Climate Change and Infectious Disease: Stormy Weather Ahead?
Epstein, Paul R.
From the Center for Health and the Global Environment, Harvard Medical School, Boston, MA.
Address correspondence to: Paul R. Epstein, Center for Health and the Global Environment, Harvard Medical School, 333 Longwood Avenue, Suite 640, Boston, MA 02115; firstname.lastname@example.org
Extreme weather events are becoming more intense, and are likely to become more frequent as the world climate changes. 1,2 For epidemiologists, one important aspect of these trends is their impact on infectious disease.
In this issue of Epidemiology, Woodruff et al. 3 demonstrate a strong association between heavy rainfall and outbreaks of Ross River virus disease. Ross River virus is mosquito borne, and, although the disease is little known outside of Australia, is found in nearly all parts of the continent. Infection can produce disabling polyarthritis, and there is no specific treatment. In southeast Australia, Ross River virus disease poses a threat not just to local populations, but also to tourism—Australia’s largest industry.
The work of Woodruff et al. 3 adds to a growing body of studies 4 that explore the impact of weather on infectious disease. Beginning in the mid-1970s, there has been a worldwide emergence, resurgence, and redistribution of infectious diseases. 5 Although the spread of infectious diseases is multicausal, 6 global climate change may be a major contributor. Weather and climate can influence host defenses, vectors, pathogens, and habitat. Studying climate effects requires integration of information from many sources. For example, by mapping multiple datasets into geographic information systems (GIS), researchers can detect emerging patterns, and these spatial and temporal associations can lead to new hypotheses regarding causality.
The findings of Woodruff et al. 3 are plausible. Although Ross River virus disease can spread even without excessive rain, extreme rainfall increases the likelihood of large outbreaks (via the mosquito Culex australicus). As floodwaters abate, oxbow lakes are pinched off at river bends, creating “billabongs”—ideal sites for breeding mosquitoes. With alert public health monitoring, preventive measures can be taken to avoid spread of the disease.
But a larger question is, can we predict the conditions that lead to the spread of the disease? Our capacity for long-term weather forecasting has greatly improved, with monitoring of Pacific Sea surface temperatures and the state of the El Niño/Southern Oscillation. Such forecasts have helped predict weather patterns that may lead to infectious disease outbreaks. 7–9 There are longer trends that must also be considered in making weather projections—which brings us to the issue of climate change.
In the study of global climate change, the field is an N of 1, an experiment that cannot be repeated. 10 For the past 420,000 years, atmospheric CO2 levels (which parallel average global temperatures) have remained within a range of 180 to 280 parts per million. 11 CO2 is now close to 370 parts per million and rising. 2 Taken as a whole, the Holocene Age—the past 10,000 years—has been one of the most stable periods in climate records. 12 Even so, warming this century has been rapid, and it is not occurring uniformly. Although the overall rate of maximum temperature increase since 1950 is approximately 1°C per century, minimum (nighttime and winter) temperatures have increased at twice that rate (∼2°C per century), 13 and winter temperatures are rising even faster near the poles. 2 In global change research, models are used to project what might be expected with warming, and data are examined for consistency with the projections. The accumulating number of such “fingerprint” studies forms the basis for the conclusion that human-induced climate change has indeed begun.
Global warming has implications for the spread of infectious disease. Small arthropods are highly temperature sensitive, 14 and temperature constrains the range of vector-borne diseases like Ross River virus disease. 15–17 Ticks have been moving northward in Sweden as winters warm. 18 Mosquitoes are appearing in mountainous regions where plant communities and freezing levels have shifted upward and glaciers are rapidly retreating. 19 Changes in mountain ecosystems are consistent with projections, 20 and the biological and physical observations are consistent with one another.
In addition, extreme weather events can be associated with “clusters” of vector-, rodent-, and water-borne diseases. 21 Flash floods leave behind mosquito breeding grounds, drive rodents from burrows, and seed the waterways with toxic chemicals, microorganisms (such as E. Coli, Cryptosporidium, and Vibrio cholerae), and nutrients that can trigger red tides. Sequential extremes can be particularly destabilizing. Droughts reduce predators, whereas heavy rains boost food for their opportunistic prey.
Other emerging climate-related health concerns that require further investigation include: the role of increased variability in heat and cold mortality;22 synergies with air pollution, including CO2 fertilization, ragweed pollen, and asthma;23 travel hazards associated with unstable winter weather;24 and genetic shifts in arthropods induced by warming. 25
As important as the overall tendency toward global warming may be to human health, the effects of the extreme and anomalous weather that accompany it may be even more profound. 12 The rate of warming has recently increased, and anomalies and wide swings away from norms have become more frequent. 2 This increased variance raises the possibility that natural corrective mechanisms are being overwhelmed. Increased variability may also be characteristic of transitions in climate. Ice core records from near the end of the last ice age (about 10,000 years ago) indicate that increased variability was associated with a rapid change in state. 12
“As important as. . .global warming may be to human health, the effects of the extreme. . .weather that accompany it may be even more profound.”
Further evidence for instability comes from an increase in temperature gradients in the world ocean. Whereas the ocean has warmed overall, a large region of the North Atlantic has cooled in the past several decades, perhaps from melting and thinning of Arctic ice 26–28 and from increased rain at high latitudes. 29 The North Atlantic is where deep-water formation drives thermohaline circulation, the “ocean conveyor belt” that is regarded as key to climate stabilization. 30
Warming is accelerating the hydrological (water) cycle. As heat builds up in the deep ocean—down to 2 miles 31 —more water evaporates and sea ice melts. 2 Over the past century, droughts have lasted longer and heavy rainfall events (defined as more than 5 cm, or 2 inches, per day) have become more frequent. 32 Enhanced evapotranspiration dries out soils in some regions, whereas the warmer atmosphere holds more water vapor, fueling more intense, tropical-like downpours elsewhere. 33 Prolonged droughts and intense precipitation have been especially punishing for developing nations.
The resurgence of infectious diseases in the late 20th century has brought infectious disease back into the mainstream of epidemiology. Investigating weather variables associated with Ross River virus disease and other infectious diseases can help anticipate future epidemics, and can focus our efforts at surveillance and interventions. Early warning systems can have direct health and economic benefits.
“Volatility of infectious diseases may be one of the earliest biological expressions of climate instability.”
But the epidemiologic monitoring of infectious diseases may have even more fundamental utility. We have already underestimated the rate at which climate would change. So, also, we have underestimated the sensitivity of biological systems to this change. 34,35 Volatility of infectious diseases may be one of the earliest biological expressions of climate instability. Close monitoring of the spread of infectious disease can thus contribute to the evidence that will be needed to motivate strong precautionary policies. 36 Pollutants from fossil fuel combustion are the primary drivers of climate change. The environmental, health, 37 and security reasons for weaning ourselves from these buried carbon stores are mounting. Although the costs of changing our patterns of energy production and consumption would be high in the short run, we may also be underestimating the economic and social benefits from developing clean energy technologies and greater energy efficiency. The alternative of continuing our present course may cost more in the long run than any society would choose to pay.
1. Albritton DL, Allen MR, Baede APM, et al
. Climate Change 2001: The Scientific Basis
. Intergovernmental Panel on Climate Change (IPCC) Working Group Summary for Policy Makers, 3rd Assessment Report. New York: Cambridge University Press, 2001.
2. Houghton JT, Ding Y, Griggs DJ, et al
. Climate Change 2001: The Scientific Basis
. Intergovernmental Panel on Climate Change (IPCC) Working Group I Third Assessment Report. New York: Cambridge University Press, 2001.
3. Woodruff RE, Guest CS, Garner MG, et al
. Predicting Ross River virus epidemics from regional weather data. Epidemiology 2002; 13: 384–393.
4. McMichael AJ, Githeko A, Confalonieri U, et al.
Contribution of working group II to the third assessment report of the Intergovernmental Panel on Climate Change (IPCC). In: JJ McCarthy, Canziani OF, Leary NA, et al.
, eds. Climate Change 2001: Impacts, Adaptation & Vulnerability
. New York: Cambridge University Press, 2001.
5. World Health Organization. The World Health Report 1996: Fighting Disease, Fostering Development. Geneva: World Health Organization, 1996.
6. Rothman KJ. Causes. Am J Epidemiol 1976; 104: 587–592.
7. Bouma MJ, Poveda G, Rojas W, Chavasse D, Quinones M, Patz JA. Predicting high-risk years for malaria in Colombia using parameters of El Niño Southern Oscillation. Trop Med Int Health 1997; 2: 1122–1127.
8. Kovats RS, Bouma MJ, Haines A. El Niño and Health
. WHO/SDE/PHE/99.4. Geneva: World Health Organization, Geneva, 1999.
9. Linthicum KJ, Anyamba A, Tucker CJ, Kelley PW, Myers MF, Peters CJ. Climate and satellite indicators to forecast Rift Valley fever epidemics in Kenya. Science 1999; 285: 397–400.
10. Davis D. The global experiment with “an n of one.” Lancet 2001; 358: 1737.
11. Petit JR, Jouze J, Raynaud D, et al
. Climate and atmospheric history of the past 420,000 years from the Vostok Ice Core, Antarctica. Nature 1999; 399: 429–436.
12. National Research Council. National Academy of Sciences. Abrupt Climate Change: Inevitable Surprises. Washington DC: National Academy Press, 2001.
13. Easterling DR, Horton B, Jones PD, et al
. Maximum and minimum temperature trends for the globe. Science 1997; 277: 363–367.
14. Elias SA. Quaternary Insects and Their Environments. Washington DC: Smithsonian Institution Press, 1994.
15. McMichael AJ, Haines A, Slooff R, Kovats S, eds. Climate Change and Human Health. Geneva: World Health Organization, World Meteorological Organization, United Nations Environmental Program, 1996.
16. Patz JA, Epstein PR, Burke TA, Balbus JM. Global climate change and emerging infectious diseases. JAMA 1996; 275: 217–223.
17. Haines A, McMichael A, Epstein PR. Global climate change and health. CMAJ 2001; 163: 729–734.
18. Lindgren E, Gustafson R. Tick-borne encephalitis in Sweden and climate change. Lancet 2001; 358: 16–18.
19. Epstein PR, Diaz HF, Elias S, et al
. Biological and physical signs of climate change: focus on mosquito-borne disease. Bull Am Meteorological Soc 1998; 78: 409–417.
20. Martens WJM, Jetten TH, Focks D. Sensitivity of malaria, schistosomiasis and dengue to global warming. Climate Change 1997; 35: 145–156.
21. Epstein PR. Climate and health. Science 1999; 285: 347–348.
22. Braga ALF, Zanobetti A, Schwartz J. The time course of weather related deaths. Epidemiology 2001; 12: 662–667.
23. Wayne P, Foster S, Connolly J, Bazzaz F, Epstein P. Production of allergenic pollen by ragweed (Ambrosia artemisiifolia
L.) is increased in CO2
-enriched atmospheres. Ann Allergy Asthma Immunol 2002; 88: 279–282.
24. Environmental Protection Agency. Potential for Personal Injuries and Travel Hazards. Environmental Protection Agency Workshop on Climate Change and Climate Variability, Washington DC, June 2001.
25. Bradshaw WE, Holzapfel CM. Genetic shift in photoperiodic response correlated with global warming. Proc Natl Acad Sci 2001; 98: 14509–14511.
26. Krabill W, Frederick E, Manizade S, et al
. Rapid thinning of parts of the southern Greenland Ice Sheet. Science 1999; 283: 1522–1524.
27. Rothrock DA, Yu Y, Marykut GA. Thinning of the Arctic Sea-ice cover. J Geophys Res Letters 1999; 26: 3469–3472.
28. Parkinson CL, Cavalieri DJ, Gloersen P, Zwally HJ, Comiso JC. Spatial distribution of trends and seasonality in the hemispheric sea ice covers. J Geophys Res 1999; 104: 20827–20835.
29. Semiletov IP, Savelieva NI, Weller GE, et al
. The dispersion of Siberian river flows into coastal waters: meteorological, hydrological and hydrochemical aspects. In: Lewis EL, ed. The Freshwater Budget of the Arctic Ocean. Dordrecht: Kluwer Academic Publishers, 2000; 323–366.
30. Broecker WS. Thermohaline circulation, the Achilles heel of our climate system: will man-made CO2 upset the current balance? Science 1997; 278: 1582–1588.
31. Levitus S, Antonov JI, Boyer TP, Stephens C. Warming of the world ocean. Science 2000; 287: 2225–2229.
32. Karl TR, Knight RW, Plummer N. Trends in high-frequency climate variability in the twentieth century. Nature 1995; 377: 217–220.
33. Trenberth KE. The extreme weather events of 1997 and 1998. Consequences 1997; 5: 3–15.
34. McCarthy JJ, Canziani OF, Leary NA, Dokken DJ, White KS, eds. Climate Change 2001: Impacts, Adaptation and Vulnerability
. Contribution of Working Group II to the Third Assessment Report of the Intergovernmental Panel on Climate Change (IPCC). Cambridge: Cambridge University Press, 2001.
35. Walther GR, Post E, Convey P, et al.
Ecological responses to recent climate change. Nature 2002; 416: 389–395.
36. Kriebel D, Tickner J, Epstein P, et al
. The precautionary principle in environmental science. Environ Health Perspect 2001; 109: 871–876.
37. Cifuentes L, Borja-Aburto VH, Gouveia N, Thurston G, Davis DL. Climate change. Hidden health benefits of greenhouse gas mitigation. Science 2001; 293: 1257–1259.
© 2002 Lippincott Williams & Wilkins, Inc.
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