1. G lobal warming For past climate change see Paleoclimatology and Geologic temperature record. For scientific and political disputes, see Global warming controversy and Climate change consensus.1880-2009 global mean surface temperature difference relative to the 1961–1990 averageclimate changePaleoclimatology Geologic temperature recordGlobal warming controversyClimate change consensusmean Comparison of ground based (blue) and satellite based (red: UAH; green: RSS) records of temperature variations since 1979. Trends plotted since January 1982.UAHRSS Mean surface temperature change for the period 2000 to 2009 relative to the average temperatures from 1951 to 1980. [1] [1] Global warming is the increase in the average temperature of Earth's near-surface air and oceans since the mid-20th century and its projected continuation. According to the 2007 Fourth Assessment Report by the Intergovernmental Panel on Climate Change (IPCC), global surface temperature increased 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 20th century. [2][A] Most of the observed temperature increase since the middle of the 20th century has been caused by increasing concentrations of greenhouse gases, which result from human activity such as the burning of fossil fuel and deforestation. [3] Global dimming, a result of increasing concentrations of atmospheric aerosols that block sunlight from reaching the surface, has partially countered the effects of warming induced by greenhouse gasesaverage temperatureEarthFourth Assessment Report Intergovernmental Panel on Climate ChangeCF [2][A]causedgreenhouse gases human activityfossil fuel deforestation [3]Global dimmingaerosols

2. G lobal warming Climate modelClimate model projections summarized in the latest IPCC report indicate that the global surface temperature is likely to rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century. [2] The uncertainty in this estimate arises from the use of models with differing sensitivity to greenhouse gas concentrations and the use of differing estimates of future greenhouse gas emissions. An increase in global temperature will cause sea levels to rise and will change the amount and pattern of precipitation, probably including expansion of subtropical deserts. [4] Warming is expected to be strongest in the Arctic and would be associated with continuing retreat of glaciers, permafrost and sea ice.surface temperature [2] sensitivity to greenhouse gas concentrations estimates of future greenhouse gas emissionssea levels to riseprecipitationsubtropicaldeserts [4]strongest in the Arcticretreat of glaciers permafrostsea ice

3. G lobal warming

4. Other likely effects include changes in the frequency and intensity of extreme weather events, species extinctions, and changes in agricultural yields. Warming and related changes will vary from region to region around the globe, though the nature of these regional variations is uncertain. [5] As a result of contemporary increases in atmospheric carbon dioxide, the oceans have become more acidic, a result that is predicted to continue. [6][7]extreme weatherspecies extinctionsagricultural yields [5] more acidic [6][7] The scientific consensus is that anthropogenic global warming is occurring. [8][9][10][B] Nevertheless, political and public debate continues. The Kyoto Protocol is aimed at stabilizing greenhouse gas concentration to prevent a "dangerous anthropogenic interference". [11] As of November 2009, 187 states had signed and ratified the protocol.scientific consensus anthropogenic [8][9][10][B] politicalpublic debateKyoto Protocol [11] 187 states had signed and ratified

5. G lobal warming Greenhouse gases Main articles: Greenhouse effect, Radiative forcing, and Atmospheric CO2Greenhouse effect schematic showing energy flows between space, the atmosphere, and earth's surface. Energy exchanges are expressed in watts per square meter (W/m 2 ).Greenhouse effectRadiative forcing Atmospheric CO2 Recent atmospheric carbon dioxide (CO 2 ) increases. Monthly CO 2 measurements display seasonal oscillations in overall yearly uptrend; each year's maximum occurs during the Northern Hemisphere's late spring, and declines during its growing season as plants remove some atmospheric CO 2.carbon dioxideNorthern Hemisphere The greenhouse effect is the process by which absorption and emission of infrared radiation by gases in the atmosphere warm a planet's lower atmosphere and surface. It was proposed by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. [32] The question in terms of global warming is how the strength of the presumed greenhouse effect changes when human activity increases the concentrations of greenhouse gases in the atmosphere.greenhouse effectabsorptionemissioninfrared atmosphereplanetJoseph FourierSvante Arrhenius [32]

6. G lobal warming

7. ผู้จัดทำ นอธิภัทร รวมทรัพย์ 5211000684 อก. ภาควิชา วิทยาศาสตร์และเทคโน ดลยีการอาหาร