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Climate Change, Extreme Heat, and Public Health Jeremy Hess, MD, MPH, FACEP Assistant Professor, Emergency Medicine, Environmental Health Emory University Schools of Medicine and Public Health Consultant, Climate Change Program, CDC Yale School of Public Health Alumni Day Overview • My opinions alone, and no conflicting interests to report • Today is not a good day to die (of heat stroke) • Sinks, bathtubs, and thermodynamics • If not now, then when? • So what do we do? Sunny, clear, high 74°F, low 54°F NO HEAT DEATHS TODAY Heat Mortality, US Thermal Homeostasis • Population is aggregate of individuals • Individual heat budgets • Narrow physiological temperature range – Behavioral maintenance – Physiological maintenance • Heat exhaustion • Heat stroke • Humidity matters (AT, THI) Handling Heat Illness Susceptibility Factors Protective Harmful • Intact thermoregulatory mechanisms • Impaired thermoregulation – – – – Sweating Thirst Renal function Cardiovascular function • Intact recognition of adverse exposure • Intact behavioral response • Resources • Agency • Social capital – Impaired sweating (anticholinergics) – Impaired thirst impulse – Kidney and CV disease – Obesity • Impaired cognition • Impaired behavioral response • Inadequate access to preventive resources • Social isolation • Lack of agency Human Heat Exposure Hazard Exposure Susceptibility Hotlanta Hotlanta (at Night) Abundant Examples Chicago, 1995 California, 2006 Climate Variability and Long Term Change SINKS, BATHTUBS, AND THE LAWS OF THERMODYNAMICS GHG Concentrations Last 10K Yrs CO2 CH4 NOx CO2 and Temperature 2010 Tied for Warmest Year Sunny, hazy, high 92°F, low 70°F ALUMNI DAY, 2091 Heat Mortality, US Evolving Estimates • 0.6°C temperature rise to date • Projections suggest 10x that by 2100 • Increasing heat wave: • Frequency • Severity • Threats to long-term habitability of large portions of the planet Projected Change, 2040-2060 Projected Change, 2060-2080 Number of Days over 100F Shifting Temperature Distributions Heat Waves • A period of abnormally and uncomfortably hot and usually humid weather • Combination of high temps and stagnant air masses •Persistent – days to weeks European Heat Wave 2003 UK 2,091 Italy 3,134 France 14,802 Portugal 1,854 Spain 4,151 Switzerland 975 Netherlands 1,400-2,200 Germany TOTAL 1,410 29,817-30,617 Did CC Make It More Likely? 75% of Add’l Risk Anthropogenic What the Future Holds Stott PA, Stone DA, Allen MR. Human contribution to the European heat wave of 2003. Nature 2004, doi:10.1038/nature03089. Mitigation and Adaptation SO WHAT DO WE DO? Mitigation Health Benefits Moving Our Coping Range Public Health Adaptation 1896 1900 1904 1908 1912 1916 1920 1924 1928 1932 1936 1940 1944 1948 1952 1956 1960 1964 1968 1972 1976 1980 1984 1988 1992 1996 2000 2004 2008 2006 2010 2014 2018 2022 2026 2030 2034 2038 2042 2046 2050 2054 2058 Scenario Based Planning Historical Trends Linear Projections 110 105 100 95 90 Tmax 85 Tmean Tmin 80 Tmax 75 Tmean Tmin 70 65 60 Projected Extremes 100 US Cities Projected extreme value distributions Projected average (2035) In Conclusion • Heat is already the country’s leading weather-related cause of death • Heat is also associated with a significant burden of morbidity • Our GHG emissions are adding to the atmospheric sink faster than it is depleted • The result is a steady, delayed, significant warming • Temperatures will increase, but the greatest concern is in the extremes • Mitigation is fundamentally important – remember the delay! • Adaptation is necessary now and will need to be increasingly aggressive in the future Thank you!