Dr. Laurence S. Kalkstein
Center for Climatic Research
Department of Geography
University of Delaware
J. Scott Greene
Oklahoma Climatological Survey
University of Oklahoma
Norman, OK 73109
ACKNOWLEDGMENTS:
This research was primarily funded by
the Climate and Policy Assessment Division, U.S. Environmental Protection
Agency, on Cooperative Agreement numbers CR-817693 and CR-824404. The authors
would like to thank the Agency for its continued support.
ABSTRACT
A new air mass-based synoptic procedure
is used to evaluate climate/mortality relationships as they presently exist,
and to estimate how a predicted global warming might alter these values. Forty-four
large U.S. cities with metropolitan areas exceed ing 1,000,000 population
are analyzed. Sharp increases in mortality are noted in summer for most cities
in the East and Midwest when two particular air masses are present. A very
warm air mass of maritime origin is most important in the eastern U.S., an
d when present can increase daily mortality by as many as 30 deaths in large
cities. A hot, dry air mass is important in many cities, and, although rare
in the East, can increase daily mortality by up to 50 deaths. Cities in the
South and Southwest show lesser weather/mortality relationships in summer.
During winter, air mass-induced increases in mortality are considerably less
than in summer. Although daily winter mortality is usually higher than summer,
the causes of death which are responsible for most winter mortality do not
vary much with temperature. Using models which estimate climate change for
the years 2020 and 2050, it is estimated that summer mortality will increase
dramatically and winter mortality will decrease slightly, even if people
acclimatize to the increased warmth. Thus, a sizable net increase in weather-related
mortality is estimated if the climate warms as the models predict.