If you are browsing the subtropical ocean and look up, it is likely that you are lumpy, gray, and occasionally stratocumulus when you are freezing the clouds.
Large cloud clouds are those that call cloud bridges, help them shut off the sun's rays and increase the planet's reach, or the ability to reflect solar energy and radiation in space.
But if the planet continues to heat up, these clouds will not be too long.
As a new study simulates emissions of carbon dioxide emissions into "atmospheric business" that emit atmospheric emissions, the clouds of terrestrial stratocytes would disappear in the next 100 and 150 years.
When the clouds fade, the simulations show that the Earth's temperature rises to 8 degrees (14 degrees).
This could have made the planet "grow" a climate that was 56 million years old in the world, when the oceans grew and lifted, the animals fled to the North Pole and stormed the storms when the weather was warmed up.
The absence of these clouds could be a 20-degree Fahrenheit global temperature increase, and on the ground "Garden" creating a climate
Stratocumulus clouds are distinguished between its members; The cloudiness lasts over the fresh air at the top and creates a sweaty sweat in a colder atmosphere.
But if the level of carbon dioxide rises if it reaches more heat in the surrounding atmosphere, the strata can not keep clouds, Tapio Schneider, a senior scientist and research scientist at the California Institute of Technology at the California Institute of Technology, said Business Insider. For this reason, cloud protocols could be introduced into smaller clouds, when they do not reflect shade or sunlight.
Using a supercomputer, Schneider's team would measure how different atmospheric carbon concentrations were measured in the survival of the stratocellular clouds. Simulation 1,200 ppm (currently three times the atmospheric carbon dioxide three times), these critical clouds have disappeared.
Even if it is not possible to reach around 1,200 ppm, it is the level of greenhouse gas emissions that can be "slow in the machining". After reaching the tipping point, the clouds have gone well until the carbon dioxide emissions are reduced.
In the end, the planet's risk of 12-degree Cycle (20-degree Fahrenheit) is compromised in the next 150 years. If the Stratocumulus cloud gets this punctuality, it shows Schneider's simulations.
Schneider said that cloud bridges would return to lower carbon dioxide levels by lowering their point of descent. But he added that if it happened, there would not be much to reverse the effects of heat melting on melting ice sheets and sea levels.
Once the clouds come out, the simulated climate goes "over a cliff", said one of the climate science scientists at Kerry Emanuel Massachusetts Institute.
The simulations can solve a mystery of 56 million years
Schneider thinks it's a mystery of a long-time investigator that could spark light on those clouds. Almost 56 million years ago, Earth had a "climate of temperature", where the 11-degree stream was over 20,000 Fahrenheit over 20,000 years ago. At that time, the oceans reached levels of 100 degrees Fahrenheit and melted Arctic.
Climate models should demonstrate the level of carbon dioxide in the atmosphere so that biologists can test their geological record twice.
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Maybe the clouds were missing the puzzle.
When the carbon dioxide level occurred, the stratocits disappeared and the absence of clouds was helped by the additional heating. This means that models and evidence do not match.
"This was a question about climate models," said Schneider. "But that could slow down how hot the climate was."