Mutli-decadal time series of daily mortality counts and hourly temperature for seven U.S. cities with different climates were examined via a generalized additive model. The temperature effect was modeled separately for each hour of the day (with up to three-day lags) in addition to several different methods of determining daily maximum, minimum, and mean temperature.
In three northern U.S. cities that are typically considered to have heat-sensitive populations (Boston, Philadelphia, and Seattle), the heat-mortality response is diurnal, with the strongest relationships for afternoon or maximum temperature at lag zero (day of death) or lag one (afternoon and evening). The temperature-mortality relationships are weaker in the warmer, southern U.S. cities, where slightly stronger relationships to morning temperatures are evident. The strongest temperature-mortality relationships are associated with maximum temperature, though the results using mean temperature are comparable.
The results for the three northern cities, in which heat-mortality relationships developed using afternoon/maximum temperatures are stronger than those using morning/minimum temperatures, suggest that cooler mornings may provide a protective effect from heat-related mortality in these climates. In general, choice of observation time, lag, and variable calculation method often impacts the robustness of the model results. In general, heat-related mortality is most closely coupled to afternoon and maximum temperatures in most cities, particularly those that are typically heat-sensitive.