{"title":"非球面大气散射体极化变量的全波电磁计算","authors":"D. Mirković, D. Zrnic, A. Ryzhkov","doi":"10.1109/USNC-URSI-NRSM.2013.6525014","DOIUrl":null,"url":null,"abstract":"A model of spheroid is commonly utilized to simulate polarimetric characteristics of natural scatterers in atmosphere such as hydrometeors or biota (birds, insects, bats, etc.) The estimates of polarimetric radar variables are usually obtained using either closed form Rayleigh solutions, if size of particle is much smaller than radar wavelength or T-matrix codes otherwise.","PeriodicalId":123571,"journal":{"name":"2013 US National Committee of URSI National Radio Science Meeting (USNC-URSI NRSM)","volume":"65 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2013-06-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"Full wave EM calculation of polarimetric variables for the atmospheric scatterers with nonspheroidal shape\",\"authors\":\"D. Mirković, D. Zrnic, A. Ryzhkov\",\"doi\":\"10.1109/USNC-URSI-NRSM.2013.6525014\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"A model of spheroid is commonly utilized to simulate polarimetric characteristics of natural scatterers in atmosphere such as hydrometeors or biota (birds, insects, bats, etc.) The estimates of polarimetric radar variables are usually obtained using either closed form Rayleigh solutions, if size of particle is much smaller than radar wavelength or T-matrix codes otherwise.\",\"PeriodicalId\":123571,\"journal\":{\"name\":\"2013 US National Committee of URSI National Radio Science Meeting (USNC-URSI NRSM)\",\"volume\":\"65 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2013-06-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2013 US National Committee of URSI National Radio Science Meeting (USNC-URSI NRSM)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/USNC-URSI-NRSM.2013.6525014\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2013 US National Committee of URSI National Radio Science Meeting (USNC-URSI NRSM)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/USNC-URSI-NRSM.2013.6525014","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Full wave EM calculation of polarimetric variables for the atmospheric scatterers with nonspheroidal shape
A model of spheroid is commonly utilized to simulate polarimetric characteristics of natural scatterers in atmosphere such as hydrometeors or biota (birds, insects, bats, etc.) The estimates of polarimetric radar variables are usually obtained using either closed form Rayleigh solutions, if size of particle is much smaller than radar wavelength or T-matrix codes otherwise.