Lake Michigan Lake Breezes: Climatology, Local Forcing, and Synoptic Environment

A method was developed to identify the occurrence of lake-breeze events-along the eastern, western, and both shores of Lake Michigan during a 15-yr period (1982-96). Comparison with detailed observations from May through September of 1996-97 showed that the method reasonably identified Lake Michigan lake-breeze events. The method also demonstrated the important ability to distinguish non-lake-breeze events; a problem experienced by previously developed lake-breeze criteria. Analyses of the 15-yr climatological data indicated that lake breezes tended to occur more frequently along the eastern shore of Lake Michigan than along the western shore. On average, a maximum number of lake-breeze events occurred during August at each location. This maximum is most closely associated with weaker monthly average wind speeds. Even though the air-lake temperature difference AT provides the local forcing for the development of the lake-breeze circulation, large temperature differences are not required. Nearly 70% of all events occurred with a daytime maximum [Delta]T [is less than or equal to] 12 [degrees] C. The evaluation of a lake-breeze index [Epsilon] used in past studies and many forecasting applications showed indices computed using offshore or shore-perpendicular wind speeds (U or |U|, respectively) at inland sites resolved [is greater than or equal to] 95% of identified events based on critical [Epsilon] values of 2-6. When wind speed, irrespective of wind direction, was used to calculate [Epsilon], the success of the critical indices decreased by as much as 26%. Results also showed that the lake-breeze index has a considerable tendency to overestimate the number of events. Although the possibility was suggested by previous investigations, the critical value of [Epsilon] may not be appreciably affected by changes in location along the shoreline. In addition, noteworthy differences in the position of synoptic-scale sea level pressure and wind fields with respect to Lake Michigan were found to occur during eastern, western, and both-shore lake-breeze events.