You have requested a machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Neither SPIE nor the owners and publishers of the content make, and they explicitly disclaim, any express or implied representations or warranties of any kind, including, without limitation, representations and warranties as to the functionality of the translation feature or the accuracy or completeness of the translations.
Translations are not retained in our system. Your use of this feature and the translations is subject to all use restrictions contained in the Terms and Conditions of Use of the SPIE website.
12 November 2020Investigation of condensation grows of aerosol particles
This document presents the results of the study of condesation grows of atmospheric aerosol. We analyze effect of aerosol effective radius changes versus relative humidity. In our experiment we suppose that aerosol has same type (refractive index) during the measurements. We consider different scatterplots Ref f vs RH, β vs RH and α vs RH inside planetary boundary layer and estimate humidification factor. From the experiment we found that: 1) the radius of the particles grows with the index k = 0.484 in accordance with formula (10); 2) an increase in the backscattering coefficients at wavelengths of 355 nm and 532 nm is described by formula (11) and γ = 0.694 and γ= 0.585, respectively. Trend of particulate depolarization ratio as a function of relative humidity corresponds to Case II of Continental Clean atmospere model where water soluble particles has spherical shape.
The alert did not successfully save. Please try again later.
Konstantin A. Shmirko, Vladimir V. Lisitsa, Andrey N. Pavlov, Sergey Yu. Stolyarchuk, "Investigation of condensation grows of aerosol particles," Proc. SPIE 11560, 26th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, 115604P (12 November 2020); https://doi.org/10.1117/12.2575588