The climate changes expected from increased atmospheric concentrations of
greenhouse gases are likely to have widespread effects, many of them
negative, on ecological systems, human health, and socioeconomic
sectors. In general, people in developing countries are more vulnerable
to climate change because of limited infrastructure and capital and
greater dependence on natural resources. Unless otherwise specified, the
impacts and vulnerabilities discussed below are based on scenarios of
doubling of current levels of CO2 by 2100 (700 ppm). Beyond such
concentrations, impacts appear to worsen, but uncertainty about what will
happen increases. In general, uncertainty cuts both ways: outcomes could
be less dramatic than expected based on our current understanding, but
could just as well be much more severe.
Worsening Health Effects - Climate change will impact human
health in a variety of ways. Warmer temperatures increase the risk of
mortality from heat stress. For example, in July 1995, 465 deaths in
Chicago were attributed to a heat wave with temperatures exceeding
90o F day and night. Today, such events occur about once
every 150 years. By 2100, they could become six times more frequent.
The potential increases in the heat index, a calculation combining
temperature and humidity, illustrate the magnitude of this threat.
Washington, D.C. currently has an average July heat index of
85o F, but if CO2 levels reach 550 ppm (double the
preindustrial level), this could increase to 950 F, and if
concentrations quadrupled to 1100 ppm, it could increase to
110o F. Climate change will also exacerbate air quality
problems, such as smog, and increase levels of airborne pollen and spores
that aggravate respiratory disease, asthma, and allergic disorders
(Figure 15). Because children and the elderly
are the most vulnerable populations, they are likely to suffer
disproportionately with both warmer temperatures and poorer air quality.
Diseases that thrive in warmer climates, such as malaria, dengue and
yellow fevers, encephalitis, and cholera, are likely to spread due to the
expansion of the ranges of mosquitos and other disease-carrying organisms
and increased rates of transmission. This could result in 50 million to
80 million additional malaria cases per year worldwide by 2100.
Rising Sea Level - Rising sea level erodes beaches and coastal
wetlands, inundates low-lying areas, and increases the vulnerability of
coastal areas to flooding from storm surges and intense rainfall. By
2100, sea level is expected to rise by 6 to 37 inches. A 20-inch sea
level rise will result in substantial loss of coastal land in the United
States, especially along the southern Atlantic and Gulf coasts, which are
subsiding and are particularly vulnerable. The oceans will continue to
expand for several centuries after temperatures stabilize. Because of
this, the sea level rise associated with CO2 levels of 550 ppm (double
pre-industrial levels) could eventually exceed 40 inches. A CO2 level of
1100 ppm could produce a sea level rise of 80 inches or even more,
depending on the extent to which the Greenland and Antarctic ice sheets
melt.
A 20-inch sea level rise would double the global population at
risk from storm surges, from roughly 45 million at present to over 90
million, and this figure does not account for any increases in coastal
populations. A 40-inch rise would triple the number.
South Florida is highly vulnerable to sea level rise (Figure 16). A third of the Everglades has an elevation
of less than 12 inches. Salt water intrusion would adversely affect
delicate ecological communities and degrade the habitat for many species.
Disruption of the Water Cycle - Among the most fundamental
effects of climate change are intensification and disruption of the water
cycle.
Droughts and floods - Intensification of the water cycle will
produce more severe droughts in some places and floods in others. Such
events are costly. Damages from the Southern Plains drought of 1996 were
estimated at $4 billion, the 1993 Mississippi River flood damages at $10
billion to $20 billion, the Pacific Northwest floods in the winter of
1996-1997 at about $3 billion, the 1997 Ohio River flood at about $1
billion, and the 1997 Red River flood in the Northern Plains at about $2
billion.
Water quality and quantity - Areas of greatest vulnerability are
those where quality and quantity of water are already problems, such as
the arid and semi-arid regions of the United States and the world (Figure
17).
Climate change would likely increase water supply problems in
several U.S. river basins, such as the Missouri, Arkansas, Texas Gulf,
Rio Grande, and Lower Colorado.
Water scarcity in the Middle East and Africa is likely to be
aggravated by climate change, which could increase international tension
among countries that depend on water supplies originating outside their
borders.
Changing Forests and Natural Areas - Climate change could
dramatically alter the geographic distributions of vegetation types. The
composition of one-third of the Earth's forests would undergo major
changes as a result of climate changes associated with a CO2 level of 700
ppm. Over the next 100 years, the ideal range for some North American
forest species will shift by as much as 300 miles to the north, far
faster than the forests can migrate naturally. Economically important
species, such as the sugar maple, could be lost from New England by the
end of the next century (Figure 18).
Such changes could have profound effects on the U.S. system of national
parks and refuges, leading to reductions in biological diversity and in
the benefits provided by ecosystems, such as clean water and recreation.
Wetlands are particularly at risk. The wetlands of the prairie pothole
region, which support half the waterfowl population of North America,
could diminish in area and change dramatically in character in response
to climate change. The glaciers of Glacier National Park have receded
steadily for decades (Figure 19). Model projections indicate that all
the ParkÕs glaciers will disappear by 2030 unless temperatures begin to
cool instead of warm.
Challenges to Agriculture and the Food Supply - Climate strongly
affects crop yields. A CO2 concentration of 550 ppm is likely to
increase crop yields in some areas by as much as 30 percent to 40
percent, but it will decrease yields in other places by similar amounts,
even for the same crop. A warmer climate would reduce flexibility in
crop distribution and increase irrigation demands. Expansions of the
ranges of pests could also increase vulnerability and result in greater
use of pesticides. Despite these effects, total global food production
is not expected to be altered substantially by climate change, but there
are likely negative regional impacts. Agricultural systems in the
developed countries are highly adaptable and can probably cope with the
expected range of climate changes without dramatic reductions in yields.
It is the poorest countries, already subject to hunger, that are the most
likely to suffer significant decreases in agricultural productivity
(Figure 20).
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