The Earth experiences variability in climate trends on a range of timescales from one year to millions of years, with some intervals warmer than present and others far colder, as tanstaafl, AWB and DrFidelius pointed out. The potential range of natural climate variability, and the forcings responsible for that variability, are not fully understood. So when you read the papers and it looks as though no one really knows what’s happening, it’s true - to a point.
Because we don’t know exactly what will happen in near future (say, the next 100,000 years or so), we have to assume for the moment that we are in fact still living in an ice age; we just happen to be living during a slighlty warmer period of time, called an interglacial, between periods of major ice sheet development (glacials). The oscillation between cold and warm intervals is referred to as the glacial-interglacial cycle.
The present interglacial (i.e., the Holocene Epoch, 10,000 BP to present) has itself been marked by shorter-term climate fluctuations including intervals as warm as (or warmer) than today (the Holocene Climatic Optimum [9,000-7,000 BP] and the Secondary Optimum [1000-1200 AD]), as well as colder times (the Iron Age cold epoch [2900-2300 BP] and the Little Ice Age [1400-1700 AD]). Our current climatic conditions are part of a naturally warmer phase that began around 1700.
What many scientists have finally reached a consensus upon is that at least SOME of the present global warming trend can be accounted for by anthropogenic activity, e.g., burning of fossil fuels, use of CFC’s and HCFC’s. The level of carbon dioxide in the atmosphere has increased from about 280 ppm in 1800 (the “pre-industrial value”) to about 315 ppm in 160, to roughly 360 ppm today - so the increase is NOT linear.
Contrary to popular belief, “global warming” doesn’t mean that every spot on the Earth will get warmer - the average global temperature will rise because the difference between daytime maximum temperatures and nighttime minimum temperatures will diminish. However, regional variability can still result in some areas getting somewhat cooler than the are now, and precipitation patterns ought to change noticeably.
Although there continue to be debates about whether or not the warming trend will continue (or whether any anthropogenic interference will contribute to longer-term cliamtic change), I have to agree with DrFidelius that we shouldn’t continue to burn fossil fuels just because we can. This is our first (and maybe only) home - we ought to take care of it better.
A few more quick points:
kylen, continental ice sheet buildup begins when winter snow precipitation is high and summer temperatures are not warm enough to completely melt all the snow. (We’ll assume here that ice sheet buildup begins at high latitudes to make the process a bit easier.) Putting an exact number on the required drop in global average termperature that would permit this scenario is tricky business, because the present computer models (from which such estimates are often derived) aren’t perfect. That’s not to say, though, that a drop of 1 or 2 degrees in global avg. temp wouldn’t have an impact on climatic patterns at all. The current global avg. temp. has increased by 0.5 degrees since last century.
falcon2, annual to decadal climate variability is likely connected to short-term solar variability (e.g., the sunspot cycle), but it is not yet clear that the decades-long warming trend in the 20th century be explained entirely in this way. The present data also do not suggest that anthropogenic negative climate feedbacks (such as sulfur dioxide) are balancing out the positive feedbacks (carbon dioxide and CFCs), else we wouldn’t see a warming trend. BTW, if you live in a coastal area you should care very much if the East Antarctic ice sheet shows signs of collapsing, because the melting of all that ice into the ocean may raise global sea level by as much as several tens of meters.
DrFidelius, while atmospheric temps have been measured in realtime by reliable instruments for only the last century or so, we can still determine reliable temperature measurements for the last several thousand years through a variety of proxies, including gases dissolved in groundwater, tree-ring data, and lake sediments. Individual methods may not be absolutely perfect, but the combined data yield a pretty good picture of cliamte in the recent past.