The concept of the greenhouse
effect, which underlies global warming, evolved from a series of observations
dating back to the early nineteenth century. In 1826, Joseph Fourier calculated
that the Earth’s temperature, if it were warmed only by the sun, would be 60ºF
(15.5ºC) cooler and further surmised that the atmosphere served as an insulator
that prevented heat loss. Later, in 1859, John Tyndall discovered that water
vapor and carbon dioxide (CO2) in the atmosphere were responsible
for this heat trapping. In 1896, Svante Arrhenius noted a quantitative
relationship between the concentration of atmospheric carbon dioxide (CO2)
and the average surface temperature of the Earth. He called this phenomenon
hothouse, which a decade later was renamed “the greenhouse effect.”
Overwhelmingly, the
scientific community has attributed this temperature rise to an increase in
greenhouse gases (GHG). The most important GHG are water vapors and CO2,
with human activity responsible for most of the CO2. Sources of this
gas are fossil fuels used by cars, factories, electricity production, and
deforestation. The Intergovernmental Panel on Climate Change (IPCC) projects a
further average rise of 2–5.2ºF (1.1–2.9ºC) during this century, to be most
extreme in the Arctic, leading to glacial melting. Other predicted consequences
of global warming include more extreme weather (heat waves, drought, heavy
rain), decreased crop yields, changes in migratory patterns of animals, a
decrease in biodiversity, and plant and animal species extinction.
Some scientists predict that global warming will cause more extreme weather, including abnormally persistent periods of drought and heavier rainfall. |
The IPCC, a United Nations
group with representatives from all major industrialized nations, and virtually
all national scientific academies agree that both the Earth’s surface
temperature and the rate of warming of the atmosphere and oceans have been
rising faster in recent decades. Some scientists and members of the general
population, however, question whether these temperature changes are within
normal climatic variation, if human activities are responsible for their
occurrence, and what the appropriate measures for its remediation may be. Some
of these questions undoubtedly arise from sincere differences in the
interpretation of the data, while others are motivated by political,
philosophic, or economic considerations.
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