The Coming Health Crisis
Indirect effects of global climate change threaten the health
of hundreds of millions of people. The very uncertainty that shrouds this issue must serve as an organizing principle
for adaptation to its ill effects.
Human activity is disrupting Earth’s climate, and the rising emissions of greenhouse gases are accelerating that disruption. (See “Our Changing Climate” box below) Some of the health consequences of climate change are straightforward: warmer temperatures, changes in the hydrologic cycle, increased ground-level ozone, and enhanced pollen production will increase exposure to heat stress, alter patterns of infectious disease, and compromise air quality. These and similar direct impacts of climate change have been well covered in the scientific literature, and what we know of their likely considerable effects is discussed in the sidebar “1 Enormous uncertainties surround predictions regarding how climate change may affect human well-being. Acknowledging these uncertainties is a critical component of designing optimal approaches to mediating the health impacts of climate change.
Water scarcity is already a major global issue that carries heavy adverse health sequelae, and climate change will further destabilize access to fresh water.
A sampling of four current crises illustrates the gravity of the situation. One: In the North China Plain, where half of China’s wheat is grown, the water table is falling by as much as 3 meters/year. Two: Certain states in India are using half of their electricity budget to pump water from depths as deep as one kilometer to irrigate crops. Three: Roughly 300 million Chinese and Indians are eating food grown on “fossil” water that is not replenished. Four: In the Middle East and North Africa, current rates of freshwater use are equivalent to 115% of total renewable runoff.
Given such unsustainable use around the world, the number of people living in water-scarce countries is expected to rise six-fold from 470 million to 3 billion between 1990 and 2025.
OUR CHANGING CLIMATE
Carbon dioxide levels in the atmosphere exceed anything Earth has experienced in the past million years and are rapidly approaching levels not seen since the Eocene when there were no ice caps, sea level was 100 meters above current levels, and there were crocodiles near the North Pole. Global temperatures have been rising steadily for nearly 40 years; the eight warmest years on record have occurred since 2001 and the global average land-surface temperature for the period January to September 2010 was the second warmest on record behind 2007. In addition to rising mean global-surface temperatures, climatic disruption is causing other changes to the physical conditions of the planet. Among these are rising sea level and changes in the pattern of precipitation leading to more frequent droughts, floods, and forest fires, and more extreme storms.
Future trends are of even greater concern. Rapid human population growth combined with economic development begets increased water demand from homes, industry, and agriculture. In agriculture alone, the amount of water required to keep pace with global food demand—roughly 2,000–3,000 km3—represents a tripling of water used for irrigation. This is water that, in many parts of the world, simply is not available.
The availability of adequate potable water is a pillar of public health without which human well-being falters. In addition to hindering food production inadequate access to water and sanitation has direct effects on human health. Today half of the urban populations of Africa, Asia, Latin America, and the Caribbean suffer from diseases associated with inadequate access to water and sanitation, and roughly 1.7 million people die every year from these diseases.
Climate change is expected to exacerbate water scarcity in several ways. Scientists predict that the hydrologic cycle will be altered with, generally speaking, wet areas becoming wetter while dry areas become dryer. Precipitation will likely fall in greater amounts and cause more rapid runoff. Heavy precipitation events and associated runoff may make water supplies less reliable and may also make conditions favorable to outbreaks of water-borne disease. In the United States, for example, over 50% of water-borne disease outbreaks in the second half of the 20th century were preceded by precipitation events that were above the 90th percentile.2
Warmer temperatures will also increase evapotranspiration, increasing water requirements for agriculture. At the same time, the availability of water during the height of the growing season may be less owing to earlier melting of winter snowpack in the spring, leaving less water for summer irrigation. Agricultural systems dependent on glacial melt, such as the Andean nations of South America or much of Asia that receives water from the Tibetan plateau, may suffer such a fate as glaciers melt away. As these glaciers dwindle they will provide ever less dry season water flow into many of the world’s great rivers. The Indus River, for example, receives 40–50% of its dry season flow from glaciers that are rapidly receding. Finally, sea-level rise and more extreme storms will lead to coastal inundation and intrusion of salt water into freshwater aquifers, further reducing coastal freshwater supply.
Perhaps even more problematic to human welfare in the coming century than a further diminution in the availability of fresh water is the impact of climatic disruption on the supply of food. As with water, global access to food is already tenuous. In 2009 the number of people suffering from protein-calorie malnutrition exceeded one billion after reaching a low of around 830 million in the 1990s. (See Figure 1) In poor countries around the world malnutrition underlies roughly one-third of the entire burden of disease, and roughly 2 to 3 billion people—almost half the human population—already suffer from micronutrient deficiencies.
Climate change has further relevance to agricultural yields. As discussed above, climate change is expected to alter the timing and quantity of water available for agriculture while increasing the needs of plants as temperatures rise. Increased production of ground-level ozone curtails agricultural yields, as ozone is a potent plant toxin. When ozone concentrations reach 30 to 45 ppb (parts per billion), yield losses for the major grains approach 10 to 40%. By 2030 mean annual ozone concentrations in South Asia are expected to exceed 50 ppb. Increasingly intense tropical cyclones, sea level rise, more frequent forest fires, droughts, and floods will also conspire to diminish local harvests.
Despite strong evidence that climate change will increase the risk of numerous challenges to agricultural production, the net effect of climate change on global food production is difficult to quantify. Little is known, for example, about how climate change may alter the relationships between plants and their pests and pathogens, though several worrying examples indicate that climate change may promote infestations of plant pests as higher winter minimum temperatures enable insects to overwinter more effectively. Also poorly understood is how climate change will impact the extent and pattern of cloud cover which, to some degree, determines the solar radiation available to plants for photosynthesis.
In addition to these impacts on the quantity of food produced, it appears that rising concentrations of atmospheric carbon dioxide also affect nutritional quality. Grains grown at elevated concentrations of carbon dioxide appear to have reduced concentrations of protein, iron, zinc, and perhaps other nutrients. As with other examples already cited in this article, these potential decrements in plant nutritional content are of particular concern given the current state of affairs: iron and zinc deficiency account for roughly 63 million years of life lost annually, and the major grains are a critical source of these nutrients for many populations around the world.6,7 Taken together these additional threats to food production may very well have extensive impacts on human nutrition and global health.
Population displacement may be the final common pathway for many of the climate change impacts discussed above. Regional changes in precipitation leading to increased droughts and flooding, increased incidence of natural disasters like tropical cyclones and forest fires, local crop failures, and severe water scarcity are all likely to force people around the world to abandon their homes. (See Figure 2) In addition to these threats, coastal vulnerability puts many people at risk for displacement. More than one-third of the human population lives in coastal areas and on small islands that are within 100 kilometers of the shore and less than 50 meters above sea level. The combination of sea-level rise, increasingly intense storms, and destruction of coastal barriers (mangroves, wetlands, vegetated dunes, and coral reefs) leaves these populations extremely vulnerable. By 2050 an estimated 200 million to 1 billion people may be displaced due to climate change. These estimates are highly uncertain in part because many of the biophysical changes that contribute to displacement remain hard to quantify.8,9
Despite this uncertainty, a significant fraction of the human population will undoubtedly be displaced in this century, and displaced persons face stark health realities. Nonimmune populations migrating into endemic areas are more susceptible to a variety of infectious diseases. Poor housing, sanitation, and access to safe drinking water combined with poor nutrition lead to disease epidemics, particularly diarrheal disease, measles, and acute respiratory infections. Malnutrition plagues displaced populations, with rates as high as 50% seen in refugee populations in Africa.10 In addition to infectious disease and malnutrition, displaced people suffer from high rates of violence, sexual abuse, and mental illness. Post-traumatic stress disorder has been diagnosed in 30 to 75% of resettled refugee children and adolescents.11 Finally, displacement may lead to civil strife and violent conflict as large numbers of people with few resources move into areas where they frequently are not welcome.
DIRECT IMPACTS OF CLIMATE CHANGE
• Climate change will alter the distribution of malaria, dengue fever, schistosomiasis, and others that are transmitted by an insect vector or those that have animal reservoir hosts.
• The range of these diseases is limited geographically by the range of the insects and/or animal reservoirs that effect their transmission to humans. As temperature and precipitation patterns change, so too will the geography conducive to the survival of these other species.
• Warming temperatures increase the rates of reproduction, development, survival, and biting of blood-feeding vectors as well as shortening the parasite development time inside these vectors.
• Geographic shift from one locale to another may introduce pathogens into novel and nonimmune human populations who may be far more susceptible to infection than those now living in endemic areas.
• Increased extreme heat events can exact a heavy human health toll.
• Hyperthermia may cause relatively mild illness such as heat rash, exhaustion, or heat syncope (fainting), but may also precipitate severe sequelae including heat stroke, which is often fatal.
• Survivors of heat stroke experience a marked increase in illness and mortality in years subsequent to the extreme heat event.
• An additional 2.5 billion people will be added to the planet’s population over the next 40 years and nearly all of them will live in cities. Cities tend to be warmer due to the urban heat-island effect.
• The human population is aging, and the elderly are particularly sensitive to heat stress.
• The formation of ground-level ozone, the major cardiorespiratory toxin in smog, is coupled to temperature particularly as temperatures rise above 90°F (32°C).
• Climate change has brought about an earlier start to spring and later end to fall, and these changes to seasonality, along with higher CO2 concentrations, yield both longer pollen seasons and more pollen production from many allergenic plants.
• Allergic respiratory disease, particularly asthma, is already associated with a quarter of a million deaths annually worldwide.
• The frequency and extent of forest fires is expected to rise, generating large amounts of air pollutants, including potent lung irritants (such as acrolein and other aldehydes), carcinogens (such as formaldehyde and benzene) and fine particulates (PM 2.5) which are known to increase risk of cardiorespiratory disease and death.
There is no doubt that climate change will have important impacts on human health, but we are uncertain about what those impacts will be and where and when they will be most severe. The most consequential health effects of climate change will come about from interactions between biophysical changes to the natural environment, demographic trends, and human adaptations. (See Figure 3) The biophysical changes—such as temperature variability or sea level rise—are difficult to predict with accuracy today, and the capacity for adapting to these changes is largely unknown.
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