COMPLICATED MATTER
Aerosols are small, complex clumps of matter, composed of anything in the atmosphere that's not a gas, and even in very small concentrations--parts per million or parts per billion--they can have major impacts on the overall dynamics of the Earth's climate. In addition to health effects and overall air quality, aerosols affect climate directly, by absorbing and scattering the sun's radiation, and indirectly, by changing the optical properties, lifetimes, and amounts of clouds. And just as importantly for atmospheric simulations, aerosols act as a small aqueous-phase chemical reactor.
Dabdub's group has pioneered the computational modeling of atmospheric aerosols, and their developments for modeling both the total mass and size distribution of the particles was published in the February 20, 1998, Journal of Geophysical Research and the July 4, 1997, Science. The main advance in Dabdub's model is that it does not make an assumption commonly used to simplify the computation in other models.
"Unlike earlier models, we have not assumed instantaneous gas-aerosol equilibrium for volatile inorganics," said Dabdub, a professor in UC Irvine's Mechanical and Aerospace Engineering Department and leader of the Earth Systems Science thrust area Atmospheric Chemistry project. "This assumption is usually made because otherwise it becomes a major computational sink and one of the most demanding parts of the model." In fact, the aerosol module consumes more than 90 percent of the CPU cycles used in an atmospheric simulation.
The equilibrium assumption works well in predicting the behavior of gasses in the atmosphere, such as carbon dioxide and organic vapors, but experimental studies have shown that it does not always hold for aerosols. For some compounds, mass transfer equilibrium between the gas and aerosol phase is established slowly relative to the time scale over which other changes are occurring. Thus, to be more accurate, the most general form of an aerosol model should not rely on the assumption of instantaneous, local equilibrium of volatile aerosol types.
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