Hi Buckeye_Nut,
I've put this response together quite quickly, so I've just copy and pasted from some publications. There is a physical explanation for ice ages:
'There are various cycles in climate and the longest of those and the most important in some ways on a very long-term scale are the cycles of the ice ages. We get an ice age roughly every 100,000 years and we know what triggers ice ages; it is the variations of the earth's orbit round the sun, the variations of the eccentricity of the orbit, the variations in the tilt of the earth's orbit, and the variations of the time where the earth is closest to the sun which all vary from 100,000 years to 40,000 years to about 23,000 years. You can find all those periods within the climatic history of the last million years during which there have been around 10 ice ages...I mention the ice ages because there are people who say we are heading for another ice age so getting warmer is a good idea. The next ice age we know from astronomical data is due in something like 50,000 years' time, so it is not a concern on the timescale that even you politicians deal with!' [1]
As you stated, there is a problem with understanding natural climate variability. It is possible to make an estimate of how the climate will respond to increasing carbon dioxide levels by looking at how it has behaved in the past:
'The sensitivity of the climate system to a forcing is commonly expressed in terms of the global mean temperature change that would be expected after a time sufficiently long for both the atmosphere and ocean to come to equilibrium with the change in climate forcing... a doubling of the concentration of carbon dioxide (from the pre-Industrial value of 280 parts per million) in the global atmosphere causes a forcing of 4 watts per meter squared. The central value of the climate sensitivity to this change is a global average temperature increase of 3°C (5.4°F), but with a range from 1.5°C to 4.5°C (2.7 to 8.1°F) (based on climate system models: see section 4). The central value of 3°C is an amplification by a factor of 2.5 over the direct effect of 1.2°C (2.2°F). Well-documented climate changes during the history of Earth, especially the changes between the last major ice age (20,000 years ago) and the current warm period, imply that the climate sensitivity is near the 3°C value. However, the true climate sensitivity remains uncertain, in part because it is difficult to model the effect of cloud feedback. In particular, the magnitude and even the sign of the feedback can differ according to the composition, thickness, and altitude of the clouds, and some studies have suggested a lesser climate sensitivity. On the other hand, evidence from paleoclimate variations indicates that climate sensitivity could be higher than the above range, although perhaps only on longer time scales.' [2]
I think your point on warming being beneficial is true to some extent. There is, of course, great uncertainty with making economic assessments of climate change (the paper 'How much damage will climate change do?' [3] describes climate change impacts and is far more precise than this short description). For richer countries, climate change impacts are more likely to become negative overall with larger temperature increases. Even with small temperature increases, climate change will probably have net negative impacts with poorer countries.
'ABSTRACT. This paper examines the impact of climate change on rich and poor countries across the world. We measure two indices of the relative impact of climate across countries, impact per capita, and impact per GDP. These measures sum market impacts across the climate-sensitive economic sectors of each country. Both indices reveal that climate change will have serious distributional impact across countries, grouped by income per capita. We predict that poor countries will suffer the bulk of the damages from climate change. Although adaptation, wealth, and technology may influence distributional consequences across countries, we argue that the primary reason that poor countries are so vulnerable is their location. Countries in the low latitudes start with very high temperatures. Further warming pushes these countries ever further away from optimal temperatures for climate sensitive economic sectors.' [4]
'In contrast to human systems, the U.S. National Assessment makes a strong case that ecosystems are the most vulnerable to the projected rate and magnitude of climate change, in part because the available adaptation options are very limited... The impacts of these climate changes will be significant, but their nature and intensity will depend strongly on the region and timing of occurrence. At a national level, the direct economic impacts are likely to be modest. However, on a regional basis the level and extent of both beneficial and harmful impacts will grow. Some economic sectors may be transformed substantially and there may be significant regional transitions associated with shifts in agriculture and forestry.' [2]
[1] Sir John Houghton, edited testimony to the UK House of Lords Economic Affairs Select Committee
http://www.publications.parliament.uk/pa/ld200506/ldselect/ldeconaf/12/5011802.htm
[2] 'Climate Change Science: An Analysis of Some Key Questions', National Research Council. p6-7, 20.
http://www.gcrio.org/OnLnDoc/pdf/ClimateChangeScience.pdf
[3] Tol, R.S.J., S.Fankhauser, R.G. Richels and J.B. Smith (2000), 'How Much Damage Will Climate Change Do? Recent Estimates', FNU-2,Centre for Marine and Climate Research, Hamburg University, Hamburg.
http://www.fnu.zmaw.de/fileadmin/fnu-files/publication/working-papers/worldecon1.pdf
[4] 'The distributional impact of climate change on rich and poor countries', R. Mendelsohn, A. Dinar, L. Williams.
http://environment.yale.edu/posts/downloads/o-u/The_distributional_impact_of_climate_change.pdf