate cold air outbreak conditions. A greater sensitivity of PCF clouds to convection than PBL schemes was found in the PCF region. The key processes that are found to significantly impact the cloud fraction distribution in the PCF region are the strength of the PBL decoupling, the vertical wind shear and the occurrence of drizzle. The results suggest both the properties of the boundary layer and the presence of an upper</span><span style='Math",serif'>‐</span><span>level cyclone associated with the cold front determine PCF cloud properties. </span></p>
LOCATION:HUCE Seminar Room MCZ 440
STATUS:CONFIRMED
DTSTART:20181026T160000Z
DTEND:20181026T160000Z
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