BEGIN:VCALENDAR VERSION:2.0 PRODID:-//132.216.98.100//NONSGML kigkonsult.se iCalcreator 2.20.4// BEGIN:VEVENT UID:20250802T003147EDT-78714fUlTp@132.216.98.100 DTSTAMP:20250802T043147Z DESCRIPTION: \n\nStudent Seminar Series\n\nDepartment of Atmospheric & Ocea nic Sciences\n\npresents\n\na talk by\n\nKai Melamed-Turkish\n MSc Student \n\nA Dynamic Approach to the development of a precipitation climatology a s applied to Montréal\, Québec\n\nMost precipitation climatologies partiti on the precipitation time series by identifying 24-\, 48- or 72-h precipit ation events. However\, these partitioning methods inherently lack physica l intuition. Here\, I will present a precipitation climatology for Montréa l\, Québec that utilizes our understanding of atmospheric dynamics.\n\nThe quasigeostrophic (QG) omega equation provides meteorologists with a means to qualitatively diagnose vertical motion\, which is necessary to produce precipitation\, in the atmosphere. Knowing the positions of the low-level cyclones and anticyclones relative to the upper-level troughs and ridges\ , we can infer the contributions of the low-level temperature advections a nd upper-level vorticity advections towards omega. With this knowledge\, w e can use the troughs and ridges in the 500-hPa geopotential heights to qu alitatively diagnose the vertical motion in the atmosphere and partition t he precipitation time series. The end result is a 40-year climatology wher e we investigate whether precipitation in Montréal conforms to our expecta tions from the QG-omega equation.\n\nAcross all seasons\, our results show that Montreal receives significantly more intense precipitation during th e times when we expect unambiguous ascent\, and significantly less intense precipitation during periods when we expect unambiguous descent. During t he periods when we expect unambiguous ascent\, the values of omega are the lowest (strongest ascent) and the 850-hPa equivalent potential temperatur e (qe) anomalies are the highest and vice-versa for the periods of unambig uous descent. Overall\, the results suggest that\, climatologically\, prec ipitation in Montréal conforms to expectations from the QG-omega equation. \n\nWednesday Nov 06/ 2.30 PM/ Room 934 Burnside Hall\n\n \n\n \n\n \n DTSTART:20191106T193000Z DTEND:20191106T203000Z LOCATION:Room 934\, Burnside Hall\, CA\, QC\, Montreal\, H3A 0B9\, 805 rue Sherbrooke Ouest SUMMARY:A Dynamic Approach to the development of a precipitation climatolog y as applied to Montréal\, Québec URL:/meteo/channels/event/dynamic-approach-development -precipitation-climatology-applied-montreal-quebec-302204 END:VEVENT END:VCALENDAR