Global Warming

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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.[2] Warming of the climate system is unequivocal, and scientists are more than 90% certain that it is primarily caused by increasing concentrations ofgreenhouse gases produced by human activities such as the burning offossil fuels and deforestation.[3][4][5][6] These findings are recognized by the national science academies of all major industrialized nations.[7][A] Climate model projections were summarized in the 2007 Fourth Assessment Report (AR4) by the Intergovernmental Panel on Climate Change (IPCC). They indicated that during the 21st century the global surface temperature is likely to rise a further 1.1 to 2.9 °C (2 to 5.2 °F) for their lowest emissions scenario and 2.4 to 6.4 °C (4.3 to 11.5 °F) for their highest.[8] The ranges of these estimates arise from the use of models with differing sensitivity to greenhouse gas concentrations.[9][10] Future climate change and associated impacts[11] will vary from region to region around the globe.[12] 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 a probable expansion of subtropicaldeserts.[13] Warming is expected to be strongest in the Arctic and would be associated with the continuing retreat of glaciers, permafrost and sea ice. Other likely effects of the warming include a more frequent occurrence of 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 tofood security from decreasing crop yields and the loss of habitat from inundation.[14][15] Proposed policy responses to global warming include mitigation byemissions reduction, adaptation to its effects, and possible futuregeoengineering. Most countries are parties to the United Nations Framework Convention on Climate Change (UNFCCC),[16] whose ultimate objective is to prevent dangerous anthropogenic (i.e., human-induced) climate change.[17] Parties to the UNFCCC have adopted a range of policies designed to reduce greenhouse gas emissions[18]:10[19][20][21]:9and to assist in adaptation to global warming.[18]:13[21]:10[22][23] Parties to the UNFCCC have agreed that deep cuts in emissions are required,[24] and that future global warming should be limited to below 2.0 °C (3.6 °F) relative to the pre-industrial level.[24][B] Reports published in 2011 by the United Nations Environment Programme[25] and the International Energy Agency[26] suggest that efforts as of the early 21st century to reduce emissions may be inadequate to meet the UNFCCC's 2 °C target.

Observed temperature changes
The Earth's average surface temperature rose by 0.74±0.18 °C over the period 1906–2005. The rate of warming over the last half of that period was almost double that for the period as a whole (0.13±0.03 °C per decade, versus 0.07±0.02 °C per decade). The urban heat island effect is very small, estimated to account for less than 0.002 °Cof warming per decade since 1900.[28] Temperatures in the lower troposphere have increased between 0.13 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Climate proxies show the temperature to have been relatively stable over the one or two thousand years before 1850, with regionally varying fluctuations such as the Medieval Warm Period and theLittle Ice Age.[29] The warming that is evident in the instrumental temperature record is consistent with a wide range of observations, as documented by many...
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