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New approach to determining human impact on climate gives same answer

Although some people continue to question whether Earth's temperatures have actually warmed significantly over the last century, the focus of many has shifted to cause: while the world has clearly warmed, a lot of people have suggested that the cause of that warming is "up for debate." Many studies have looked at that question and determined that human activity is the primary driver, as the 2007 IPCC report concluded. A paper published this week in Nature Geoscience makes a novel contribution to this question, even as it comes up with the same answer.

Previous work has primarily used observations of temperature trends (from the deep ocean or the lower atmosphere) combined with computer modeling to assess the cause of warming. For example, the latest IPCC report showed climate models run with and without the effect of greenhouse gases to illustrate that temperatures would have been stable without anthropogenic warming.

The new study, published by researchers from the Institute for Atmospheric and Climate Science at ETH in Switzerland, directly examined Earth’s energy balance instead.

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Last big chill suggests lower climate impact of carbon

One of the key measures of the impact of atmospheric carbon dioxide is called the climate sensitivity, which provides an estimate of how much the planet will warm in response to a doubling of the CO2 concentration. This figure has been estimated using a variety of methods, producing a range of values; the Intergovernmental Panel on Climate Change estimates that the most likely value is 3 Kelvin, but recognizes there's a reasonable chance it could range anywhere from 2.4-4.5K. A new study that uses a climate model to evaluate the peak of the last glacial period, however, suggests that the IPCC's figure might be a bit high, and that very high values are overwhelmingly unlikely.

Glacial periods are triggered by small changes in the Earth's orbit. These aren't enough by themselves to alter the global climate, but they set off a drop in atmospheric CO2 and an expansion of ice, which reflects sunlight back to space. These feedbacks help the Earth enter a deep chill during glacial periods.

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