GSTDTAP  > 地球科学
DOI10.5194/acp-18-11847-2018
Depolarization and lidar ratios at 355, 532, and 1064 nm and microphysical properties of aged tropospheric and stratospheric Canadian wildfire smoke
Haarig, Moritz1; Ansmann, Albert1; Baars, Holger1; Jimenez, Cristofer1; Veselovskii, Igor2; Engelmann, Ronny1; Althausen, Dietrich1
2018-08-20
发表期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN1680-7316
EISSN1680-7324
出版年2018
卷号18期号:16页码:11847-11861
文章类型Article
语种英语
国家Germany; Russia
英文摘要

We present spectrally resolved optical and microphysical properties of western Canadian wildfire smoke observed in a tropospheric layer from 5-6.5 km height and in a stratospheric layer from 15-16 km height during a record-breaking smoke event on 22 August 2017. Three polarization/Raman lidars were run at the European Aerosol Research Lidar Network (EARLINET) station of Leipzig, Germany, after sunset on 22 August. For the first time, the linear depolarization ratio and extinction-to-backscatter ratio (lidar ratio) of aged smoke particles were measured at all three important lidar wavelengths of 355, 532, and 1064 nm. Very different particle depolarization ratios were found in the troposphere and in the stratosphere. The obviously compact and spherical tropospheric smoke particles caused almost no depolarization of backscattered laser radiation at all three wavelengths (< 3 %), whereas the dry irregularly shaped soot particles in the stratosphere lead to high depolarization ratios of 22% at 355 nm and 18% at 532 nm and a comparably low value of 4% at 1064 nm. The lidar ratios were 4045 sr (355 nm), 65-80 sr (532 nm), and 80-95 sr (1064 nm) in both the tropospheric and stratospheric smoke layers indicating similar scattering and absorption properties. The strong wavelength dependence of the stratospheric depolarization ratio was probably caused by the absence of a particle coarse mode (particle mode consisting of particles with radius > 500 nm). The stratospheric smoke particles formed a pronounced accumulation mode (in terms of particle volume or mass) centered at a particle radius of 350-400 nm. The effective particle radius was 0.32 mu m. The tropospheric smoke particles were much smaller (effective radius of 0.17 mu m). Mass concentrations were of the order of 5.5 mu g m(-3) (tropospheric layer) and 40 mu g m(-3) (stratospheric layer) in the night of 22 August 2017. The single scattering albedo of the stratospheric particles was estimated to be 0.74, 0.8, and 0.83 at 355, 532, and 1064 nm, respectively.


领域地球科学
收录类别SCI-E
WOS记录号WOS:000442099800005
WOS关键词MULTIWAVELENGTH RAMAN LIDAR ; FOREST-FIRE SMOKE ; MINERAL DUST ; OPTICAL-PROPERTIES ; SAHARAN DUST ; AEROSOL CLASSIFICATION ; POLARIZATION LIDAR ; EARLINET ; CALIPSO ; BACKSCATTER
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/21696
专题地球科学
作者单位1.Leibniz Inst Tropospher Res, Leipzig, Germany;
2.Gen Phys Inst, Phys Instrumentat Ctr, Moscow, Russia
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GB/T 7714
Haarig, Moritz,Ansmann, Albert,Baars, Holger,et al. Depolarization and lidar ratios at 355, 532, and 1064 nm and microphysical properties of aged tropospheric and stratospheric Canadian wildfire smoke[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2018,18(16):11847-11861.
APA Haarig, Moritz.,Ansmann, Albert.,Baars, Holger.,Jimenez, Cristofer.,Veselovskii, Igor.,...&Althausen, Dietrich.(2018).Depolarization and lidar ratios at 355, 532, and 1064 nm and microphysical properties of aged tropospheric and stratospheric Canadian wildfire smoke.ATMOSPHERIC CHEMISTRY AND PHYSICS,18(16),11847-11861.
MLA Haarig, Moritz,et al."Depolarization and lidar ratios at 355, 532, and 1064 nm and microphysical properties of aged tropospheric and stratospheric Canadian wildfire smoke".ATMOSPHERIC CHEMISTRY AND PHYSICS 18.16(2018):11847-11861.
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