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   https://doi.org/10.21552/edpl/2018/2/7  

   Jasmontaite, L. ; Kamara, I. ; Zanfir-Fortuna, G. ; Leucci, S. ( January 2018 , European Data Protection Law Review)
2. SNP by SNP by environment interaction network of alcoholism

   https://doi.org/10.1186/s12918-017-0403-7  

   Zollanvari, Amin ; Alterovitz, Gil ( March 2017 , BMC Systems Biology)
3. Wave damping by flexible marsh plants influenced by current

   https://doi.org/10.1103/PhysRevFluids.6.100502  

   Zhang, Xiaoxia ; Nepf, Heidi ( October 2021 , Physical Review Fluids)
4. Interpretable by Design: Learning Predictors by Composing Interpretable Queries

   https://doi.org/10.1109/TPAMI.2022.3225162  

   Chattopadhyay, Aditya ; Slocum, Stewart ; Haeffele, Benjamin D. ; Vidal, René ; Geman, Donald ( June 2023 , IEEE Transactions on Pattern Analysis and Machine Intelligence)
5. Shortwave absorption by wildfire smoke dominated by dark brown carbon

   https://doi.org/10.1038/s41561-023-01237-9  

   Chakrabarty, Rajan K. ; Shetty, Nishit J. ; Thind, Arashdeep S. ; Beeler, Payton ; Sumlin, Benjamin J. ; Zhang, Chenchong ; Liu, Pai ; Idrobo, Juan C. ; Adachi, Kouji ; Wagner, Nicholas L. ; et al ( August 2023 , Nature Geoscience)

   Wildfires emit large amounts of black carbon and light-absorbing organic carbon, known as brown carbon, into the atmosphere. These particles perturb Earth’s radiation budget through absorption of incoming shortwave radiation. It is generally thought that brown carbon loses its absorptivity after emission in the atmosphere due to sunlight-driven photochemical bleaching. Consequently, the atmospheric warming effect exerted by brown carbon remains highly variable and poorly represented in climate models compared with that of the relatively nonreactive black carbon. Given that wildfires are predicted to increase globally in the coming decades, it is increasingly important to quantify these radiative impacts. Here we present measurements of ensemble-scale and particle-scale shortwave absorption in smoke plumes from wildfires in the western United States. We find that a type of dark brown carbon contributes three-quarters of the short visible light absorption and half of the long visible light absorption. This strongly absorbing organic aerosol species is water insoluble, resists daytime photobleaching and increases in absorptivity with night-time atmospheric processing. Our findings suggest that parameterizations of brown carbon in climate models need to be revised to improve the estimation of smoke aerosol radiative forcing and associated warming.

    

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