Friday, September 04, 2020

Cloud Loss and Climate Change

Recent research and updates to climate models are indicating that the global climate is more sensitive to increases in carbon dioxide than previously thought. A doubling of carbon dioxide from current levels could result in a 5.6C (10F) increase in temperatures. Part of the reason for that change in predictions is that scientists are getting a better handle on the role that clouds play in moderating global temperatures. 

Even more troubling, some research indicates that there is a tipping point in carbon dioxide levels, around 1,200 ppm. or roughly triple what it is now. This could be reached in a century or so if emissions remain at current levels. That would result in a sudden decrease in could levels and an extra 8C rise in temperatures.

Climate physicists at the California Institute of Technology performed a state-of-the-art simulation of stratocumulus clouds, the low-lying, blankety kind that have by far the largest cooling effect on the planet. The simulation revealed a tipping point: a level of warming at which stratocumulus clouds break up altogether. The disappearance occurs when the concentration of CO2 in the simulated atmosphere reaches 1,200 parts per million — a level that fossil fuel burning could push us past in about a century, under “business-as-usual” emissions scenarios. In the simulation, when the tipping point is breached, Earth’s temperature soars 8 degrees Celsius, in addition to the 4 degrees of warming or more caused by the CO2 directly.

Once clouds go away, the simulated climate “goes over a cliff,” said Kerry Emanuel, a climate scientist at the Massachusetts Institute of Technology. A leading authority on atmospheric physics, Emanuel called the new findings “very plausible,” though, as he noted, scientists must now make an effort to independently replicate the work.

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