{"title":"侧视激光雷达的多重散射","authors":"Y. Benayahu, S. Fastig, A. Cohen","doi":"10.1364/orsa.1991.owe2","DOIUrl":null,"url":null,"abstract":"It is accepted that the contribution of multiple scattering in Lidar measurements from optically dense media causes difficulties in the interpretation of the Lidar signal usually based on a single-scattering approximation(1). This is due to the fact that most methods used in the past for inferring particle sizes from measurements obtained by a Lidar, were based on spectral or angular single scattering measurements(2). On the other hand the multiple scattering itself provides an additional piece of information when it can be separated from the single-scattering contribution.This additional information is used below to deduce the cloud droplet size distribution function.","PeriodicalId":320202,"journal":{"name":"Optical Remote Sensing of the Atmosphere","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Multiple Scattering by The Side Looking Lidar\",\"authors\":\"Y. Benayahu, S. Fastig, A. Cohen\",\"doi\":\"10.1364/orsa.1991.owe2\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"It is accepted that the contribution of multiple scattering in Lidar measurements from optically dense media causes difficulties in the interpretation of the Lidar signal usually based on a single-scattering approximation(1). This is due to the fact that most methods used in the past for inferring particle sizes from measurements obtained by a Lidar, were based on spectral or angular single scattering measurements(2). On the other hand the multiple scattering itself provides an additional piece of information when it can be separated from the single-scattering contribution.This additional information is used below to deduce the cloud droplet size distribution function.\",\"PeriodicalId\":320202,\"journal\":{\"name\":\"Optical Remote Sensing of the Atmosphere\",\"volume\":\"1 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Optical Remote Sensing of the Atmosphere\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1364/orsa.1991.owe2\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Optical Remote Sensing of the Atmosphere","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1364/orsa.1991.owe2","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
It is accepted that the contribution of multiple scattering in Lidar measurements from optically dense media causes difficulties in the interpretation of the Lidar signal usually based on a single-scattering approximation(1). This is due to the fact that most methods used in the past for inferring particle sizes from measurements obtained by a Lidar, were based on spectral or angular single scattering measurements(2). On the other hand the multiple scattering itself provides an additional piece of information when it can be separated from the single-scattering contribution.This additional information is used below to deduce the cloud droplet size distribution function.