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Effects of Biomass Burning on Stratocumulus Droplet Characteristics, Drizzle Rate, and Composition. | LitMetric

AI Article Synopsis

  • The study investigates how biomass burning (BB) plumes affect cloud properties, based on airborne measurements conducted off the California coast during five campaigns, two of which were impacted by wildfires.
  • The findings show that subcloud aerosol concentrations, such as cloud condensation nuclei, were more closely related to cloud droplet numbers than those measured above the clouds, suggesting that BB particles were primarily sourced from the free troposphere.
  • It was also found that BB-affected clouds had lower activation fractions of cloud condensation nuclei due to less hygroscopic aerosols, and the composition of cloud water and droplet residual particles varied depending on the age of the BB plume and dust presence.

Article Abstract

This study reports on airborne measurements of stratocumulus cloud properties under varying degrees of influence from biomass burning (BB) plumes off the California coast. Data are reported from five total airborne campaigns based in Marina, California, with two of them including influence from wildfires in different areas along the coast of the western United States. The results indicate that subcloud cloud condensation nuclei number concentration and mass concentrations of important aerosol species (organics, sulfate, nitrate) were better correlated with cloud droplet number concentration ( ) as compared to respective above-cloud aerosol data. Given that the majority of BB particles resided above cloud tops, this is an important consideration for future work in the region as the data indicate that the subcloud BB particles likely were entrained from the free troposphere. Lower cloud condensation nuclei activation fractions were observed for BB-impacted clouds as compared to non-BB clouds due, at least partly, to less hygroscopic aerosols. Relationships between and either droplet effective radius or drizzle rate are preserved regardless of BB influence, indicative of how parameterizations can exhibit consistent skill for varying degrees of BB influence as long as is known. Lastly, the composition of both droplet residual particles and cloud water changed significantly when clouds were impacted by BB plumes, with differences observed for different fire sources stemming largely from effects of plume aging time and dust influence.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7709909PMC
http://dx.doi.org/10.1029/2019JD031159DOI Listing

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