Yes, this is not some groundbreaking new assertion. In fact it is things like this - feedback mechanisms (both positive and negative) that make climate change modelling so hard. If it was a simple matter of "C02 creates more warmth" we'd have figured it all out a while ago. More warmth can produce more water vapor, but depending on what type of clouds are formed you can end up with trapped heat, or more solar radiation reflected and a cooling effect. There are many other feedback mechanisms that I simply can't recall and many more I've never heard of. How and when they respond, and how they interact makes for a very difficult and complex problem indeed.
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