Give us your view of what has been happening to the Earth's climate for the last 150 years and your best forecast what will happen in the next, taking into account the lack of any significant change in the Top of Atmosphere radiative imbalance (~1.1
+0.4 W/m^2). That is, take into account that the rate at which the Earth is accumulating solar energy has not changed significantly since at least 1985.
A few handy references if you'd like to familiarize yourself with the issue. When researching this, keep in mind that "radiative forcing" is not the same thing as the "Top of Atmosphere (ToA) radiative imbalance":
An observationally based energy balance for the Earth since 1950 - Murphy - 2009 - Journal of Geophysical Research: Atmospheres (1984?2012) - Wiley Online Library
http://www.atmos-chem-phys-discuss.net/9/24731/2009/acpd-9-24731-2009-print.pdf
https://en.wikipedia.org/wiki/Radiative_forcing
What matters is the radiative imbalance | Wotts Up With That Blog
And there are many more out there, including articles disagreeing with the IPCC observations and conclusions.
I have a better one, provide us with a repeatable experiment that shows that raising CO2 caused the increased heat. You know rather then ask us to disparage YOUR theory simply prove it to us, via the Scientific method.
Then start your own thread.
For you to think no such experiment has been conducted or that no such experiment is possible - particularly considering the number of times this request of yours has already been answered - is beginning to make it look as if you just talk and never listen. There's a name for behavior like that. It begins with an S and ends with TUPID. Not the sort of behavior I'd expect from a gunny seargant.
^ "Annex II Glossary". Intergovernmental Panel on Climate Change. Retrieved 15 October 2010.
^ Jump up to: a b A concise description of the greenhouse effect is given in the Intergovernmental Panel on Climate Change Fourth Assessment Report, "What is the Greenhouse Effect?" FAQ 1.3 - AR4 WGI Chapter 1: Historical Overview of Climate Change Science, IIPCC Fourth Assessment Report, Chapter 1, page 115: "To balance the absorbed incoming [solar] energy, the Earth must, on average, radiate the same amount of energy back to space. Because the Earth is much colder than the Sun, it radiates at much longer wavelengths, primarily in the infrared part of the spectrum (see Figure 1). Much of this thermal radiation emitted by the land and ocean is absorbed by the atmosphere, including clouds, and reradiated back to Earth. This is called the greenhouse effect."
Stephen H. Schneider, in Geosphere-biosphere Interactions and Climate, Lennart O. Bengtsson and Claus U. Hammer, eds., Cambridge University Press, 2001, ISBN 0-521-78238-4, pp. 90-91.
E. Claussen, V. A. Cochran, and D. P. Davis, Climate Change: Science, Strategies, & Solutions, University of Michigan, 2001. p. 373.
A. Allaby and M. Allaby, A Dictionary of Earth Sciences, Oxford University Press, 1999, ISBN 0-19-280079-5, p. 244.
^ Jump up to: a b Wood, R.W. (1909). "Note on the Theory of the Greenhouse". Philosophical Magazine 17: 319–320. "When exposed to sunlight the temperature rose gradually to 65 °C., the enclosure covered with the salt plate keeping a little ahead of the other because it transmitted the longer waves from the Sun, which were stopped by the glass. In order to eliminate this action the sunlight was first passed through a glass plate." "it is clear that the rock-salt plate is capable of transmitting practically all of it, while the glass plate stops it entirely. This shows us that the loss of temperature of the ground by radiation is very small in comparison to the loss by convection, in other words that we gain very little from the circumstance that the radiation is trapped."
^ Jump up to: a b Schroeder, Daniel V. (2000). An introduction to thermal physics. San Francisco, California: Addison-Wesley. pp. 305–7. ISBN 0-321-27779-1. "... this mechanism is called the greenhouse effect, even though most greenhouses depend primarily on a different mechanism (namely, limiting convective cooling)."
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^ Jump up to: a b Intergovernmental Panel on Climate Change Fourth Assessment Report. Chapter 1: Historical overview of climate change science page 97
Jump up ^ The elusive "absolute surface air temperature," see GISS discussion
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Jump up ^ Grosvenor and Wesson, 1997, p. 269.
Jump up ^ "The HITRAN Database". Atomic and Molecular Physics Division, Harvard-Smithsonian Center for Astrophysics. Retrieved August 8, 2012. "HITRAN is a compilation of spectroscopic parameters that a variety of computer codes use to predict and simulate the transmission and emission of light in the atmosphere."
Jump up ^ "Hitran on the Web Information System". Harvard-Smithsonian Center for Astrophysics (CFA), Cambridge, MA, USA; V.E. Zuev Insitute of Atmosperic Optics (IAO), Tomsk, Russia. Retrieved August 11, 2012.
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Jump up ^ IPCC Fourth Assessment Report Synthesis Report: Summary for Policymakers (p. 5)
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Climate Milestone: Earth's CO2 Level Nears 400 ppm
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Or do you think all these people are just making this stuff up?
