HR: 14:55h
AN: A32C-05 [PDF]
TI: IN SITU AEROSOL SIZE DISTRIBUTIONS AND RADIATIVE CLOSURE STUDY DURING AEROSOL INTENSIVE OPERATION
PERIOD (ARM-IOP)
AU: * Wang, J
EM: jian@bnl.gov
AF: Brookhaven National Lab, Bldg. 815E,
75 Rutherford Drive, Upton, NY 11973-5000 United States
AU: Collins, D R
EM: dcollins@tamu.edu
AF: Texas A&M University, Department of Atmospheric Sciences
3150 TAMU, College Station, TX 77843-3150 United States
AU: Gasparini, R
EM: gasparini@tamu.edu
AF: Texas A&M University, Department of Atmospheric Sciences
3150 TAMU, College Station, TX 77843-3150 United States
AU: Lee, Y
EM: ynlee@bnl.gov
AF: Brookhaven National Lab, Bldg. 815E,
75 Rutherford Drive, Upton, NY 11973-5000 United States
AU: Nunnermacker, L J
EM: lindan@bnl.gov
AF: Brookhaven National Lab, Bldg. 815E,
75 Rutherford Drive, Upton, NY 11973-5000 United States
AU: Ogren, J A
EM: John.A.Ogren@noaa.gov
AF: Climate Monitoring & Diagnostics Laboratory, 325 Broadway R/CMDL, Boulder, CO 80305 United States
AU: Sheridan, P
EM: Patrick.Sheridan@noaa.gov
AF: Climate Monitoring & Diagnostics Laboratory, 325 Broadway R/CMDL, Boulder, CO 80305 United States
AU: Song, Z
AF: Guangzhou Institute of Geochemistry, Guangzhou Institute of Geochemistry, Guangzhou, 510640
China
AB:
During the Aerosol Intensive Operation Period of the Department of Energy's Atmospheric Radiation Measurement (ARM) program,
the microphysical, chemical, and radiative properties of atmospheric aerosol were characterized in detail at ARM Southern
Great Plains (SGP) site in north central Oklahoma in May, 2003. A differential mobility analyzer and an optical particle
counter measured aerosol size distribution from 25 nanometers to several microns. Aerosol chemical composition and
hygroscopicity were characterized using a Particle Into Liquid Sampler and a high flow tandem differential mobility analyzer
system, respectively. Combined with the chemical composition and hygroscopicity measurements, aerosol size distributions
measured were used to predict a wide range of aerosol optical properties and compared to the simultaneous direct
measurements. This closure study allows one to assess the validity of the physicochemical description of the aerosol when
closure is achieved, and also provides insight into potential sources of error when some or all of the comparisons result in
disagreement.
DE: 0305 Aerosols and particles (0345, 4801)
DE: 0360 Transmission and scattering of radiation
DE: 4801 Aerosols (0305)
SC: Atmospheric Sciences [A]
MN: 2003 Fall Meeting