Determining aerosol radiative properties using the TSI 3563 integrating nephelometer

被引:725
作者
Anderson, TL
Ogren, JA
机构
[1] Univ Washington, Joint Inst Study Atmosphere & Oceans, Seattle, WA 98195 USA
[2] NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80803 USA
基金
美国国家航空航天局;
关键词
D O I
10.1080/02786829808965551
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
Methods for reducing and quantifying the uncertainties in aerosol optical properties measured with the TSI 3563 integrating nephelometer are presented. For nearly all applications, the recommended calibration gases are air and CO,. By routinely characterizing the instrumental response to these gases, a diagnostic record of instrument performance can be created. This record can be used to improve measurement accuracy and quantify uncertainties due to instrumental noise and calibration drift. When measuring scattering by particles, size segregation upstream of the nephelometer at about I Crm aerodynamic diameter greatly increases the information content of the data for two reasons: one stemming from the independence of coarse and fine particles in the atmosphere, and the second stemming from the size dependence of the nephelometer response. For many applications (e.g., extinction budget studies) it is important to correct nephelometer data for the effects of angular nonidealities. Correction factors appropriate to a broad range of sampling conditions are given herein and are shown to be constrained by the wavelength dependence of light scattering, as measured by the nephelometer. Finally, the nephelometer measurement is nondestructive, such that the sampled aerosol can be further analyzed downstream. Data from two nephelometers operated in series are used to evaluate this procedure. A small loss of super-mu m particles (5-10%) is found, while the sub-mu m data demonstrates measurement reproducibility within +/- 1%. (C) 1998 American Association for Aerosol Research.
引用
收藏
页码:57 / 69
页数:13
相关论文
共 25 条
[1]  
Anderson TL, 1996, J ATMOS OCEAN TECH, V13, P967, DOI 10.1175/1520-0426(1996)013<0967:PCOAHS>2.0.CO
[2]  
2
[3]   Evaporation of ammonium nitrate aerosol in a heated nephelometer: Implications for field measurements [J].
Bergin, MH ;
Ogren, JA ;
Schwartz, SE ;
McInnes, LM .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1997, 31 (10) :2878-2883
[4]   Vertical profiles, aerosol microphysics, and optical closure during the Atlantic Stratocumulus Transition Experiment: Measured and modeled column optical properties [J].
Clarke, AD ;
Porter, JN ;
Valero, FPJ ;
Pilewskie, P .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D2) :4443-4453
[5]  
Covert D. S., 1972, Journal of Applied Meteorology, V11, P968, DOI 10.1175/1520-0450(1972)011<0968:ASOTRO>2.0.CO
[6]  
2
[7]  
ENSOR DS, 1970, ATMOS ENVIRON, V4, P481
[8]   RAYLEIGH VOLUME SCATTERING COEFFICIENTS FOR FREON-12, FREON-22, AND SULFUR-HEXAFLUORIDE [J].
HARRISON, AW .
CANADIAN JOURNAL OF PHYSICS, 1977, 55 (21) :1898-1901
[9]  
Heintzenberg J, 1996, J ATMOS OCEAN TECH, V13, P987, DOI 10.1175/1520-0426(1996)013<0987:DAAOTI>2.0.CO
[10]  
2