Monday, October 17, 2011
Combined land/sea surface temperatures since the late 1800s
Friday, October 7, 2011
Extent of multi-year ice in the Arctic
Thursday, October 6, 2011
Ocean heat content since WWII
Northern Hemisphere snow cover since 1920
Sea level changes since 1870
Tuesday, October 4, 2011
Wednesday, September 7, 2011
Cosmic rays and climate change
Tuesday, April 26, 2011
Friday, March 4, 2011
Thursday, February 10, 2011
Does carbon dioxide cause warming?

Using Planck's equation to overlay the amount of incoming solar radiation to outgoing thermal radiation, and you can see that the top of the outgoing thermal radiation curve aligns nicely with the carbon dioxide curve - this means that incoming light goes through the carbon dioxide but is absorbed going out.

So yes, basic radiative physics shows that carbon dioxide does cause warming.
2.1 million year record of carbon dioxide levels
Thursday, January 13, 2011
Global Average Temperatures since 1880
Saturday, January 8, 2011
Carbon isotope signatures in coral skeletons
Short refresher on carbon isotopes: Burning of fossil fuels adds huge amounts 12C to the atmosphere which should yield declining 13C/12C ratios.
Sea Surface Temperatures in Australia
Friday, January 7, 2011
Carbon Dioxide Forcing

And the IPCC's illustration of carbon dioxide forcing relative to other factors:

So it's clear that carbon dioxide is a strong greenhouse gas. But what about water vapor? Water vapor is also a strong greenhouse gas, but it stays relatively constant and falls out of the atmosphere quickly (as compared to carbon dioxide which stays in the atmosphere for hundreds of years). More importantly, water vapor is a positive feedback in the climate and is very sensitive to carbon dioxide warming. That is, when carbon dioxide increases and the globe warms, the amount of water vapor in the atmosphere increases as well, due to increased evaporation, and this causes the atmosphere to get even warmer. This is a well known process, and current climate models take this into account.












