A new set of model results from Purdue University give us a foreshadowing of what the effects of global warming-induced climate disruption will be on the nation that currently puts the most greenhouse gases into the air: the United States.
In an article to be published later this week in the Proceedings of the National Academy of Sciences, geophysicist Noah Diffenbaugh and colleagues Jeremy S. Pal, Robert J. Trapp and Filippo Giorgi discuss the results of a five-month supercomputer simulation of global warming across North America over this century. This simulation exercise ranks as one of the most sophisticated ever run; the model was able to consider effects on individual regions 25 kilometers square, down from 50 square kilometers used in previous models.
It's something of an article of faith among the remaining holdouts denying the existence of global warming that computerized climate models, as they abstract aspects of the climate, are essentially useless -- and (implicitly) if they had more details, they'd show that all was right with the world. Unfortunately, as our modeling methods and technologies have gotten better, quite the opposite has occurred. These days, reports from computer models are apt to show that things are worse than we thought, climate-wise. This one is no exception:
Some of these expectations include:
The model, Diffenbaugh said, assumes that greenhouse gases will attain a concentration more than twice their current levels.
And it's that line that gives us a sliver of hope. The current atmospheric CO2 concentration is around 380ppm, so twice that is 760ppm; serious efforts to move off of a carbon-intensive global economy should allow us to keep CO2 concentration around 450-500ppm -- still higher than is safe, but potentially not disastrous. In many respects, the 760+ppm Diffenbaugh used for this simulation represents a scenario in which efforts to shift us off of carbon-intensive technologies fail. This isn't a worse-case scenario; that would be one in which we start getting dramatic greenhouse feedback effects, such as an unconstrained release of methane into the atmosphere, making the heat capture even worse.
Diffenbaugh suggests that it would take a substantially faster supercomputer to improve the results: "... we'll need a computer at least 100 times as powerful as the cluster we used to really improve the accuracy." Such a computer should be available within ten years, if current trends hold true.








