BEGIN:VCALENDAR VERSION:2.0 PRODID:-//132.216.98.100//NONSGML kigkonsult.se iCalcreator 2.20.4// BEGIN:VEVENT UID:20250508T201553EDT-7086uKSGU0@132.216.98.100 DTSTAMP:20250509T001553Z DESCRIPTION:Large-eddy simulations of sea breezes over a mountainous island \n\nAbstract\n\nMountains and coastlines both favor the development of the rmally-driven diurnal circulations\, including slope flows induced by elev ated heating and land/sea breezes generated by differential heating of lan d and water bodies. Although slope flows and sea-breeze circulations have each been studied intensively using observations and numerical simulations \, the interactions between the two remain only partially understood. In p articular\, some studies suggest an enhancement of the sea breeze in the p resence of coastal orography while others point to a blocking or weakening effect. To gain insight into these interactions\, we conduct a series of large-eddy simulations of daytime airflow over an idealized Gaussian-shape d island terrain. We analyze the simulated sea-breeze propagation characte ristics and frontal-circulation strength under varying environmental and t opographic factors\, including island geometry (width\, terrain height and steepness)\, boundary-layer static stability\, and ambient winds. The res ults suggest that inland orography accelerates the sea-breeze front inland but also causes a weakening of the baroclinicity and frontal circulation. Over sufficiently tall mountains\, the latter effect causes the sea-breez e front to vanish entirely as it ascends the slope. The mountain effects o n the sea breeze are quantified by tracking the frontogenesis terms and al ong-front vertical motion in a sea-breeze-following reference frame. This analysis suggests that the mountain upslope flow acts much like an onshore ambient wind: it hastens the inland frontal propagation but also induces strong frontolysis\, both of which scale with the mountain height. The pot ential for sea-breeze blocking at the foot of the mountain is also assesse d through a simple Boussinesq scaling.\n DTSTART:20151104T193000Z DTEND:20151104T203000Z LOCATION:Room 934\, Burnside Hall\, CA\, QC\, Montreal\, H3A 0B9\, 805 rue Sherbrooke Ouest SUMMARY:Student Seminar: Chun-Chih (David) Wang URL:/meteo/channels/event/student-seminar-chun-chih-da vid-wang-255058 END:VEVENT END:VCALENDAR