{"title":"以Pearson-Moskowitz谱密度函数表征的表面的后向散射光学和微波截面-全波方法","authors":"E. Bahar, B. Lee","doi":"10.1109/COMEAS.1995.472330","DOIUrl":null,"url":null,"abstract":"In the study of wave scattering from terrain, ice, sea and other features on the Earth's surface, the use of the full wave approach leads to solutions that are valid over a broad range of frequencies and roughness scales. The backscattering radar cross sections for two-dimensional random rough surfaces are obtained for surfaces characterized by the Pearson-Moskowitz surface height spectral density function using the full wave approach. These solutions properly account for the small and large scale components of the rough sea surface. They are compared with solutions for surfaces characterized by the usually assumed Gaussian spectral density functions. The impact of the particular rough surface height spectral density function is discussed.<<ETX>>","PeriodicalId":274878,"journal":{"name":"Conference Proceedings Second Topical Symposium on Combined Optical-Microwave Earth and Atmosphere Sensing","volume":"24 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1995-04-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Backscatter optical and microwave cross sections for surfaces characterized by Pearson-Moskowitz spectral density functions-full wave approach\",\"authors\":\"E. Bahar, B. Lee\",\"doi\":\"10.1109/COMEAS.1995.472330\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In the study of wave scattering from terrain, ice, sea and other features on the Earth's surface, the use of the full wave approach leads to solutions that are valid over a broad range of frequencies and roughness scales. The backscattering radar cross sections for two-dimensional random rough surfaces are obtained for surfaces characterized by the Pearson-Moskowitz surface height spectral density function using the full wave approach. These solutions properly account for the small and large scale components of the rough sea surface. They are compared with solutions for surfaces characterized by the usually assumed Gaussian spectral density functions. The impact of the particular rough surface height spectral density function is discussed.<<ETX>>\",\"PeriodicalId\":274878,\"journal\":{\"name\":\"Conference Proceedings Second Topical Symposium on Combined Optical-Microwave Earth and Atmosphere Sensing\",\"volume\":\"24 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1995-04-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Conference Proceedings Second Topical Symposium on Combined Optical-Microwave Earth and Atmosphere Sensing\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/COMEAS.1995.472330\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Conference Proceedings Second Topical Symposium on Combined Optical-Microwave Earth and Atmosphere Sensing","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/COMEAS.1995.472330","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Backscatter optical and microwave cross sections for surfaces characterized by Pearson-Moskowitz spectral density functions-full wave approach
In the study of wave scattering from terrain, ice, sea and other features on the Earth's surface, the use of the full wave approach leads to solutions that are valid over a broad range of frequencies and roughness scales. The backscattering radar cross sections for two-dimensional random rough surfaces are obtained for surfaces characterized by the Pearson-Moskowitz surface height spectral density function using the full wave approach. These solutions properly account for the small and large scale components of the rough sea surface. They are compared with solutions for surfaces characterized by the usually assumed Gaussian spectral density functions. The impact of the particular rough surface height spectral density function is discussed.<>