mhaze
Banned
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- Jan 10, 2007
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We know that the air is warmer, and we know that warmer air holds more water, so unless there is some other link between greenhouse gases and air moisture then this statement makes no sense. We expect to find more moisture in the atmosphere because the air is warmer, this is true regardless of how the air got to be warmer.
If this is true, if there is no other mechanism in the system to moderate or reverse this "positive feedback", then why isn't our climate like Venus due to a runaway greenhouse effect from the last warming period from 1500 years ago?
This isn't the first time the Earth has been this warm. If the warming causes the ice caps to melt, releases trapped CO2 in the permafrost, releases methane trapped under the sea, and all these countless other effects that feed this loop, then life should have ended many times over.
That I've never seen an adequate answer to this question is one of the primary reasons I'm skeptical of global warming theories.

Indeed, this simple everyday reality - that the water cycle releases heat - seems to be lost on the warmers. And then they escape into arm waving about "Intensity of severe weather events has increased".
No, it hasn't. Check this.
Is there a relation between Hurricane Intensity and Global Warming in Australia?
Nott, J., J. Haig, H. Neil, and D. Gillieson. 2007. Greater frequency variability of landfalling tropical cyclones at centennial compared to seasonal and decadal scales. Earth and Planetary Science Letters, 255, 367–372.
A team of scientists from institutions in Australia and New Zealand figured a way to do it, and here is the trick. The water that condenses in the clouds of tropical cyclones is slightly different from the water that forms in regular tropical clouds. Due to the enormous amount of water in a tropical cyclone and the height at which water condenses, the water is depleted in a particular isotope of oxygen (called the "oxygen 18 isotope" and denoted as "δ18O"). The Nott et al. team explain "An isotope gradient occurs across the cyclone with the eye wall region experiencing lowest levels of δ18O and low levels also occur within the zones of uplifted air around the cyclone known as spiral bands." It is likely that the most intense tropical cyclones will have "cloud tops at greater altitude around the eye and in spiral bands. The longevity of the system and hence the amount of rain that has occurred prior to the system crossing the coast also plays a role in the extent of isotope depletion." So if we had a water sample from each event, we could examine the δ18O level and have an index of the severity of the storm – finding the water samples sounds like a problem.
They estimate tropical cyclone intensity from AD 1226 to AD 2003, and global warmers will not be happy.
Nott et al. writes "it is clear that the period between AD 1600 to 1800 had many more intense or hazardous cyclones impacting the site than the post AD 1800 period. Seven events that were more intense/hazardous than the 1911 event occurred during this 200 yr period. Indeed the cyclone registering the lowest isotope difference value, hence the most intense or hazardous, of the entire record occurred here during this time."