Global warming is the rising average temperature of Earth’s atmosphere and oceans since the late 19th centuryand its proje...
Initial causes of temperature changesGreenhouse effect schematic showing energy flows between space, the atmosphere, and e...
Greenhouse gasesThe greenhouse effect is the process by which absorption and emission of infrared radiation by gases inthe...
Particulates and soot The climatic impacts from particulate forcing could have a large effect on climate through the indir...
Solar activitySolar variations causing changes in solar radiation energy reaching the Earth have been the cause ofpast cli...
Global warming and greenhouse effect
Global warming and greenhouse effect
Global warming and greenhouse effect
Global warming and greenhouse effect
Upcoming SlideShare
Loading in …5
×

Global warming and greenhouse effect

641 views
442 views

Published on

0 Comments
0 Likes
Statistics
Notes
  • Be the first to comment

  • Be the first to like this

No Downloads
Views
Total views
641
On SlideShare
0
From Embeds
0
Number of Embeds
0
Actions
Shares
0
Downloads
25
Comments
0
Likes
0
Embeds 0
No embeds

No notes for slide

Global warming and greenhouse effect

  1. 1. Global warming is the rising average temperature of Earth’s atmosphere and oceans since the late 19th centuryand its projected continuation. Since the early 20th century, Earths average surface temperature has increased byabout 0.8 C (1.4 F), with about two thirds of the increase occurring since 1980. Warming of the climate system isunequivocal, and scientists are more than 90% certain that most of it is caused by increasing concentrationsof greenhouse gases produced by human activities such as deforestation and the burning of fossil fuel.An increase in global temperature will cause sea levels to rise and will change the amount and patternof precipitation, and a probable expansion of subtropical deserts. Warming is expected to be strongest in theArctic and would be associated with continuing retreat of glaciers, permafrost and sea ice. Other likely effects ofthe warming include more frequent occurrence of extreme-weather events including heat waves, droughts andheavy rainfall ,species extinctions due to shifting temperature regimes, and changes in crop yields. Warming andrelated changes will vary from region to region around the globe, with projections being more robust in someareas than others. Hence, the ecosystem services upon which human livelihoods depend would not be preserved.
  2. 2. Initial causes of temperature changesGreenhouse effect schematic showing energy flows between space, the atmosphere, and earths surface. Energyexchanges are expressed in watts per square meter (W/m2).
  3. 3. Greenhouse gasesThe greenhouse effect is the process by which absorption and emission of infrared radiation by gases inthe atmosphere warm a planets lower atmosphere and surface.Naturally occurring amounts of greenhouse gases have a mean warming effect of about 33 C(59 F).The majorgreenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect; carbon dioxide (CO2),which causes 9–26%; methane (CH4), which causes 4–9%; and ozone (O3), which causes 3–7%.Human activity since the Industrial Revolution has increased the amount of greenhouse gases in the atmosphere,leading to increased radiative forcing from CO2, methane, tropospheric ozone, CFCs and nitrous oxides. Fossilfuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years.The rest of this increase is caused mostly by changes in land-use, particularly deforestation. CO2emissions are continuing to rise due to the burning of fossil fuels and land-use change.Emissions scenarios, estimates of changes in future emission levels of greenhouse gases, have been projected thatdepend upon uncertain economic, sociological, technological, and natural developments. In most scenarios,emissions continue to rise over the century, while in a few, emissions are reduced. Fossil fuel reserves areabundant, and will not limit carbon emissions in the 21st century. Emission scenarios, combined with modeling ofthe carbon cycle, have been used to produce estimates of how atmospheric concentrations of greenhouse gasesmight change in the future. Reduced stratospheric ozone has had a slight cooling influence on surface temperatures, whileincreased tropospheric ozone has had a somewhat larger warming effect.
  4. 4. Particulates and soot The climatic impacts from particulate forcing could have a large effect on climate through the indirect effect.Global dimming, a gradual reduction in the amount of global direct irradiance at the Earths surface, wasobserved. The main cause of this dimming is particulates produced by volcanoes and human made pollutants,which exerts a cooling effect by increasing the reflection of incoming sunlight. The effects of the products of fossilfuel combustion – CO2 and aerosols – have largely offset one another in recent decades, so that net warming hasbeen due to the increase in non-CO2 greenhouse gases such as methane. Carbon dioxide has a lifetime of acentury or more, and as such, changes in particulate concentrations will only delay climate changes due to carbondioxide. Sulfates act as cloud condensation nuclei and thus lead to clouds that have more and smaller clouddroplets. These clouds reflect solar radiation more efficiently than clouds with fewer and larger droplets, known asthe Twomey effect. This effect also causes droplets to be of more uniform size, which reduces growth ofraindrops and makes the cloud more reflective to incoming sunlight, known as the Albrecht effect. Indirect effectsare most noticeable in marine stratiform clouds, and have very little radiative effect on convective clouds.Soot may cool or warm the surface, depending on whether it is airborne or deposited. Atmospheric soot directlyabsorb solar radiation, which heats the atmosphere and cools the surface. When deposited, especially on glaciersor on ice in arctic regions, the lower surface albedo can also directly heat the surface. The influences ofparticulates, including black carbon, are most pronounced in the tropics and sub-tropics, particularly in Asia, whilethe effects of greenhouse gases are dominant in the extratropics and southern hemisphere.
  5. 5. Solar activitySolar variations causing changes in solar radiation energy reaching the Earth have been the cause ofpast climate changes. The effect of changes in solar forcing in recent decades is uncertain, but small, withsome studies showing a slight cooling effect, while others studies suggest a slight warming effect.Greenhouse gases and solar forcing affect temperatures in different ways. While both increased solar activityand increased greenhouse gases are expected to warm the troposphere, an increase in solar activity shouldwarm the stratosphere while an increase in greenhouse gases should cool the stratosphere.The magnetic activity of the sun deflects cosmic rays that may influence the generation of cloudcondensation nuclei and thereby affect the climate. The influence of cosmic rays on cloud cover is about afactor of 100 lower than needed to explain the observed changes in clouds or to be a significant contributor topresent-day climate change.Its worth noting, because this provides unequivocal evidence that the sun is not the dominant driver of globalwarming. The sun is not nearly the biggest factor in global warming. It is more evidence that greenhousegases are the largest culprit.

×