06 January 2016

Soot Sources, a Savvy Study, and the Tibetan Plateau

Science

Airborne soot from fires, burning fossil fuels, and other sources can threaten water supplies in mountainous regions far from the burning source. Now, a new method developed at Pacific Northwest National Laboratory tagged sources of soot from different global regions in a climate model, and tracked where it lands on China's Tibetan Plateau. Researchers determined which areas around the plateau contributed the most soot-and where. The technique also pointed to the most effective way to reduce soot on the plateau to ease the amount of warming the region undergoes.

"Soot on snow in the northwest plateau causes more warming than all other sources in the area. It's bigger than the effect of greenhouse gases and soot in the atmosphere," said corresponding author and PNNL atmospheric scientist Dr. Hailong Wang. "The strong heating caused by soot on snow and in the atmosphere can change air circulation over the Plateau, leading to a broader impact on climate."

Approach

Although earlier work showed soot's warming effect over the whole region, the researchers wanted to pinpoint what kind of sources contribute. The team looked specifically at fossil fuel sources, biofuel and biomass sources of soot. For example, people in the surrounding countries use much wood, grass and agricultural wastes to cook with, which the team categorized as biofuel.

To track soot, the team developed a new way to tag particles emitted from individual sources within the climate model. This was an improvement on the other source-attribution methods that either don't completely isolate contributions from particular sources or they require running the model many times in order to turn the sources off and on one at a time. Running the computer model in this way not only showed which source sent the most soot over, but also can determine which source would make the biggest impact if emissions are cut. The soot destination that changed the most was the northwest Plateau by cuts in central Asia's fossil fuel burning. Cuts in South Asia can effectively reduce the soot level on the entire plateau, especially in the Himalayas.

Impact

Like a dark blanket, the soot acts to warm the ice and snow enough to speed up snowmelt and shrink glaciers. The study confirmed previous work that soot causes net warming over the entire Himalayan-Tibetan Plateau region. The work showed that soot pollution could affect the people living there by altering the seasonal water supply. By pinpointing sources of soot that would make the biggest difference when cut, the study points to areas where cutting pollution could provide a large impact.

"If we really want to address the issue of soot on the Tibetan Plateau," said Dr. Yun Qian, a study co-author and atmospheric scientist at PNNL, "we need to know where we should start."

Contact
Hailong Wang
Pacific Northwest National Laboratory
Publications
Zhang, R., Wang, H., Qian, Y., et al. "Quantifying Sources, Deposition, Transport and Radiative Forcing of Black Carbon Over the Himalayas and Tibetan Plateau." Atmospheric Chemistry and Physics 15, 6205-6223 (2015). [10.5194/acp-15-6205-2015].
Acknowledgments

This research is based on work supported by the U.S. Department of Energy (DOE), Office of Science, Biological and Environmental Research as part of the Earth System Modeling Program. The Pacific Northwest National Laboratory (PNNL) is operated for DOE by Battelle Memorial Institute under contract DE-AC05-76RLO1830. The CESM project is supported by the National Science Foundation and the DOE Office of Science. R. Zhang acknowledges support from the China Scholarship Fund. J. Huang and Q. Fu acknowledge support from the National Basic Research Program of China (2012CB955303), NSFC grant 41275070, and the China 111 project (no. B13045). Computational resources were provided by the National Energy Research Scientific Computing Center (NERSC), a national scientific user facility located at Lawrence Berkeley National Laboratory in Berkeley, California. NERSC is the flagship scientific computing facility for the Office of Science of DOE.