This study reports on heterogeneous ice nucleation activity of predominantly organic or coated with organic material anthropogenic particles sampled within and around the polluted environment of Mexico City. The onset of heterogeneous ice nucleation was observed as a function of particle temperature (Tp), relative humidity (RH), nucleation mode, and chemical composition of particles influenced by their photochemical atmospheric aging. Particle analyses was conducted using computer controlled scanning electron microscopy with energy dispersive analysis of X-rays (CCSEM/EDX) and scanning transmission X-ray microscopy with near edge X-ray absorption fine structure spectroscopy (STXM/NEXAFS). In contrast to the majority of laboratory studies employing proxies of organic aerosol, we show that anthropogenic organic particles collected in Mexico City have can potentially induce ice nucleation at experimental conditions relevant to cirrus formation. The reported results suggest a new paradigm for the potential impact of organic particles on ice cloud formation and climate.
Revised: October 7, 2010 |
Published: June 5, 2010
Citation
Knopf D.A., B. Wang, A. Laskin, R.C. Moffet, and M.K. Gilles. 2010.Heterogeneous Nucleation of Ice on Anthropogenic Organic Particles Collected in Mexico City.Geophysical Research Letters 37, no. 11:Article No. L11803.PNNL-SA-71529.doi:10.1029/2010GL043362