{"title":"Influence of Suspended Hydrometeors on Determination of Dielectric Permittivity of Medium in a Cloudy Atmosphere","authors":"P. Evdokimov, E. Shirokova, I. Shirokov","doi":"10.1109/AGERS56232.2022.10093452","DOIUrl":null,"url":null,"abstract":"The article considers the possibility of using a previously developed mathematical model for calculating the dielectric constant of a cloudy atmosphere medium. For the accounting the influence of suspended hydrometeors on the value of dielectric permittivity, an expression for the electrical susceptibility of the aerosol fraction was determined. The modeling of changes in the dielectric permittivity of the medium depending on meteorological parameters at different liquid water content of atmospheric formations is carried out.","PeriodicalId":370213,"journal":{"name":"2022 IEEE Asia-Pacific Conference on Geoscience, Electronics and Remote Sensing Technology (AGERS)","volume":"66 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-12-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2022 IEEE Asia-Pacific Conference on Geoscience, Electronics and Remote Sensing Technology (AGERS)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/AGERS56232.2022.10093452","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
The article considers the possibility of using a previously developed mathematical model for calculating the dielectric constant of a cloudy atmosphere medium. For the accounting the influence of suspended hydrometeors on the value of dielectric permittivity, an expression for the electrical susceptibility of the aerosol fraction was determined. The modeling of changes in the dielectric permittivity of the medium depending on meteorological parameters at different liquid water content of atmospheric formations is carried out.
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