Global warming
Global warming
Global
warming is the rise in the average temperature of Earth's atmosphere and oceans
since the late 19th century and its projected continuation. Since the early
20th century, Earth's mean surface temperature has increased by about 0.8 °C
(1.4 °F), with about two-thirds of the increase occurring since 1980. Warming
of the climate system is unequivocal, and scientists are 95-100% certain that
it is primarily caused by increasing concentrations of greenhouse gases
produced by human activities such as the burning of fossil fuels and
deforestation. These findings are recognized by the national science academies
of all major industrialized nations. Future climate change and associated
impacts will vary from region to region around the globe.
The effects of an increase in
global temperature include a rise in sea levels and a change in the amount and
pattern of precipitation, as well as a probable expansion of subtropical
deserts. Warming is expected to be strongest in the Arctic, with the continuing
retreat of glaciers, permafrost and sea ice. Other likely effects of the
warming include more frequent extreme weather events including heat waves,
droughts and heavy rainfall; ocean acidification; and species extinctions due
to shifting temperature regimes. Effects significant to humans include the
threat to food security from decreasing crop yields and the loss of habitat
from inundation.
Cause of Global Warming
·
Greenhouse gases
·
Solar activity
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