Study: Earth’s climate more sensitive to CO2 than previously thought

Sure, I believe a nonfalsiable hypothesis about 50 million years ago vs. NASA/NOAA satellite data.

The media release is below.

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PUBLIC RELEASE: 16-NOV-2015
Study: Earth’s climate more sensitive to CO2 than previously thought
Return to hothouse climate may take less carbon dioxide than expected

BINGHAMTON UNIVERSITY

BINGHAMTON, NY – Ancient climates on Earth may have been more sensitive to carbon dioxide than was previously thought, according to new research from Binghamton University.

A team of Binghamton University researchers including geology PhD student Elliot A. Jagniecki and professors Tim Lowenstein, David Jenkins and Robert Demicco examined nahcolite crystals found in Colorado’s Green River Formation, formed 50 million years old during a hothouse climate. They found that CO2 levels during this time may have been as low as 680 parts per million (ppm), nearly half the 1,125 ppm predicted by previous experiments. The new data suggests that past predictions significantly underestimate the impact of greenhouse warming and that Earth’s climate may be more sensitive to increased carbon dioxide than was once thought, said Lowenstein.

“The significance of this is that CO2 50 million years ago may not have been as high as we once thought it was, but the climate back then was significantly warmer than it is today,” said Lowenstein.”

CO2 levels in the atmosphere today have reached 400 ppm. According to current projections, doubling the CO2 will result in a rise in the global average temperature of 3 degrees Centigrade. This new research suggests that the effects of CO2 on global warming may be underestimated.

“Take notice that carbon dioxide 50 million years ago may not have been as high as we once thought it was. We may reach that level in the next century, and so the climate change from that increase could be pretty severe, pretty dramatic. CO2 and other climate forcings may be more important for global warming than we realized.”

The only direct measurement of carbon dioxide is from ice cores, which only go back less than 1 million years. Lowenstein and his team are trying to develop ways to estimate ancient carbon dioxide in the atmosphere using indirect proxies. He said that their approach is different than any ever undertaken.

“These are direct chemical measurements that are based on equilibrium thermodynamics,” he said. “These are direct laboratory experiments, so I think they’re really reliable.

Lowenstein wants to look at nahcolite deposits in China to confirm the results found in Colorado.

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The study, “Eocene atmospheric CO2 from the nahcolite proxy,” was published Oct. 23 in Geology.

4 thoughts on “Study: Earth’s climate more sensitive to CO2 than previously thought”

  1. As has been noted, there are a lot of variables not considered. I suppose the results were verified by direct observation and analysis, so that the atmospheric mix of gasses at that time is known, the ratio of free CO2 conversion to mineral is known, and that any gain or loss of mineral concentration over time is known.

  2. The comments above miss the point. The temporal resolution of the data is +/-20,000 years. Yep, a chemical analysis of NaHCO3 (nacholite) can possibly estimate an atmospheric CO2 content, but if you can’t tell the date with +/-20,000 years then how do you tell if the temperature led or lagged the change in CO2 by days, months, decades, or millennium? All of the historical data is so temporally coarse that there is no way to tell if the CO2 content is the cause of a temperature change or the result of that change.

  3. Umm, what about the ice age where CO2 was more than 10 times today? Forget about that part, did they?

  4. And what was the water vapor content of the atmosphere at that time? Also, what other “greenhouse gasses” such as methane etc were present and in what concentrations. Also, what was the solar constant at that time? Without a decent characterization of the atmosphere and energy input the “sensitivity” calculated means nothing.

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