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What Is This Indicator, and Why Is It Important?
This indicator will describe the difference between urban
and rural air temperatures for major U.S. metropolitan areas.
Temperatures within urban areas will be compared to those
in less-developed surrounding areas.
Extremely hot weather is responsible for greater loss of
human life in the United States than hurricanes, lightning,
tornadoes, floods, and earthquakes combined. Building density
and type, amount of road surface, and energy use, as well
as local topography and regional weather patterns, all work
together to modify a citys climate. The urban heat island
effect is often noticed most at night when buildings and other
constructed surfaces radiate the heat they have accumulated
during the day. Beyond posing a threat to human health (through
heat stroke, for example) and raising air conditioning costs,
the heat island effect can cause physiological stress in other
animals, change the mix of plants and animals that live in
the area, and even lead to changes in the distribution of
pathogens. Elevated temperatures also accelerate the formation
of ground-level ozone (see Air Quality)
and other air pollutants that adversely affect human health.
Why Can't This Indicator Be Reported at This Time?
There is no single metric that has been adopted
by the scientific community as an indicator of the heat island
effect. One possible presentation would report the percentage
of all U.S. metropolitan areas where the average annual difference
between urban and rural air temperatures is relatively small
(less than 7ºF), moderate (7º to less than 13ºF),
or large (more than 13ºF).
National Weather Service data could be used to determine
current and historic heat island effects in many locations.
However, there is no program in place either to retrieve and
analyze historic information or to identify appropriate pairs
of urban and rural sites necessary to make calculations of
the heat island effect.
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