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Aerosol Obsveration System (AOS) in the MAGICal experiment

Aerosol Obsveration System (AOS) in the MAGICal experiment . Gunnar Senum BNL. First MAGIC Science Workshop. Aerosol Instrumentation. CPC (Condensation Particle Counter) Measures the Total Aerosol Particle Concentration from 10 nm and up.

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Aerosol Obsveration System (AOS) in the MAGICal experiment

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  1. Aerosol Obsveration System (AOS) in the MAGICal experiment Gunnar Senum BNL First MAGIC Science Workshop

  2. Aerosol Instrumentation CPC (Condensation Particle Counter) Measures the Total Aerosol Particle Concentration from 10 nm and up. UHSAS (Ultra High Sensitivity Aerosol Spectrometer Measures the Aerosol Size Concentration Distribution from 55nm to 1000nm. CCN (Cloud Condensation Nuclei Counter) Measures the concentration of aerosols that can be activated as cloud nuclei at specified humidity supersaturation, 0.2 to 1 %. Nephelometers Measures the light scattering of aerosol particles at 450, 550 and 700 nm, humidified and or dried, and or with size cuts at 1 and 10 microns. 4a. Humidigraph Dries or humidifies the aerosol sample, in between the 2 Nephs PSAP (Particulate Soot Absorption Photometer) Measures the light absorption of aerosols, and with the Neph data will yield aerosol albedo. Also sized cuts at 1 and 10 microns. HT-DMA (Humidified Tandem-Differential Mobility Analyzer) Measures the hygroscopicity of aerosols as a function of aerosol size. Ozone Measures the ambient ozone concentration. Meteorology Ambient temperature, humidity, precipitation, windspeed and direction.

  3. How do these aerosol measurements relate to science Next slides will illustrate some examples

  4. Example of the AOS Science The discontinuity is from the aerosol particle impactor, which removes particles from greater than 1 micron (lower traces). Note how the red scattering is predominating about 0900, due to more larger particles.

  5. Examples of AOS Science This is an example of the “Humidigraph” which is between the two Nephs in the AOS. This alternately dries and humidifies the aerosol sample. Note between 1000 and 1400, that the aerosol particles are more hygroscopic, they grow much with the applied humidity.

  6. Example of AOS Science This is the CCN data for the same data as the previous slide. Note again we have more hydrophilic aerosol particles from 1000 to 1200. The CCNs are almost all activated by 0.4% supersaturation.

  7. Examples of AOS Science This is an example of the UHSAS. Almost every day has evidence of ship emissions from other ships in the LA-Hawaii shipping lane. Note that these sharp ship emission spikes are anti-correlated with calculated aerosol mean radius, since diesel ship emissions are very small sizes, less that 50nm. Blindly averaging this data would leave to an incorrect result.

  8. Example of AOS Science This is the same UHSAS dataset as the previous slide. I have made use of the anti-corelation and segregated out the ship emissions. Note that there are only three major ship emission peaks, but they are broader and larger, that is, more aged ship emissions. This when averaged would be realistic of a maritime aerosol background

  9. Same day as earlier, and note the “aged” ship emissions are more hydrophilic and CCN activated

  10. This is one of the worst examples of the UHSAS data, totally contaminated with ship emissions Here, is the same data, but the ship emissions are segregated out

  11. Mentors AOS Mentor: Stephen Springston: Infrastructure, ozone, met: Stephen Springston CCN, UHSAS, Neph, HT-DMA: Gunnar Senum CPC : ChongaiKuang PSAP: Art Sedlacek

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