Cooperative Institute for Research in Environmental Sciences at the University of Colorado Boulder

Jose-Luis Jimenez

Research Interests

Aerosols are small particles suspended in air, with lifetimes of 1-2 weeks in the atmosphere. They have ma­jor effects on climate, human health, visibility, crops, and ecosystems. A large portion is composed of organic compounds. Important sources of these organic aerosols (OA) include anthropogenic pollution (cars, trucks, volatile chemical products), bio­genic compounds (plants, soils), and biomass burning (agricultural and wild fires). Gas-phase chemistry followed by gas-to-particle conversion produces secondary OA (SOA) and inorganic species. The amount, properties, and evolu­tion of aerosols from these sources are poorly characterized, and our group combines field, laboratory, modeling, and instrument development research to better understand them.

Current Research

We recently participated in two collaborative aircraft field missions studying the chemistry of the wintertime NE United States (NSF WINTER) and springtime Korean Peninsula (NASA KORUS-AQ). The goals of the studies were to gain better understanding the sources, chemistry, transport, and losses of air pollutants of understudied urban wintertime conditions in the United States, and of an Asian megacity. We focused our research on quantifying the key sources and processes that lead to SOA production and aging.

During the WINTER campaign, we operated a High-Resolution Time-of-Flight Aerosol Mass Spectrometer (AMS) on the NSF/NCAR C-130 aircraft during daytime and nighttime over the NE United States. We showed that the OA fraction of aerosol was half that of summertime studies in that region, but almost as oxidized. OA was roughly half oxygenated (secondary) and half primary (POA). Biomass burning OA (likely from residential heating) was ubiquitous and accounted for one-third of OA. Large discrepancies with current computer models (GEOS-Chem versions) were uncovered that predict too little SOA and too much POA. A case study of urban outflow from New York City showed similar efficiency of SOA formation compared to summer, although slower due to lower oxidant levels in wintertime (Figure 1).

We participated in the KORUS campaign (making AMS measurements) onboard the NASA DC-8 aircraft over the Korean Peninsula. Our analysis showed that the efficiency of SOA production over Seoul was higher than for other megacities. Contrary to some previous speculation about the dominance of aerosol transport from China, we showed that production of SOA from locally-emitted precursors is a major source in the Seoul region. Transport modeling, strong correlations with short-lived secondary photochemical species, chemical box modeling, and results from an in situ oxidation flow reactor (OFR) were all used to discover and support these findings. An OFR was flown for the first time and provided unique constraints on the potential of air masses to form SOA by taking “snapshots” of that chemical potential periodically during flight. It showed that a factor of 4.5 increase in potential SOA over Seoul versus over the Yellow Sea (representative of background air masses advected into Seoul). See Figure 2.

Other ongoing research in our group includes: aircraft-based measurements of aerosol in the remote Atlantic and Pacific Ocean basins; modeling of the radical and SOA-forming chemistry in OFRs; chemically-speciated gas-particle partitioning on a wide range of aerosol seed compositions in the CU Environmental Chamber Facility; development and characterization of AMS and extractive electrospray (EESI) measurements; explicit chemistry modeling comparing chambers, OFRs and the atmosphere; developing improved parameterizations to simulate SOA formed from isoprene and terpenes; exploring the factors controlling SOA production among megacities; measurements of the sources, chemistry, and building interactions of organic compounds as well as cooking emissions in indoor environments; and wildfire and agricultural fire biomass burning emissions and chemical evolution from aircraft.



Figure 1: Aerosol evolution in the New York City plume advected over the ocean. Aerosol concentrations are normalized to carbon dioxide (CO) to account for dilution and plotted vs. photochemical age. Left: Total OA and comparison to summertime studies. Middle: Total primary aerosol (POA) and the components related to fossil-fuel combustion (HOA) and biomass burning (BBOA). Right: Secondary OA and separated into more (MO-OOA) and less (LO-OOA) components. Image: Schroder et al. 2018.

 

Figure 2: Conceptual model representing the transport of background air into Seoul, and the emissions of primary species (CO and HOA) and photochemical production of secondary species (SOA, particle nitrate, Ox (O3+NO2), and formaldehyde (CH2O)) impacting Seoul. Image: Nault et al. 2018.

 

Ben Nault and Jason Schroder operating the AMS onboard the NASA DC8 during the KORUS-AQ mission.

Honors and Awards

  • 2014 Highly Cited Researcher (Thomson Reuters) in both Geosciences and Engineering
  • 2010 Rosenstiel Award of the Rosenstiel Foundation and the Rosenstiel School of Marine and Atmospheric Science at the University of Miami for "outstanding contributions" and a "significant and growing impact in the last decade" in marine and atmospheric science.
  • 2008 Kenneth T. Whitby Award of the American Association for Aerosol Research (AAAR)
  • 2007 Provost Faculty Achievement Award, CU Boulder
  • 2004 NSF Young Investigator "CAREER" Award
  • Two "Fast Breaking Paper" recognitions from Thomson ISI for Ulbrich et al. (ACP 2009) and Jimenez et al. (Science 2009)
  • 73 "Highly Cited Papers" (ISI, Top 1% in their fields) and 2 "Hot Papers" (Top 0.1%)
  • 3 "Top 20 Cited Papers" in Environmental Science and Technology
  • NASA Group Achievement Awards, 2003, 2006, and 2008
  • La Caixa Foundation Doctoral Fellowship, 1994-1996
  • Elected Fellow of the American Geophysical Union (AGU), 2015