Sqrl said:
CrazyHorse said:
That was largely the point I was trying to make on the first issue and I think we are agreement on the second point also.
I am interested in your opinion on another point though. When we were discussing the Vostok Ice Core data earlier, I think we were largely agreed that it was an initial increase in temperature (due to orbital changes) which likely acted as a mechanism for increasing atmosphoric CO2 (through warming of the oceans). However, I raised the issue that the temperature and CO2 continued to increase (over ~10k years) and suggested that CO2 may have created a feedback which further increased temperatures. If was true then it implies that human emissions will increase the Earth's temperature. I'm not saying that I definately believe this to be the case (and as usual there are many factors at play), only that it is a possibilty and was curious as to your opinion on that point?
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The proposition that earth orbit could have a catalyst effect like what you're talking about seems plausible enough in principle, but whether the C02 released as a result was responsible for continued warming is something specific period data would be needed to evaluate. And I don't mind saying I'm not familiar with this specific phenomenon you're talking about.
The key issues I would look for is how much of the temperature increase cannot be explained by the catalyst effect itself. This would include looking for what impacts it might have, for instance the orbit is eccentric and so is bound to have an effect on the annual heat retention profile of the globe (ie changes in how much heat is retained from year to year) and that alone could compound in either direction. I say either direction because while a more eccentric orbit would give us periods of increased exposure during periapsis it would also mean periods of decreased exposure during apoapsis. And I have no problem admitting I've not studied what kind of effect that dynamic would have on our climate.
With that said, if you have any papers on it I'd love to read them, I've alrady added the Bamber et al paper you refered to to my list =P If this was in fact a greenhouse effect driving climate it is certainly worth studying as an invaluable comparative source for use in studying our current situation - that possibility alone is intriguing.
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The orbital variations (Milankovitch cycles) are very interesting as they largely explain the Earth's climate over the past 1 million years and I would definately recommend reading about them as you cleary have a strong interest in the subject. In case you're not familiar with the Vostok Ice Core, here is the data from wikipedia (and as it appears in published journals).
As you can see, the ice ages follow a cycle of ~100,000 years, although I made an error in my previous post as it is orbital inclination that occurs over a 100k year cycle, not eccentricity. There are other, smaller orbital cycles which also affect the climate over ~23k and 41k years. This would suggest that this orbital change may be the initial forcing factor in climate warming. The problem is that inclination is a relatively weak orbital forcing factor and so this is why some scientists suspect that it may create an initial increase in temperature but that this effect must then be magnified by other factors. These other factors are usually thought to be the greenhouse effect (as CO2 can be seen to continually increase with temperature from the data) and ice sheet response. Therefore, if the greenhouse effect is accurate it may present problems in the future as current CO2 levels are ~370ppm (higher than anytime in the past 500k years).
The paper below provides a very good overview on all the information on Milankovitch Cycles and the potential impact they have on climate coupled with possible feedback effects. It also estimates that the greenhouse effect had a ~50% effect on the temperature at the end of each ice age (i.e was responsible for 3-4 degrees warming). It's a liitle old now but it's a good summary and I'd be happy to try and find something more current if you're interested (all the recent papers I have are print outs and I don't have them with me).
Lorius et al (1992), Glacials-interglacials in Vostok: climate and greenhouse gases, Global and Planetary Change, 7;131-143.
(If you have any trouble finding it, I will be happy to send you a link)