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Atmospheric Sciences & Global Change
Research Highlights

May 2015

From Fire to Ice

Volcanic ash proves inefficient cloud ice maker

volcano eruption
Tons of volcanic ash entered the atmosphere in 2010 when the Icelandic volcano erupted. Researchers want to understand the ash particle properties and how well these particles can provide a nucleus for cloud ice crystals. zoom Enlarge Image.

Results: When tons of ash spewed into the atmosphere from a 2010 Icelandic volcano it caused havoc for vacationers across Europe. But did it also dramatically change clouds? Researchers at Pacific Northwest National Laboratory found that volcanic ash is not as efficient as common dust in birthing clouds' ice particles. Using a novel laboratory testing chamber they formed cloud ice, a process called ice nucleation, around particles of dust and volcanic ash. Their results revealed the importance of optimal particle structure to efficiently attract super cold water vapor to nucleate ice.

"We described the detailed particle properties of ash, not currently included in atmospheric models," said Dr. Gourihar Kulkarni, atmospheric scientist at PNNL and lead author of the study. "By including the missing information, we can increase model confidence in simulating the deposition mode of ice nucleation."

Why It Matters: Volcanic eruptions occur almost every day somewhere around the globe. These eruptions provide a constant source of fine ash injected into the part of the atmosphere where clouds are born. These particles can alter clouds but the process is not yet well understood. Researchers at PNNL are using novel techniques to simulate how ash particles compete with already existing natural particles such as dust to birth cloud ice. Because more than half the Earth's precipitation comes from cloud ice particles, scientists are working to understand all the ways ice crystals are formed during ice nucleation. Including these fundamental discoveries about cloud formation in climate and weather forecast models will support new insight for precipitation and prediction of climate change.

Methods: PNNL scientists and a collaborator from the Qatar Environment and Energy Research Institute investigated the ice nucleating properties of ash particles from the 2010 Iceland volcanic eruption at Eyjafjallajökull (see sidebar, Cloud Ice Birthing, and the Icelandic Volcano with the Hard-to-Say Name). They used the ice nucleation chamber at PNNL's Atmospheric Measurement Laboratory (AML) to test and compare how ash and dust particles nucleate ice in a super cold atmosphere.

At the same time, they applied bulk and single-particle techniques to analyze the surface elemental composition, morphology structural, and shape factor properties of volcanic ash particles at the U.S. Department of Energy's Environmental Molecular Sciences Laboratory (EMSL) user facility. Researchers also examined the relative importance of ice nucleation behavior of these particles to proxy natural dust particles. These techniques provide detailed information at a molecular level to compare and understand the ice formation ability of ash and dust particles.

What's Next? Detailed quantification of structural properties is necessary to develop the simplified equations, called parameterizations, used to describe heterogeneous (water to non-water particle) ice nucleation in climate models. Determining ice nucleation efficiencies of volcanic ash particles from different eruption periods will further explain the impact of volcanic particles on clouds. Understanding cloud condensation nucleation properties of these volcanic particles will advance the long-term goal to provide a fundamental theory basis representing the ice nucleation process in climate models.

Acknowledgments

Sponsor: The research was funded by the U.S. Department of Energy Office of Science, Biological and Environmental Research (BER) as part of the Atmospheric System Research Program. Additional support was provided by the PNNL Laboratory Directed Research and Development program for the Chemical Imaging Initiative.

Research Team: Gourihar Kulkarni, Manjula Nandasiri, Alla Zelenyuk, Josef Beránek, Nitesh Madaan, Arun Devaraj, Vaithiyalingam Shutthanandan, and Tamas Varga,  PNNL; Suntharampillai Thevuthasan, Qatar Environment and Energy Research Institute, Doha.

Research Area: Climate & Earth Systems Science

Facilities: Atmospheric Measurement Laboratory and EMSL, a DOE Office of Science User Facility sponsored by BER and located at PNNL

Reference: Kulkarni G, M Nandasiri, A Zelenyuk, J Beranek, N Madaan, A Devaraj, V Shutthanandan, S Thevuthasan, and T Varga. 2015. "Effects of Crystallographic Properties on the Ice Nucleation Properties of Volcanic Ash Particles." Geophysical Research Letters 42. DOI: 10.1002/2015GL063270.

Related highlights: Dust Takes Detour on Ice-Cloud Journey
Nailing Down Ice in a Cloud Model
When Nudge Comes to Shove
Dust Achieves Lofty Aspirations
Ice Heating Up Cold Clouds


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Cloud Ice Birthing, and the Icelandic Volcano with the Hard-to-Say Name

In April 2010, the Eyjafjallajökull volcano in Iceland blew its top. Air travel over Europe was halted for almost 10 days, and some areas suffered further delays. While a major concern for aircraft engines, ash is also of interest to scientists who study cloud formation and precipitation. Ice is surprisingly difficult to create in the atmosphere. At supercooled temperatures (to -37°C), water vapor can exist unfrozen until it "collides" with a heterogeneous (non-water) particle, such as dust, soot, organic material, and ash. A large area of scientific uncertainty remains about these non-water particles, their frequency and their abilities to efficiently prompt ice crystals. These questions are important to answer because more than half the Earth's precipitation originates as ice in clouds.

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