Abstract
Biomass burning particulate matter (BBPM) affects regional air quality and global climate, with impacts expected to continue to grow over the coming years. We show that studies of North American fires have a systematic altitude dependence in measured BBPM normalized excess mixing ratio (NEMR; ΔPM/ΔCO), with airborne and high-altitude studies showing a factor of 2 higher NEMR than ground-based measurements. We report direct airborne measurements of BBPM volatility that partially explain the difference in the BBPM NEMR observed across platforms. We find that when heated to 40-45 °C in an airborne thermal denuder, 19% of lofted smoke PM1 evaporates. Thermal denuder measurements are consistent with evaporation observed when a single smoke plume was sampled across a range of temperatures as the plume descended from 4 to 2 km altitude. We also demonstrate that chemical aging of smoke and differences in PM emission factors can not fully explain the platform-dependent differences. When the measured PM volatility is applied to output from the High Resolution Rapid Refresh Smoke regional model, we predict a lower PM NEMR at the surface compared to the lofted smoke measured by aircraft. These results emphasize the significant role that gas-particle partitioning plays in determining the air quality impacts of wildfire smoke.
| Original language | English |
|---|---|
| Pages (from-to) | 17011-17021 |
| Number of pages | 11 |
| Journal | Environmental Science and Technology |
| Volume | 57 |
| Issue number | 44 |
| DOIs | |
| State | Published - Nov 7 2023 |
Funding
We thank the crews, pilots, and support staff from all the field campaigns included for making these measurements possible. The CU HR-AMS team was funded by NASA grants 80NSSC18K0630, 80NSSC19K0124, and 80NSSC21K1451. Work by DP at Weber State University was funded by NASA grant 80NSSC21K1451. VS and RY were supported by the NSF grant AGS-1748266 and NOAA-CPO grant NA16OAR4310100. The WE-CAN measurements herein were supported by the NOAA OAR Climate Program Office Award No. NA17OAR4310010. The Fuel2Fire team (AJS, EMG, and EBW) were supported by NASA grants 80NSSC18K0685 and 80NSSC21K1456. We acknowledge the work of many additional scientists for the generation and analysis of the data used in this work. This includes, but is not limited to, Eben Cross, Conner Daube, Christoph Dyroff, Delphine Farmer, Andy Freedman, Alan Fried, Lauren Garofalo, Hannah Halliday, Anne Handschy, Thomas Hanisco, Jordan Krechmer, Matson Pothier, J. Rob Roscioli, Joshua Schwarz, and Glenn Wolfe.
| Funders | Funder number |
|---|---|
| 80NSSC21K1456, NA17OAR4310010, 80NSSC18K0685 | |
| NA16OAR4310100 | |
| AGS-1748266 | |
| National Aeronautics and Space Administration | 80NSSC18K0630, 80NSSC19K0124, 80NSSC21K1451 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
-
SDG 13 Climate Action
Keywords
- Biomass burning organic aerosol volatility
- volatility basis set
Fingerprint
Dive into the research topics of 'Impact of Biomass Burning Organic Aerosol Volatility on Smoke Concentrations Downwind of Fires'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver