S. Samoilova, Y. Balin, G. Kokhanenko, S. Nasonov, I. É. Penner
{"title":"Use of lidar signals of Raman scattering for retrieval of aerosol microphysical characteristics","authors":"S. Samoilova, Y. Balin, G. Kokhanenko, S. Nasonov, I. É. Penner","doi":"10.1117/12.2645295","DOIUrl":null,"url":null,"abstract":"A procedure is proposed for deriving the aerosol microphysical characteristics of the spherical particle, the complex refractivity index m = mreal + i*mimage and the bimodal size distribution function U(r), using laser sensing data at the wavelengths within 355-1064 nm. A possibility of different optical set, (3β + 2σ) and (3β + 3σ), is studied for weakly absorbing particles for mimage ≤ 0.010, when mfine ≠ mcoarse holds. The algorithms are tested for one mfine (1.50+i*0.01) and nine mcoarse (mreal= 1.40, 1.50, 1.60; mimage = 0.0001, 0.001, 0.01). In order to include the influence of the contribution from the modal particles into the total concentration, 462 empirical models of U(r) are used.","PeriodicalId":217776,"journal":{"name":"Atmospheric and Ocean Optics","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-12-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Atmospheric and Ocean Optics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1117/12.2645295","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
A procedure is proposed for deriving the aerosol microphysical characteristics of the spherical particle, the complex refractivity index m = mreal + i*mimage and the bimodal size distribution function U(r), using laser sensing data at the wavelengths within 355-1064 nm. A possibility of different optical set, (3β + 2σ) and (3β + 3σ), is studied for weakly absorbing particles for mimage ≤ 0.010, when mfine ≠ mcoarse holds. The algorithms are tested for one mfine (1.50+i*0.01) and nine mcoarse (mreal= 1.40, 1.50, 1.60; mimage = 0.0001, 0.001, 0.01). In order to include the influence of the contribution from the modal particles into the total concentration, 462 empirical models of U(r) are used.