BEGIN:VCALENDAR VERSION:2.0 PRODID:-//132.216.98.100//NONSGML kigkonsult.se iCalcreator 2.20.4// BEGIN:VEVENT UID:20250805T060746EDT-9017DkgFId@132.216.98.100 DTSTAMP:20250805T100746Z DESCRIPTION:Tropical Subseasonal Variability and Its Teleconnection in Cana dian EC GEM\n\nAccording to the past studies\, the analysis of observation s indicates the tropical convection anomaly may have impacts on the pressu re distribution in higher latitude with Rossby wave train. Aimed at improv ing the Madden-Julian Oscillation (MJO) in Global Environmental Multiscale Model developed by Environment Canada (EC GEM) and the prediction of the wintertime weather in North America\, the convection structure of MJO and the teleconnection in the north hemisphere from GEM are assessed.  In gene ral\, the significant convective features of MJO can be reproduced by GEM and the signal is also more intense than observation. In the 23 model year s\, the outgoing longwave radiation (OLR) and the precipitation distributi on in the tropics from our simulation is able to represent the eastward pr opagation of the convection system and to capture the corresponding locati ons of convection in each phase of MJO. Based on the MJO index defined by Wheeler and Hendon\, the same method is applied here for the further analy sis of the linkage between the tropical subseasonal variability and the te leconnection in the Northern Hemisphere.  Since the MJO index can be consi dered as the convection signal\, the lag composite analysis of the geopote ntial height with the index depicts the distribution after the convection. After MJO phase 3\, the convection occurance in the Indian Ocean\, the 50 0hPa geopotential height anomaly draws a positive-North Atlantic Oscillati on (NAO) like pattern. While after the convection reaches the Western Paci fic Ocean\, MJO Phase 7\, the 500hPa geopotential height anomaly behaves l ike negative NAO pattern. Reversely\, the lag composite of NAO index in GE M with respect to each MJO phase also has the statistic significant correl ation to phase 3 and 7\, which is similar to the former research that reve als the connection between the NAO and the MJO. Results in this study sugg est the understanding of MJO may provide an access to the better forecast of the wintertime weather in North America.\n DTSTART:20160413T190000Z DTEND:20160413T203000Z LOCATION:Room 934\, Burnside Hall\, CA\, QC\, Montreal\, H3A 0B9\, 805 rue Sherbrooke Ouest SUMMARY:Student Seminar: Pei-Ning Feng URL:/meteo/channels/event/student-seminar-pei-ning-fen g-256985 END:VEVENT END:VCALENDAR