BEGIN:VCALENDAR VERSION:2.0 PRODID:-//132.216.98.100//NONSGML kigkonsult.se iCalcreator 2.20.4// BEGIN:VEVENT UID:20250511T050800EDT-1954gsfsSm@132.216.98.100 DTSTAMP:20250511T090800Z DESCRIPTION: \n\nStudent Seminar Series\n\nDepartment of Atmospheric & Ocea nic Sciences\n\npresents\n\na talk by\n\nJing Feng\n PhD candidate\n\nDistr ibution of upper tropospheric and lower stratospheric (UTLS) water vapor i nfluenced by deep convections\n\nDespite its scarcity\, water vapor in the upper troposphere and lower stratosphere (UTLS) is crucial to the climate due to both its radiative and chemical impacts. The distribution of water vapor in this region\, however\, remains poorly measured\, partly due to deep convection processes that injected potential water sources through th e cold trap. Researchers have found inconsistency among products from diff erent satellite missions. This brings large uncertainty to stratospheric w ater vapor decadal variation and its contribution to climate feedback.\n \n The focus of this study is to apply an innovative method to sounding UTLS water vapor profiles above opaque deep convective cloud layers\, using nad ir view satellite measurements. The retrieval algorithm is performed based on a widely used Optimal Estimation method that combines satellite observ ation and historical data to give an optimal estimation of the atmospheric state. Theoretical assessments show that this method largely eliminates m ajor difficulties in a clear-sky retrieval\, including the non-monotonic t emperature around the tropopause\, and the spectral signal of upper-level water vapor being weak relative to noise from lower atmosphere uncertainty .\n\nComparisons between the retrieval using radiance data from Atmospheri c Infrared Sounder (AIRS\, https://airs.jpl.nasa.gov/) and collocated airc raft measurements show that the retrieval can detect the water vapor anoma lies caused by deep convective events. Using this approach in synergy with cloud properties retrieved by CloudSat\, we further characterize the wate r vapor distribution pattern above deep convection events passed by A-trai n satellites in the past decades.\n\nWednesday Oct 16/ 2.30 PM/ Room 934 B urnside Hall\n\n \n\n \n\n \n DTSTART:20191016T183000Z DTEND:20191016T193000Z LOCATION:Room 934\, Burnside Hall\, CA\, QC\, Montreal\, H3A 0B9\, 805 rue Sherbrooke Ouest SUMMARY:Distribution of upper tropospheric and lower stratospheric (UTLS) w ater vapor influenced by deep convections URL:/meteo/channels/event/distribution-upper-troposphe ric-and-lower-stratospheric-utls-water-vapor-influenced-deep-convections-3 01658 END:VEVENT END:VCALENDAR