New research uncovers secrets of snowflakes movement - study

Amazingly, every tiny snowflake that falls to the ground is unique, like human fingerprints. University of Utah atmospheric sciences Prof. Tim Garrett has devoted his scientific career to characterizing snowflakes, the multifaceted particles of ice that form in clouds and dramatically drop to Earth.

Now, he is unlocking the mystery of how snowflakes move in response to air turbulence that accompanies snowfall using novel instrumentation developed on campus. After analyzing more than half a million snowflakes, what his team has discovered has left him astonished. Instead of something that is incredibly complicated, he and his team found that predicting how snowflakes move proved to be surprisingly simple. 

“How snowflakes fall has attracted a lot of interest for many decades because it’s a critical parameter for predicting weather and climate change,” Garrett said. “This is related to the speed of the water cycle. How fast moisture falls out of the sky determines the lifetime of storms.”

The famed Japanese physicist Ukichiro Nakaya termed snow crystals as “letters sent from heaven” because their delicate structures carry information about temperature and humidity fluctuations in the clouds where crystal basal and prism facets competed for water vapor deposition.

While every snowflake is believed to be completely unique, how these frosty particles fall through the air as the accelerate, drift, and swirl follows patterns, according to new research by Garrett and colleagues Dhiraj Singh and Eric Pardyjak of the university’s mechanical engineering department. They published their findings in the journal Physics of Fluids under the title “A universal scaling law for Lagrangian snowflake accelerations in atmospheric turbulence.” 

important implications for weather forecasting

Snowflake movement has important implications for weather forecasting and climate change, even in the tropics. “Most precipitation starts as snow. How fast it falls affects predictions of where on the ground precipitation lands, and how long clouds last to reflect radiation to outer space,” Garrett explained. “It can even affect forecasts of a hurricane trajectory.”

The team developed instrumentation called the Differential Emissivity Imaging Disdrometer (DEID) that measures snowflakes’ hydrometeor mass, size, and density. This device has since been commercialized by a company Garrett co-founded called Particle Flux Analytics. Utah’s transportation department has already deployed the equipment in Little Cottonwood Canyon – the famed ski destination and that state’s snowiest place – for the winter of 2020-2 to help with avalanche forecasting, The instrumentation was deployed alongside measurements of air temperature, relative humidity and turbulence, and placed directly beneath a particle tracking system consisting of a laser light sheet and a single-lens reflex camera.

“By measuring the turbulence, the mass, density and size of the snowflakes and watching how they meander in the turbulence,” Garrett said, “we are able to create a comprehensive picture that hadn’t been able to be obtained before in a natural environment before.”

The findings were not what the team expected. Despite the intricate shapes of snowflakes and the uneven movement of the air they encounter, they found they could predict how snowflakes would accelerate based on a parameter known as the Stokes number that reflects how quickly the particles respond to changes in the surrounding air movements.

When they analyzed the acceleration of individual snowflakes, the average increased in a nearly linear fashion with the Stokes number, and the distribution of these accelerations could be described by a single exponential curve independent of that number.

The researchers found that the same mathematical pattern could be connected to how changing snowflake shapes and sizes affect how fast they fall, suggesting a fundamental connection between the way the air moves and how snowflakes change as they fall from the clouds to the ground.

“That, to me, almost seems mystical,” Garrett concluded. “There is something deeper going on in the atmosphere that leads to mathematical simplicity rather than the extraordinary complexity we would expect from looking at complicated snowflake structures swirling chaotically in turbulent air. We just have to look at it the right way and our new instruments enable us to see that.”