Airborne Aerosol in Situ Measurements during TCAP: A Closure Study of Total Scattering
We present a framework for calculating the total scattering of both non-absorbing and absorbing aerosol at ambient conditions from aircraft data. Our framework is developed emphasizing the explicit use of chemical composition data for estimating the complex refractive index (RI) of particles, and t...
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doaj-f2113411ecf849b5a0653f83d834c5172020-11-24T23:46:40ZengMDPI AGAtmosphere2073-44332015-07-01681069110110.3390/atmos6081069atmos6081069Airborne Aerosol in Situ Measurements during TCAP: A Closure Study of Total ScatteringEvgueni Kassianov0Larry K. Berg1Mikhail Pekour2James Barnard3Duli Chand4Connor Flynn5Mikhail Ovchinnikov6Arthur Sedlacek7Beat Schmid8John Shilling9Jason Tomlinson10Jerome Fast11Pacific Northwest National Laboratory, Richland, WA 99352, USAPacific Northwest National Laboratory, Richland, WA 99352, USAPacific Northwest National Laboratory, Richland, WA 99352, USADepartment of Physics, University of Nevada, Reno, NV 89557, USAPacific Northwest National Laboratory, Richland, WA 99352, USAPacific Northwest National Laboratory, Richland, WA 99352, USAPacific Northwest National Laboratory, Richland, WA 99352, USABrookhaven National Laboratory, Upton, NY 11973, USAPacific Northwest National Laboratory, Richland, WA 99352, USAPacific Northwest National Laboratory, Richland, WA 99352, USAPacific Northwest National Laboratory, Richland, WA 99352, USAPacific Northwest National Laboratory, Richland, WA 99352, USAWe present a framework for calculating the total scattering of both non-absorbing and absorbing aerosol at ambient conditions from aircraft data. Our framework is developed emphasizing the explicit use of chemical composition data for estimating the complex refractive index (RI) of particles, and thus obtaining improved ambient size spectra derived from Optical Particle Counter (OPC) measurements. The feasibility of our framework for improved calculations of total scattering is demonstrated using three types of data collected by the U.S. Department of Energy’s (DOE) aircraft during the Two-Column Aerosol Project (TCAP). Namely, these data types are: (1) size distributions measured by a suite of OPC’s; (2) chemical composition data measured by an Aerosol Mass Spectrometer and a Single Particle Soot Photometer; and (3) the dry total scattering coefficient measured by a integrating nephelometer and scattering enhancement factor measured with a humidification system. We demonstrate that good agreement (~10%) between the observed and calculated scattering can be obtained under ambient conditions (RH < 80%) by applying chemical composition data for the RI-based correction of the OPC-derived size spectra. We also demonstrate that ignoring the RI-based correction or using non-representative RI values can cause a substantial underestimation (~40%) or overestimation (~35%) of the calculated scattering, respectively.http://www.mdpi.com/2073-4433/6/8/1069aircraft measurements of aerosol microphysical, chemical, and optical components and ambient relative humidityUltra-High Sensitivity Aerosol Spectrometer (UHSAS)Passive Cavity Aerosol Spectrometer (PCASP)Cloud and Aerosol Spectrometer (CAS)Aerosol Mass Spectrometer (AMS)Single Particle Soot Photometer (SP2)integrating nephelometerhumidification systemTwo-Column Aerosol Project (TCAP) |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Evgueni Kassianov Larry K. Berg Mikhail Pekour James Barnard Duli Chand Connor Flynn Mikhail Ovchinnikov Arthur Sedlacek Beat Schmid John Shilling Jason Tomlinson Jerome Fast |
spellingShingle |
Evgueni Kassianov Larry K. Berg Mikhail Pekour James Barnard Duli Chand Connor Flynn Mikhail Ovchinnikov Arthur Sedlacek Beat Schmid John Shilling Jason Tomlinson Jerome Fast Airborne Aerosol in Situ Measurements during TCAP: A Closure Study of Total Scattering Atmosphere aircraft measurements of aerosol microphysical, chemical, and optical components and ambient relative humidity Ultra-High Sensitivity Aerosol Spectrometer (UHSAS) Passive Cavity Aerosol Spectrometer (PCASP) Cloud and Aerosol Spectrometer (CAS) Aerosol Mass Spectrometer (AMS) Single Particle Soot Photometer (SP2) integrating nephelometer humidification system Two-Column Aerosol Project (TCAP) |
author_facet |
Evgueni Kassianov Larry K. Berg Mikhail Pekour James Barnard Duli Chand Connor Flynn Mikhail Ovchinnikov Arthur Sedlacek Beat Schmid John Shilling Jason Tomlinson Jerome Fast |
author_sort |
Evgueni Kassianov |
title |
Airborne Aerosol in Situ Measurements during TCAP: A Closure Study of Total Scattering |
title_short |
Airborne Aerosol in Situ Measurements during TCAP: A Closure Study of Total Scattering |
title_full |
Airborne Aerosol in Situ Measurements during TCAP: A Closure Study of Total Scattering |
title_fullStr |
Airborne Aerosol in Situ Measurements during TCAP: A Closure Study of Total Scattering |
title_full_unstemmed |
Airborne Aerosol in Situ Measurements during TCAP: A Closure Study of Total Scattering |
title_sort |
airborne aerosol in situ measurements during tcap: a closure study of total scattering |
publisher |
MDPI AG |
series |
Atmosphere |
issn |
2073-4433 |
publishDate |
2015-07-01 |
description |
We present a framework for calculating the total scattering of both non-absorbing and absorbing aerosol at ambient conditions from aircraft data. Our framework is developed emphasizing the explicit use of chemical composition data for estimating the complex refractive index (RI) of particles, and thus obtaining improved ambient size spectra derived from Optical Particle Counter (OPC) measurements. The feasibility of our framework for improved calculations of total scattering is demonstrated using three types of data collected by the U.S. Department of Energy’s (DOE) aircraft during the Two-Column Aerosol Project (TCAP). Namely, these data types are: (1) size distributions measured by a suite of OPC’s; (2) chemical composition data measured by an Aerosol Mass Spectrometer and a Single Particle Soot Photometer; and (3) the dry total scattering coefficient measured by a integrating nephelometer and scattering enhancement factor measured with a humidification system. We demonstrate that good agreement (~10%) between the observed and calculated scattering can be obtained under ambient conditions (RH < 80%) by applying chemical composition data for the RI-based correction of the OPC-derived size spectra. We also demonstrate that ignoring the RI-based correction or using non-representative RI values can cause a substantial underestimation (~40%) or overestimation (~35%) of the calculated scattering, respectively. |
topic |
aircraft measurements of aerosol microphysical, chemical, and optical components and ambient relative humidity Ultra-High Sensitivity Aerosol Spectrometer (UHSAS) Passive Cavity Aerosol Spectrometer (PCASP) Cloud and Aerosol Spectrometer (CAS) Aerosol Mass Spectrometer (AMS) Single Particle Soot Photometer (SP2) integrating nephelometer humidification system Two-Column Aerosol Project (TCAP) |
url |
http://www.mdpi.com/2073-4433/6/8/1069 |
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