From Discover Magazine:
The plane pitches violently as it plows through the milky innards of a cloud bank. A commercial pilot would fly high above these clouds over California’s Sierra Nevada Range, but this 63-foot Gulfstream-1 seems to invite the turbulence. Updrafts grab hold of the aircraft and shove it up even as the pilot noses it down. In the back of the plane, atmospheric chemist Kimberly Prather wears headphones to muffle the roar of the propellers. She steadies herself with a hand on an instrument rack and focuses on the bobbing screen of her laptop. Readings from the clouds spool across it.
Those numbers tell Prather that these winter clouds are cold and heavy, –30 degrees Fahrenheit and just over 100 percent relative humidity. Yet despite being 62 degrees below the freezing point of water, the cloud droplets remain stubbornly liquid. As long as they don’t form ice crystals, these clouds won’t shed more than a few flakes of snow over the Sierras’ 13,000-foot peaks. They are typical clouds, teasers that won’t drop much of anything.
After two hours of flying, though, something changes. The voice of another researcher crackles over Prather’s headset: “Ice!” The plane has entered a cloud layer where suddenly every droplet is frozen. Prather’s instrument—a tangle of metal tubes, wires, and airtight chambers nicknamed Shirley—tick-tick-ticks as its laser blasts apart hundreds of microscopic cloud particles, one by one, that are drawn in from the air outside. The size and composition of each particle flash across Prather’s monitor. The specks at the heart of those ice crystals are high in aluminum, iron, silicon, and titanium, the chemical signatures of dust not from California but from faraway deserts in Asia or even Africa. There’s something else in the crystals too: carbon, nitrogen, and phosphorus, telltale signs of biological cells.
The skies are full of invisible life. Bacteria, algae, and fungi are swept up by winds and lifted to the altitude of a Boeing 747—or catapulted 20 miles into the stratosphere by electric fields during thunderstorms. Prather, a 49-year-old professor at the University of California, San Diego, is one of a growing number of scientists who suspect this largely unexplored microbial ecosystem might hold the answer to one of the great mysteries of the weather: Why do clouds produce precipitation when they do?
It seems like such a basic question, but “we really don’t understand why some clouds drop rain and others don’t,” Prather says. At the heart of this mystery is the physics of ice formation. A pure cloud droplet can cool to –40ºF before it freezes, and many clouds on Earth never get anywhere near this cold. Rain and snow often require tiny particles floating in the cloud to trigger ice to form, and not just any particle will do. A cubic yard of air contains hundreds of thousands of microscopic specks, but only about one in a million possesses the exact molecular geometry that will organize water molecules on its surface to spawn an ice crystal. Without those rare ice-forming triggers, much of the planet would see less precipitation than it does today.
Soot and dust were long considered the best candidates for these one-in-a-million particles. But the discovery that certain bacteria carry a gene that allows them to form ice, along with the realization that the skies are teeming with microbial life, has made some researchers look to airborne biology for answers. “The amount of different types of microbial life present in the cloud droplets that make up a winter storm is amazing,” says Gary Franc, a microbiologist and plant pathologist at the University of Wyoming in Laramie. “There’s a whole ecosystem going on in the clouds that’s largely undefined.”
Scientists like Franc are only now starting to catalog what could be thousands of species of microbes drifting in the sky, many of them almost certainly new to science, and some perhaps capable of surviving high in the stratosphere, where conditions are roughly as favorable for life as they are on Mars. Prather’s studies suggest that dust from Asia and Africa might carry ice-forming microbes all around the globe.
All told, up to 2 million tons of bacteria may find their way into the atmosphere each year, not to mention 55 million tons of fungal spores and unknown quantities of algae. They have been overlooked for decades, but scientists are finally recognizing how diverse this atmospheric ecosystem is and—perhaps—how much influence it could exert over tomorrow’s weather or next year’s harvest.
Clouds feel utterly familiar to us. We idealize them as tufts of cotton drifting overhead, curse them for ruining a picnic, or just take them for granted. But clouds possess inner lives, marked by complex, second-by-second ebbs and flows.
A cloud over a mountain may look stationary, but it more closely resembles a standing wave in a river—an atmospheric river. As moist air rises over a range like the Sierras, falling temperatures cause water vapor to condense into droplets, giving rise to clouds. New droplets form in the cloud every second. But any given droplet lives for only an hour before the current sweeps it down the far side of the mountains, causing it to rewarm, evaporate, and vanish. Only an ice crystal can grow quickly enough to hit critical mass and fall during that short time. Ice doesn’t form easily, though.
Although water in an ice-cube tray will turn solid around 32ºF, pure liquid water in clean air never freezes at that temperature. The formation of ice in the air depends on water molecules latching together in a very specific hexagonal pattern that resembles three-dimensional chicken wire. Once enough water molecules organize into that pattern, an ice crystal grows rapidly. The droplet freezes in an instant. But getting that hexagonal-patterned ice embryo to form in the first place is difficult. At just below 32 degrees, more than 100,000 water molecules need to latch together before the crystal becomes stable enough to grow on its own. Since water molecules are constantly dancing around with thermal energy, the likelihood of enough water molecules happening by chance to strike this collective pose is exceedingly low, even at much colder temperatures.
Some particles facilitate the process, however, through a process called nucleation. A little mineral crystal can act as a template, coaxing water molecules on its surface to organize into the hexagonal lattice of an ice crystal. There is plenty of microscopic junk that allows the water in a puddle in your backyard (or even in your ice-cube tray) to freeze just below 32 degrees. But a cloud droplet that is just slightly wider than a red blood cell may contain only one such particle. In order for this particle to nucleate ice crystals, it needs to have just the right shape and give off minute attractive and repulsive atomic forces in just the right places so that the H’s and O’s in those H2O molecules stick to the particle in the right hexagonal pattern.
Clouds at –30 or –35ºF are often entirely liquid because they do not contain any efficient ice-nucleating particles. And yet scientists also see clouds that are much warmer, even 10ºF, that are full of ice and gushing out rain or snow. These clouds obviously contain something that efficiently nucleates ice at those much warmer temperatures.
For decades scientists could not put their finger on what that mystery particle was. In the mid-1960s Gabor Vali, a Hungarian-born Ph.D. student in physics at McGill University in Montreal, devoted most of his waking hours to looking for it. Vali spent months collecting snow and rainwater by the gallon. He brought it to the lab and squeezed it by syringe, drop by drop, onto sheets of aluminum foil, 100 drops per sheet. He cooled the sheets by 2ºF per minute, taking a photo every 30 seconds. Later he projected the photos on a wall and looked to see the temperature at which each drop had frozen.
Vali did 10 experiments a day, five or six days a week, for several years—“many hundreds of thousands of drops,” he says. Each drop froze at a different temperature depending on what specks were floating inside it. A few drops froze at 23ºF, but not frequently enough to explain how efficiently ice crystals form in warm clouds. Vali was missing something.
Then one day on a whim, he grabbed some muddy snow from under his kids’ swing set. It was sloppy science: Researchers around the world were already testing powdered minerals for their ability to form ice, but they used minerals that were sterile and pure. Vali’s quick and dirty experiment produced an unexpected result.
Water drops from the dirty snow froze at 23 degrees much more often than his cleaner samples had. When Vali added rotting leaves to the mix, some drops formed ice at 28 degrees, the highest temperature he had ever seen. The leaves’ potency increased as they turned brown, suggesting that something growing on them was causing ice formation. By this time Vali had finished his degree and moved to the University of Wyoming. There, in 1972, a graduate student named Richard Fresh managed to identify Pseudomonas syringae, a bacterium from the rotting leaves that was triggering the ice.
The discovery had big implications for agriculture. Billions of dollars of crops worldwide are damaged by frost each year. Steven Lindow, a Ph.D. student at the University of Wisconsin who independently discovered P. syringae’s ice-nucleating capability around the same time Vali and Fresh did, found that frost damage is not caused by temperature alone; syringae bacteria on leaves actually use ice crystals as crowbars to rip open plant cells and grab their nutrients. To prevent this, some growers of fruit trees and vegetables now routinely apply bactericides to crops before frosts.
During the 1980s Lindow managed further to isolate the gene that allows syringae to form ice. That gene codes for proteins that spread out on the bacteria’s surface in just the right arrangement to pull water molecules into their hexagonal crystal formation. Since then, four other bacteria have been found that nucleate ice at extremely warm temperatures. Although they are not all related, they share the same gene for ice nucleation.
Even as the importance of biological ice nucleation was being recognized by agricultural scientists, it still wasn’t embraced by atmospheric scientists, who stuck by the traditional view that soot, or sea salt, or some as-yet-unidentified mineral in dust was seeding ice in clouds. There was no real sense at the time of the number and diversity of microbes living in the atmosphere. Vali tried to collect ice-forming cells from the lowest few hundred feet of the atmosphere but failed to find anything. And no one was systematically looking thousands of feet up, where clouds actually form. People doubted that enough cells could get high in the atmosphere to make rain or snow.
“The field collapsed,” says David Sands, a bacteriologist now at Montana State University in Bozeman, who began working with syringae in the 1960s. “The people who were in it couldn’t get grants anymore.” Vali shifted his focus back to cloud physics. Sands continued to study syringae but concentrated on crop diseases, where he could still get funding. The idea that a microscopic, floating biomass was influencing the world’s weather was just too weird for most atmospheric scientists.
In 2005 Sands decided the time was ripe to reopen the investigation and find out whether bacteria really do manipulate the weather. Genetic techniques had advanced considerably in the last two decades, so that it was possible to identify even a few ice nucleators like syringae out of thousands of microbes that might inhabit a cloud. Sands contacted Brent Christner, a postdoc at Montana State who had cut his teeth searching for traces of life in 100,000-year-old Antarctic ice, and invited him to expand his search for life into the clouds.
Christner, now at Louisiana State University, started with a simple experiment. He collected snow from mountains around the world and repeated Vali’s frozen-drop experiment to look for invisible particles that spawned ice. Once Christner found the drops of water that froze above 20ºF, he treated them with an enzyme that kills bacteria but leaves other particles alone. When he cooled those droplets back down, up to 85 percent of them no longer froze (pdf).
It was indirect but tantalizing evidence that bacteria were helping the water freeze. But it left an open question: Were airborne microbes forming ice in the clouds, or were they merely getting mopped up by snowflakes as they fell to Earth? The only way to find out was to fly into a cloud to see what was happening from moment to moment.
Prather unwittingly answered the question in late 2007, soon after Christner finished his experiment but before he published it. Prather had spent 15 years developing a device that could suck in microscopic particles from the air and analyze their chemical composition in a few thousandths of a second. She intended the device to study air pollution. But that year she teamed up with Paul DeMott, a cloud physicist from Colorado State University, to see if they could use the machine to identify the particles that form ice in clouds.
Prather and DeMott made a dozen flights through clouds as high as 25,000 feet over the mountains of Wyoming, Colorado, and Montana. The results caught the researchers off guard. They saw the expected soot, sea salt, and plenty of local dust inside the liquid droplets, but those things rarely had ice associated with them. No, the icy patches in clouds contained something else: 50 percent of the particles were high-titanium dust from the deserts of Asia or possibly Africa, and another 30 percent seemed to be biological based on their carbon, nitrogen, and phosphorus content.
Until then, no one had seen life in a rain cloud. “We were not going in purposely looking for bacteria,” she says. But she has since seen similar results in two more cloud-sampling campaigns. The Sierra flights in early 2011 found that most ice crystals contained dust from deserts on other continents, along with what seemed to be bacteria. When Prather and DeMott sampled clouds over the Caribbean island of Saint Croix in July 2011, they again saw signatures of both dust and cells in the ice. The dust itself seemed to come from North Africa.
DeMott amassed a library of 100,000 ice-forming particles collected from these flights. He has only begun to identify them, but in electron microscope images he finds that some of them resemble bacteria. Franc plans to start testing them soon, looking for the DNA sequences involved in ice nucleation.
Despite these results, some researchers remain skeptical that microbes could be important for cloud formation. Corinna Hoose, a cloud physicist at the Karlsruhe Institute of Technology in Germany, thinks that the number of ice-forming cells that Christner found in snow is too low to make much difference. She estimates that airborne microbes contribute less than 1 percent of all cloud ice. “Dust and soot particles are much more abundant,” she says. “They are much more important than biological particles.”
That has been the dominant view for decades, and dominant views do not die easily. But Prather, Christner, and Sands are chipping away at it. Lab studies have yet to turn up a common mineral that triggers freezing as effectively as bacteria like syringae do. “These organisms,” Christner says, “are able to catalyze ice formation at a temperature warmer than any other naturally occurring particle.”
And Prather may actually have underestimated the abundance of ice-forming biological particles in her samples. Even though she saw lots of dust in the icy patches of clouds, 60 percent of those dust grains also contained carbon, nitrogen, and phosphorus, suggesting that they are not just minerals. They might have cells lurking inside them—or at least the guts of dead cells splattered on their surfaces. It’s an issue that Prather chats about with her colleagues plenty these days. “I don’t think it’s the dust itself” that’s forming ice, she now says. “I think it’s the bio.”
While Prather and others explore the environmental impact of airborne bacteria, Christner is trying to understand this mysterious high-altitude ecosystem as a whole. Working not far from his base at LSU, he is setting out to learn how much is alive in the sky and how far up it lives.
On a cold autumn morning, Christner guides his pickup down a two-lane highway in central Louisiana, speeding past pine thickets, swamps, and dirt roads that don’t show up on his truck’s navigation system. “I’m not sure where the hell we’re going,” he admits.
Christner’s movements are at the mercy of the shifting winds thousands of feet overhead. He and five other vehicles are following a weather balloon that was launched several minutes ago. “It’s at 5,000 feet and still ascending—we’re about two miles ahead of it on the road,” says a voice over the radio.
The balloon’s 12-pound payload, including a GPS transponder, is held together with flimsy string and Styrofoam—designed, per FAA regulations, to disintegrate if it encounters the turbines of a passenger plane. Between 10,000 and 30,000 feet, a door will spring open. The device will collect drifting cells in a coat of gooey grease, just as the front grill of Christner’s truck is collecting insects. At 35,000 feet the germ catcher will cut its string, drift down on a parachute, and hopefully land where it can be found.
The device has previously come to rest in swamps and rice paddies and tangled itself 60 feet up in a longleaf pine. Today the scientists find it in a dense forest, seven-tenths of a mile past a locked gate adorned by two deer skulls with metal stakes driven through their foreheads.
Christner’s Ph.D. student Noelle Bryan will grow the bacteria the balloon collects in order to identify them. Later she’ll look to see if they carry the gene for ice nucleation. “My guess,” Christner says, “is there are probably a whole slew of organisms out there that have this capability that we simply haven’t identified.”
Conditions in the stratosphere resemble those on the surface of Mars. Levels of damaging ultraviolet radiation are 1,000 times as high as those at sea level, threatening to chisel a cell’s DNA into haiku-length snippets. And the atmospheric pressure is only half a percent of what it is at sea level, threatening to shrivel cells into freeze-dried corpses. Christner sees his studies in the stratosphere as a test run for looking for life in other worlds. “What we are doing,” he says, “is not so different from what will happen in the future when we send missions to Mars to take samples to bring them back to Earth.”
Analyzing what, if anything, Christner’s team collected on that 122,000-foot flight will take months. But they have promising results from earlier launches to lower levels of the atmosphere.
Back at their lab Christner and Bryan examine two dozen petri dishes containing bacteria collected from flights that peaked between 10,000 and 80,000 feet. They have yet to sequence and ID the microbes’ DNA, but just looking at the petri dishes gives them some clues. Bright-colored colonies dot many of the dishes—reds, oranges, pinks, and yellows. “Those are natural sunscreens,” Christner says. Colored carotenoid pigments (similar to those in many plants, including the carrots that the compounds are named after) can neutralize damaging ultraviolet light.
Christner holds up a petri dish containing colonies mottled with beige, black, and white: an indication that these bacteria produce dehydration-resistant spores that could help them survive at extreme altitudes. They are probably some sort of Actinomyces (a group of bacteria that live in soils and include species that make streptomycin and other antibiotics), but the species could be new to science. “We don’t know,” Christner says, looking at a splotch. “That might make an antibiotic that nobody’s ever seen before.”
Searching the skies for high-living microbes may also lead to insights concerning some species that we already do know about. In the 1950s researchers funded by the U.S. military tried to sterilize canned meat by blasting it with radiation. When they opened the cans, they were surprised to find the meat rotten: It had been fermented by a bacterium, now called Deinococcus radiodurans, that is exceptionally resistant to radiation. The species carries a muscular set of enzymes that stitch its DNA strands back together as quickly as radiation splinters them apart. Deinococcus can survive 5,000 times as much radiation as human cells, but no natural environment on Earth comes close to those levels of irradiation. “So what the hell has an organism like this evolved tolerance for?” Christner asks.
John Battista, who studies the microbe at LSU, just upstairs from Christner, thinks Deinococcus’s DNA repair enzymes primarily help it survive dehydration in its native desert environment. But radiation tolerance could also allow the bacterium to join that 10-mile-high ecosystem. Windstorms in places like the Gobi Desert could easily pick up Deinococcus and propel it around the world. “If it managed to get into the upper atmosphere,” Battista says, “it has all the tools it needs to survive.” Deinococcus and other similarly hardy microbes may be lurking in the samples Christner’s team is culturing.
Just as the same genes that allow Deinococcus to thrive on the ground may give it the ability to survive at high altitudes, the ice-nucleation gene may originally have given syringae and bacteria like it an advantage other than rainmaking. The nucleation gene appears to be unrelated to any of the more than a million genes that have been sequenced to date from various organisms. And the gene seems to have arisen only once in the course of evolution; after that, it passed from one species to another, changing little along the way. No one knows how long ago the gene emerged, but its appearance may have marked a pivotal moment in Earth’s history. It may have provided a new way for life to modify the planet’s environment.
Ice nucleation might have emerged as an ecological handshake between bacteria and the plants they lived on. Many wild plants (unlike most cultivated crops) are frost tolerant. They can survive as long as the freezing happens slowly, giving the plants time to activate their defenses. By causing frost to set in at higher temperatures—at 25ºF, say, rather than 15—ice-nucleating bacteria would have caused freezing to happen more slowly, helping protect the plants they lived on.
Later on, the talent for forming ice may have found other uses. Syringae uses ice crystals to rip open the cells of plants that are not frost tolerant, so it can devour their nutrients. Microbes like syringae may also exploit ice nucleation to parachute down in raindrops or snowflakes, ensuring they do not remain stuck at high altitudes when swept up by storms.
Ice-nucleating bacteria might even influence the entire landscape. By triggering rain, Sands says, “they cause more plants.” Just as humans farm wheat, syringae might cultivate leafy ecosystems that can sustain the bacteria once they reach the ground. Those ecosystems would then spawn more bacteria, some of which would return to the sky.
The realization that bacteria could have such profound impacts adds one more twist to the already convoluted connection between human activity, weather, and climate. Forests may make their own local rain by releasing bacteria and other organic compounds into the lower atmosphere. Deserts may trigger precipitation thousands of miles away when their dust and bacteria collide with water-rich masses of air. What effect, then, of deforestation or desertification?
Researchers have studied desert dust for decades, tracking its serpentine trajectory around the globe and trying to understand its environmental impact. Now it seems that dust might have been a decoy, hiding the bacteria that could be the real directors of much of our planet’s weather. “When I look at what physically forms the ice in clouds, I’d say 80 percent of it has some sort of biological signature,” Prather says. “The dust by itself doesn’t explain it.”
Source: The Clouds Are Alive (April 2012)
Douglas Fox is a freelance science writer based in California. His work has appeared in The Best American Science and Nature Writing.
