gene90 wrote
I disagree with you on the science, but admit that it isn't cut-and-dry.
Again I ask, what part of the science do you disagree with?
Are you disputing that humans have significantly changed the energy balance of the earth system? That we have significantly changed the aerosol loading and distribution?
Are you just quibbling about the details? What?
Gerhard, Lee. Climate Change: Conflict of Observational Science, Theory, and Politics. AAPG Bulletin. Volume 88. Number 9. September, 2004. pp. 1121-1220.
In the above, the case is explicitly made for current warming to be due to solar forcing. See figure 3 on page 1216.
This is not a peer reviewed journal, as such it must be looked at as basically a magazine (i.e. it reflects the opinions of the editor). Also, as such, it is not archived in scientific databases so I cannot access it.
If you looked at the references I provided you will note that the influence of the sun is explicitly examined. These were peer reviewed journals, and ones with high ISI rankings. The sun is a forcing, and its variance must be included in long term climate models, but it just has not changed enough lately to be a major factor in recent climate. We have satellites that measure solar output in various bands, there are also various paleoclimatological databases.
Basketcase wrote
Eminently true. BUT--how much additional energy is being trapped by 100 additional parts per million of CO2, how much will the planet warm up as a result, and how long is the waiting time for that trapped energy to warm up the planet?
Now you are getting to the important questions. We know how much additional energy is being trapped, but only with respect to an unchanging atmosphere. It is on the order of a percent.
How much will the planet warm? This is somewhat unclear, it depends on the time scale you refer to and what feedbacks you admit. Best current models suggest that a level of 400 ppm will lead to about 2 degrees (C) warming. This amount of warming is expected to have large effects on natural ecosystems, and lead to the break up of the West Antartic ice sheet. At 550 ppm, about 3 degrees warming is expected, and a high probability of disruption of the oceanic thermohaline circulation.
How long? Again, depends on feedbacks, but best estimates suggest about 70 years for the affects to be fully realized. I saw a talk on this topic recently, and there will be some publications coming out during 2005. But it isn't really that important, what is more important is what the additional energy does to the earth system. As in my examples above of ice sheets and thermohaline circulation. This is where the greatest uncertainty exists.
One interesting thing is that we are entering a level of tropospheric opacity never seen in paleoclimatological records, never. Also, because we are already in a warm period (for the last half million years anyway), another few degrees warming and we are again in uncharted territory.