Climate Change Could Diminish Valuable Cloud Cover, Scientists Say
By Tim Radford
Australian and French scientists believe they have cracked one of the great puzzles of climate change and arrived at a more accurate prediction of future temperatures.
Photo courtesy of Shutterstock
The news is not good, according to Steven Sherwood of Australia’s Centre for Excellence for Climate System Science at the University of New South Wales. If carbon emissions are not reduced, then by 2100 the world will have warmed by four degrees Celsius.
This figure does not, at first, sound high: researchers have been warning for 20 years on the basis of computer models that under the notorious business-as-usual scenario in which everybody goes on burning coal and oil, then as carbon dioxide levels double, global temperatures could rise by between 1.5 degrees Celsius and 4.5 degree Celsius.
Pessimists could cite one extreme, optimists the other: the range of uncertainty was a recognition that there were still some big unknowns in the machinery of climate, and one of those unknowns was the behavior of the clouds in a warmer world.
More warmth means more evaporation, more water vapor could mean more clouds. Low-level clouds reflect sunlight back into space, and help cool the climate a bit. This is what engineers call negative feedback.
Drying the Clouds
But if more water vapor actually led to less cloud, then more sunlight would reach the surface and the world would warm even more: positive feedback would be in play. Climate models cater for such possibilities, but cannot choose between them.
What Sherwood and his colleagues from Pierre and Marie Curie University in Paris did was to start with some real-world observations of what happens when water vapor gets into the atmosphere.
They report in Nature that updraughts of water vapor can rise 15 kilometers to form high clouds that produce heavy rains, or the vapor can rise just a few kilometers before coming back to the surface without forming rain clouds.
When this happens the process actually reduces the overall cloud cover because it desiccates the clouds above: it draws away water vapor from the higher regions in a process called convective mixing.
Climate models in the past have tended to predict high cloud formation that damps warming. What Sherwood and his colleagues have done is demonstrate that the world may not work like that.
Profound Effects in Prospect
So the next step was to feed the new understanding into computer simulations. These then showed that climate cycles could develop that would take vapor to a wider range of heights in the atmosphere, with the consequence that fewer clouds would form as climate warms.
If so—and other climate scientists will have their own arguments with the findings—then as carbon dioxide levels double, which they will do in the next 50 years or so, the average planetary temperatures will increase by a colossal four degrees Celsuis.
Governments have expressed the wish, but not so far taken the necessary action, to contain planetary temperatures to a rise of no more than two degrees Celsius. If Sherwood and colleagues are right, they will not get their wish. And the process will go on. The temperatures will continue to soar beyond 2100, to reach an additional eight degrees Celsius by 2200.
“Climate skeptics like to criticize climate models for getting things wrong, and we are the first to admit they are not perfect, but what we are finding is that the mistakes are being made by those models that predict less warming, not those that predict more,” said Sherwood.
“Rises in global average temperatures of this magnitude will have profound impacts on the world and the economies of many countries if we don’t urgently curb our emissions.”
Visit EcoWatch’s CLIMATE CHANGE page for more related news on this topic.
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A Game of Jenga<p>Think of it as a game of Jenga and the planet's climate system as the tower. For generations, we have been slowly removing blocks. But at some point, we will remove a pivotal block, such as the collapse of one of the major global ocean circulation systems, for example the Atlantic Meridional Overturning Circulation (AMOC), that will cause all or part of the global climate system to fall into a planetary emergency.</p><p>But worse still, it could cause runaway damage: Where the tipping points form a domino-like cascade, where breaching one triggers breaches of others, creating an unstoppable shift to a radically and swiftly changing climate.</p><p>One of the most concerning tipping points is mass methane release. Methane can be found in deep freeze storage within permafrost and at the bottom of the deepest oceans in the form of methane hydrates. But rising sea and air temperatures are beginning to thaw these stores of methane.</p><p>This would release a powerful greenhouse gas into the atmosphere, 30-times more potent than carbon dioxide as a global warming agent. This would drastically increase temperatures and rush us towards the breach of other tipping points.</p><p>This could include the acceleration of ice thaw on all three of the globe's large, land-based ice sheets – Greenland, West Antarctica and the Wilkes Basin in East Antarctica. The potential collapse of the West Antarctic ice sheet is seen as a key tipping point, as its loss could eventually <a href="https://science.sciencemag.org/content/324/5929/901" target="_blank">raise global sea levels by 3.3 meters</a> with important regional variations.</p><p>More than that, we would be on the irreversible path to full land-ice melt, causing sea levels to rise by up to 30 meters, roughly at the rate of two meters per century, or maybe faster. Just look at the raised beaches around the world, at the last high stand of global sea level, at the end of the Pleistocene period around 120,0000 years ago, to see the evidence of such a warm world, which was just 2°C warmer than the present day.</p>
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The Atlantic Meridional Overturning Circulation has a major effect on the climate. Praetorius (2018)
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