Alright, let me lay it out for youo and you can tell me where the problem is. I'll begin by posting an article I'm currently working on for a website I'm building. It is a far more extensive description than the one given at the link in my sig.
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The greenhouse effect is largely dependent on solar variation. The energy, or radiation, that the Sun sends to the Earth is in the ultraviolet, visible and infrared regions of the electromagnetic spectrum. Solar energy, or energy below 4µm, is collectively known as shortwave radiation. When that radiation hits the atmosphere some of it is redirected via a process known as dimming, caused by aerosols such as sulfur dioxide, or surfaces with high albedo, such as snow. That radiation that does make it to the surface is absorbed and re-emitted according to Kirchoff's Law of Thermal Radiation, which states that any object at some non-zero temperature radiates electromagnetic energy. According to Planck's Radiation Law the emitted radiation varies in frequency and wavelength dependent on the temperature of the object. While the Sun emits 99% of it's radiation below 4µm, the Earth, being much cooler than the Sun, emits radiation at a longer wavelength. Although historically climate feedbacks and temperatures have reacted to an increase or decrease of solar variability an analysis of recent trends indicates that solar irradiance has actually declined in the last few decades (Lockwood, 2008; Lockwood, 2010) while greenhouse gas concentration, specifically carbon dioxide, has increased (Keeling, 2005) and the global surface temperature trend has been positive (Brohan, 2006).
From Joseph Fourier's theories on heat transfer (Fourier, Freeman, 1878), John Tyndall's discovery of the greenhouse effect (Tyndall, 1861) and Svante Arrhenius's theory of carbonic acid's contribution to surface warming (Arrhenius, 1896) to the most recent IPCC (Intergovernmental Panel on Climate Change) report we've come a long way in understanding the effects different gases have in the atmosphere. As I explained previously, most radiation in the atmosphere above 4µm comes from black-body radiation emitted by objects heated up by absorbing shorter wavelength radiation. Greenhouse gases have the ability to absorb energy at these longer wavelengths. Specifically between 4µm and 100µm. Though absorption of higher energy modes is possible it is largely inconsequential to the greenhouse effect as those frequencies are not emitted by the Earth's surface. When this electromagnetic radiation strikes a molecule with an uneven distribution of electric charges, called an electric dipole, and a matching absorption frequency it causes the molecule to oscillate or vibrate which in turn either re-emits the energy or converts it into kinetic energy. This increase in kinetic energy is what we perceive as an increase in temperature. If a collision with another molecule occurs the energy is again converted into vibrational energy which can be re-emitted. This interconverting between vibrational energy, kinetic energy and infrared light continues until it can escape into space unimpeded. This process keeps temperatures approximately 33° warmer than if these gases were not present. The greenhouse effect is an essential part of keeping our planet hospitable and helps in maintaining life. However, as both greenhouse gas concentration and, as a result, downward longwave radiation (DLR) or back radiation increase a greater amount of energy is being trapped in the troposphere resulting in more heating at or near the surface which may have deleterious effects for certain types of organisms that have not adapted to that temperature rise.
Radiative forcing refers to how much of an influence a climatic factor has in altering the balance of energy at the tropopause, or the boundary between the troposphere and stratosphere. It is a technique to assess and compare both natural and anthropogenic aspects of climate change. All climatologists, no matter what their views on this issue, all seem to agree on the basic concept of radiative forcing. Sometimes, however, disagreements come into play when discussing the values. The IPCC, or Intergovernmental Panel on Climate Change, a body consisting of thousands of scientists, economists and others who ****fy as experts in their fields of study, set the values of each anthropogenic forcing to those shown in Image 1.5 in their 2005 report. The average rate of change of specific radiative forcing components, such as those attributed to greenhouse gases, has increased since the beginning of the industrial era to a rate which has not been exceeded for over 20,000 years, the time period of the ice core data (Joos, 2008).
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That is as far as I've gotten so far on that small section. Previously I also discussed the Suns role in past climate changes. In my next chapter I plan on providing the evidences that the greater amount of CO2 concentration (http://scrippsco2.ucsd.edu/data/in_situ_co2/monthly_mlo.csv) is causing the warming.
Outbound longwave radiation decreasing at CO2 absorption wavelengths - http://journals.ametsoc.org/doi/pdf/10.1175/JCLI4204.1
Downward longwave radiation increasing at CO2 absorption wavelengths - http://www.agu.org/pubs/crossref/2009/2009JD011800.shtml
Tropospheric warming combined with upper atmospheric cooling -http://www.ann-geophys.net/16/1501/1998/angeo-16-1501-1998.pdf
Nights warming faster than days -http://www.knmi.nl/publications/fulltexts/2005jd0062903.pdf
13C to 12C atmospheric ratio changes -http://scrippsco2.ucsd.edu/publications/sioref4_2001.pdf
Ocean acidifcation during a warming period -http://www.bu-eh.org/uploads/Main/doney_ann_rev_proof.pdf
Decreasing O2 atmospheric concentration -https://bluemoon.ucsd.edu/publications/manning/ManningandKeeling2006.pdf
Now this is the second or third time I've posted these links. If you'd like me to post the parts concerning how solar input is not the cause of the recent warming I can do that as well. Note that the links above go to actual scientific studies and data from real scientists.
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