Results indicate that 100 °F+ days are not frequent at Moline, occurring only about one year in four. The typical synoptic pattern associated with these extreme heat episodes features a stronger than normal upper-tropospheric jet north of the area, a stronger than normal 500-hPA ridge over the central United States, and a warmer than normal lower-tropospheric heat dome to the southwest of the area with strong, thermal advection into the area. Analysis of local heat impacts, as determined by emergency services workload, suggests the criteria used for local heat advisories/warnings are adequate to indicate days of increased demand for heat-related emergency services. However, outliers are apparent and are associated with large-venue outdoor events.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner