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Update 29: October
9, 2003-9
Copyright © 2003 Earth Policy Institute
RECORD HEAT WAVE IN EUROPE TAKES 35,000 LIVES
Far Greater Losses May Lie Ahead
Janet Larsen
A record heat wave scorched Europe in August 2003,
claiming an estimated 35,000 lives. In France alone, 14,802 people died
from the searing temperaturesmore
than 19 times the death toll from the SARS epidemic worldwide. In the
worst heat spell in decades, temperatures in France soared to 104 degrees
Fahrenheit (40 degrees Celsius) and remained unusually high for two weeks.
This summer's high temperatures also hit other European countries. Germany
saw some 7,000 people die from the heat. Spain and Italy each suffered
heat-related losses of nearly 4,200 lives. The heat wave claimed at least
1,300 lives in Portugal and up to 1,400 lives in the Netherlands.
In Londonwhich
on August 10th recorded its first triple-digit Fahrenheit temperaturean
estimated 900 people died from the heat. Heat-related fatalities across
the United Kingdom reached 2,045. In Belgium, temperatures higher than
any in the Royal Meteorological Society's register dating back to 1833
brought 150 deaths. Since reports are not yet available for all European
countries, the total heat death toll for the continent is likely to be
substantially larger. (See data.)
August 2003 was the warmest August on record in the northern hemisphere,
but according to the projections of the Intergovernmental Panel on Climate
Change (IPCC), even more extreme weather events lie ahead. By the end
of the century, the world's average temperature is projected to increase
by 2.5-10.4 degrees Fahrenheit (1.4-5.8 degrees Celsius). As the mercury
climbs, more frequent and more severe heat waves are in store.
Though heat waves rarely are given adequate attention, they claim more
lives each year than floods, tornadoes, and hurricanes combined. Heat
waves are a silent killer, mostly affecting the elderly, the very young,
or the chronically ill.
Under normal circumstances, humans maintain a body temperature around
98.6 degrees Fahrenheit. When subject to extreme heat, the body attempts
to maintain this ideal temperature by varying blood circulation and perspiring.
When the internal body temperature rises above 104 degrees Fahrenheit,
vital organs are at risk. If the body temperature is not brought down,
death follows.
The threshold ambient temperature at which more people are at risk for
heat-related health problems varies greatly by location. In general, when
summer temperatures range 10 degrees Fahrenheit or more above the norm,
incidences of heat-related illness increase dramatically. High humidity
compounds the effects of high heat by reducing evaporation, rendering
perspiration a less-effective cooling mechanism. When excessive heat prevails
for more than two consecutive days, the risk of heat sickness and death
escalates. Health and social services may be overwhelmed.
Heat waves take the greatest human toll in cities. Urban centers, where
the area of heat-absorbing dark roofs and pavement exceeds the area covered
by cooling vegetation, are like "heat islands" and can be as much as 10
degrees Fahrenheit warmer than the surrounding countryside. While people
in rural areas generally get some relief from the heat when temperatures
fall at night, urban areas stay warmer around the clock. Air pollution,
which usually is worse in cities than in the countryside, can also exacerbate
the health-damaging effects of high temperatures by further stressing
the body's respiratory and circulatory systems.
Several of the worst heat waves of the twentieth century occurred in U.S.
cities. In 1955, an eight-day run of temperatures over 100 degrees Fahrenheit
in Los Angeles left 946 people dead. In 1972, New York City suffered a
two-week heat wave that claimed 891 lives. More recently, an extreme heat
wave in Chicago in 1995 killed 739 people in a matter of days. Slow political
recognition of the threat and an overloaded response system worsened the
effects of the weather anomaly.
A lack of public recognition of the danger that high temperatures pose
adds to the lethality of heat waves. Heat wave warnings often do not carry
the weight of other natural disaster alerts. Except during major outbreaks,
heat-related deaths often go unreported, and few governments systematically
keep records of them.
Even once a heat wave has passed, politicians are reluctant to acknowledge
its toll. Chicago's mayor denied the severity of the city's 1995 heat
wave. In Europe, it took over a month for France's government to release
heat wave fatality estimates that corroborated estimates from overwhelmed
undertakers. Several neighboring governments are still challenging reports
from medical examiners.
Even in India, where heat-related fatalities in the thousands during pre-monsoonal
high temperatures are no longer uncommon, the National Disaster Management
Cell does not classify heat waves as a natural disaster. While accurate
data are hard to come by, it appears that India has seen the number of
deaths due to heat climb over the years as populations have grown and
temperatures have risen. In May 2003, peak temperatures of 113-117 degrees
Fahrenheit (45-49 degrees Celsius) claimed over 1,600 lives throughout
the country. In the state of Andhra Pradesh alone, some 1,200 people died
from the heat. A year earlier, a one-week heat wave with temperatures
topping 122 degrees Fahrenheit took over 1,000 lives.
Over the last 25 years the average global temperature rose by 1 degree
Fahrenheit, or 0.6 degrees Celsius. The IPCC's projected rise in temperature
for this century is a global average, but the temperature is expected
to rise more over land, where people live, than over sea. As temperatures
continue to climb, the toll of heat waves in individual countries could
jump from the thousands to the tens of thousands. The World Meteorological
Organization estimates that the number of heat-related fatalities could
double in less than 20 years.
Already we are seeing evidence of more frequent heat waves. In India,
death tolls from heat that were recorded over an entire summer some 10
years ago are now occurring in just one week. In the United States, a
1998 study of summertime temperatures using data from 1949 to 1995 found
that the frequency of extremely hot and humid days and the occurrence
of multiple-day heat waves increased significantly during that period.
Some of the increase is due to urbanization, a trend that is expected
to continue for the foreseeable future.
Although the historical data for heat waves leave much to be desired,
we can say with confidence that the August heat wave in Europe has broken
all records for heat-induced human fatalities. As awareness of the scale
of this tragedy spreads, it is likely to generate pressure to reduce carbon
emissions. For many of the millions who suffered through these record
heat waves and the relatives of the tens of thousands who died, cutting
carbon emissions is becoming a pressing personal issue.
Copyright
© 2003 Earth Policy Institute
FOR ADDITIONAL INFORMATION
From Earth Policy Institute
Lester R. Brown, Plan
B: Rescuing a Planet Under Stress and a Civilization in Trouble
(New York: W.W. Norton & Company, 2003).
Lester R. Brown, Janet Larsen, and Bernie Fischlowitz-Roberts,
The Earth
Policy Reader (New York: W.W. Norton & Company, 2002).
Lester R. Brown, Eco-Economy:
Building an Economy for the Earth (New York: W.W. Norton & Company,
2001).
Lester R. Brown, "Global Temperature Near Record for 2002,"
Eco-Economy Update, 11 December
2002.
From Other Sources
David R. Easterling, et al., "Climate Extremes: Observations,
Modeling, and Impacts," Science, vol. 289 (22 September 2000),
pp. 2068-74.
Dian J. Gaffen and Rebecca J. Ross, "Increased Summertime
Heat Stress in the U.S.," Nature, vol. 396 (10 December 1998).
Additional information available at http://www.arl.noaa.gov/milestn/mile3.html.
Goddard Institute for Space Studies, NASA Goddard Space
Flight Center, Earth Sciences Directorate, "Global Temperature Anomalies
in .01 C," http://www.giss.nasa.gov/data.
Intergovernmental Panel on Climate Change, Climate
Change 2001: The Scientific Basis; Impacts, Adaptation, and Vulnerability;
and Mitigation. Contributions of Working Group I, II, and III to the Third
Assessment Report of the Intergovernmental Panel on Climate Change
(Cambridge and New York: Cambridge University Press). Text and summaries
of each report available at http://www.ipcc.ch.
LINKS
The Center for Climatic Research's Synoptic Climatology
Lab
http://www.udel.edu/SynClim
Environmental Protection Agency's Heat Island Page
http://yosemite.epa.gov/oar/globalwarming.nsf/content/ActionsLocalHeatIslandEffect.html
Intergovernmental Panel on Climate Change
http://www.ipcc.ch
National Center for Atmospheric Research, Heat Wave Awareness
Project
http://www.esig.ucar.edu/heat/index.html
National Climatic Data Center
http://www.ncdc.noaa.gov/oa/ncdc.html
National Weather Service, Office of Climate, Water, and
Weather Services, Natural Hazard Statistics
http://www.nws.noaa.gov/om/hazstats.shtml
U.S. Centers for Disease Control and Prevention, National
Center for Environmental Health, Extreme Heat Page
http://www.cdc.gov/nceh/hsb/extremeheat
Worldwatch Institute
http://www.worldwatch.org
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