Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, China
This study compares the aerosol optical and physical properties simultaneously measured by a SKYNET PREDE skyradiometer and AERONET/PHOTONS CIMEL sunphotometer at a location in Beijing, China. Aerosol optical properties (AOP) including the Aerosol Optical Depth (AOD), Angstrom exponent (<i&am...
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Copernicus Publications
2008-06-01
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Series: | Atmospheric Chemistry and Physics |
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doaj-b3ac47be0e9647f3a278a8d3ef09ca682020-11-24T20:55:54ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242008-06-0181231993214Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, ChinaH. CheG. ShiA. UchiyamaA. YamazakiH. ChenP. GoloubX. ZhangThis study compares the aerosol optical and physical properties simultaneously measured by a SKYNET PREDE skyradiometer and AERONET/PHOTONS CIMEL sunphotometer at a location in Beijing, China. Aerosol optical properties (AOP) including the Aerosol Optical Depth (AOD), Angstrom exponent (<i>α</i>), volume size distribution, single scattering albedo (<i>ω</i>) and the complex refractive index were compared. The difference between the two types of instruments was less than 1.3% for the AOD and less than 4% for the single scattering albedo below the wavelength of 670 nm. There is a difference between the volume size distribution patterns derived from two instruments, which is probably due to difference of measurement protocols and inversion algorithms for the respective instruments. <br></br> AOP under three distinct weather conditions (background, haze, and dust days) over Beijing were compared by using the retrieved skyradiometer and sunphotometer data combined with MODIS satellite results, pyranometer measurements, PM<sub>10</sub> measurements, and backtrajectory analysis. The results show that the significant difference of AOP under background, haze, and dust days over Beijing is probably due to different aerosol components under distinct weather conditions. http://www.atmos-chem-phys.net/8/3199/2008/acp-8-3199-2008.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
H. Che G. Shi A. Uchiyama A. Yamazaki H. Chen P. Goloub X. Zhang |
spellingShingle |
H. Che G. Shi A. Uchiyama A. Yamazaki H. Chen P. Goloub X. Zhang Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, China Atmospheric Chemistry and Physics |
author_facet |
H. Che G. Shi A. Uchiyama A. Yamazaki H. Chen P. Goloub X. Zhang |
author_sort |
H. Che |
title |
Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, China |
title_short |
Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, China |
title_full |
Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, China |
title_fullStr |
Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, China |
title_full_unstemmed |
Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, China |
title_sort |
intercomparison between aerosol optical properties by a prede skyradiometer and cimel sunphotometer over beijing, china |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2008-06-01 |
description |
This study compares the aerosol optical and physical properties simultaneously measured by a SKYNET PREDE skyradiometer and AERONET/PHOTONS CIMEL sunphotometer at a location in Beijing, China. Aerosol optical properties (AOP) including the Aerosol Optical Depth (AOD), Angstrom exponent (<i>α</i>), volume size distribution, single scattering albedo (<i>ω</i>) and the complex refractive index were compared. The difference between the two types of instruments was less than 1.3% for the AOD and less than 4% for the single scattering albedo below the wavelength of 670 nm. There is a difference between the volume size distribution patterns derived from two instruments, which is probably due to difference of measurement protocols and inversion algorithms for the respective instruments. <br></br> AOP under three distinct weather conditions (background, haze, and dust days) over Beijing were compared by using the retrieved skyradiometer and sunphotometer data combined with MODIS satellite results, pyranometer measurements, PM<sub>10</sub> measurements, and backtrajectory analysis. The results show that the significant difference of AOP under background, haze, and dust days over Beijing is probably due to different aerosol components under distinct weather conditions. |
url |
http://www.atmos-chem-phys.net/8/3199/2008/acp-8-3199-2008.pdf |
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