Cloud in a Box: Mixing Aerosols and Turbulence

When it comes to climate change, clouds are the wild card. Atmospheric physicists at Michigan Tech use a turbulence-generating cloud chamber to better understand the details and droplets.

There are few absolutes in life, but Will Cantrell – professor of physics at Michigan Technological University – says this is one: “Every cloud droplet in Earth’s atmosphere formed on a preexisting aerosol particle.”

And the way those droplets form – with scarce or plentiful aerosol particles – could have serious implications for weather and climate change.

It’s been known for decades that cleaner clouds tend to have bigger cloud droplets. But through research conducted in Michigan Tech’s cloud chamber, which was published today by Proceedings of the National Academy of Sciences (DOI:http://www.pnas.org/content/early/2016/11/22/1612686113.full), Cantrell, graduate student Kamal Kant Chandrakar, fellow physics professor Raymond Shaw, and colleagues found that cleaner clouds also have a much wider variability in droplet size. So wide, in fact, that some are large enough to be considered drizzle drops.

Dirtier clouds, Shaw explains, not only have smaller droplets, but also much more uniformity in droplet size, with no observable drizzle drops.

“If clouds have more aerosols in them, the drops would be smaller and more similar in size,” Shaw says. “It would be harder for the cloud to rain, and the cloud would then last longer. If a cloud rains, or has less water in it, it won’t be there to reflect sunlight.”

Aerosols, Candy and Rain

For many people, the word aerosol conjures up images of Aqua Net hairspray or household air fresheners. But an aerosol is simply any solid or liquid that’s suspended in gas or liquid.

When an aerosol particle in Earth’s atmosphere takes up water, it becomes a cloud droplet. On their own, aerosol particles are tiny; when a cloud droplet becomes a rain droplet, it grows by a factor of a million as droplets crash and coalesce together. What Shaw and Cantrell want to better understand is how aerosols affect the size where cloud droplets become heavy enough to fall as rain.

If there was no dust in the air, there would be no fogs, no clouds, no mists, and probably no rain.”John Aitken, meteorologist and physicist (1839-1919)

To figure it out, they went to the cloud chamber and created two kinds of clouds – very polluted clouds and very clean ones. Imagine the available water in these clouds as a piñata full of candy, and all the aerosols are kids. If there are a lot of kids in the room, it’s more likely that most will get a piece of candy; if only 10 percent of the kids are there, then only a few – the fast or lucky ones – will scoop up most of the good stuff. Aerosols compete in the same way for water vapor: more aerosols result in smaller drops with a more even distribution, and fewer aerosols create larger drops with uneven distribution.

But there’s another key element to consider: turbulence. The spraying and bounding candy released from the piñata is like the water vapor in a real cloud that’s continuously mixed and swirled by turbulence. Sometimes the turbulence creates a “spike” of high water vapor. In a polluted cloud, lots of droplets are there to gobble the water vapor up. In a clean cloud, the same spike of high water vapor could last a long time with only a few fortunate droplets in the vapor’s vicinity to munch plentifully and grow much bigger than their neighbors.

“In a heterogeneous spread of droplet sizes, the cloud droplets are more likely to turn into rain droplets, because they’re more likely to collide,” Cantrell explains, adding that different-sized droplets fall at different speeds because of Earth’s atmosphere. “When rain droplets fall, their speed is governed by a balance between gravity pulling them down and drag holding them back. While every raindrop falls at terminal speed, the bigger drops fall faster.”

Cloud White, Cloud Bright

There are many sources of aerosol emission. Anyone who’s been to a megacity knows the orange haze of aerosols that often hangs in the air. Scientists have good reason to expect that those massive emissions of aerosols could change the brightness of clouds and how efficiently clouds rain. The Michigan Tech study reinforces that dirtier clouds – which are brighter clouds that scatter more sunlight, reflecting some of it back to space – will probably last longer because they are less likely to lead to precipitation.

“Clouds are the big wild card,” Shaw says. “We’re looking at clouds as one part of a large climate system. Like all the interlinked parts of the system, clouds tend to respond to changes in the system. But how will they respond? Will they counteract a lot of the carbon dioxide effect or just a little?”

Studying clouds in nature is notoriously difficult. Researchers have to take what they can get on any given day, and nothing is constant. In the cloud chamber, however, Shaw and Cantrell can control what are called thermodynamic and microphysical variables – the temperature, pressure, aerosol quantity and water vapor.

What makes the Michigan Tech cloud chamber different from any other is that the cloud inside is turbulent, and researchers can keep a cloud for as long as they want, so long as they keep feeding it aerosols. In other chambers, clouds are more static and only last for a matter of minutes. The Michigan Tech chamber works differently due to cloud mixing between a hot and cold surface, the same process that forms clouds or fog over a lake on fall days when the water temperature is warmer than the air temperature.