{"title":"l波段辐射测量和粗糙海洋表面对星系的反射","authors":"E. Dinnat, D. L. Le Vine, S. Abraham","doi":"10.1109/MICRAD.2008.4579494","DOIUrl":null,"url":null,"abstract":"The celestial sky brightness temperature reflected by the ocean surface toward an L-band radiometer induces a signal that needs to be known in order to retrieve sea surface salinity. To provide an accurate correction, the effects of the surface roughness and the antenna gain pattern need to be included. We assess the impact of these effects on the reflected sky signal using the Aquarius radiometer as an example.","PeriodicalId":193521,"journal":{"name":"2008 Microwave Radiometry and Remote Sensing of the Environment","volume":"35 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2008-03-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"L-band radiometry and reflection of the galaxy by a rough ocean surface\",\"authors\":\"E. Dinnat, D. L. Le Vine, S. Abraham\",\"doi\":\"10.1109/MICRAD.2008.4579494\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The celestial sky brightness temperature reflected by the ocean surface toward an L-band radiometer induces a signal that needs to be known in order to retrieve sea surface salinity. To provide an accurate correction, the effects of the surface roughness and the antenna gain pattern need to be included. We assess the impact of these effects on the reflected sky signal using the Aquarius radiometer as an example.\",\"PeriodicalId\":193521,\"journal\":{\"name\":\"2008 Microwave Radiometry and Remote Sensing of the Environment\",\"volume\":\"35 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2008-03-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2008 Microwave Radiometry and Remote Sensing of the Environment\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/MICRAD.2008.4579494\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2008 Microwave Radiometry and Remote Sensing of the Environment","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/MICRAD.2008.4579494","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
L-band radiometry and reflection of the galaxy by a rough ocean surface
The celestial sky brightness temperature reflected by the ocean surface toward an L-band radiometer induces a signal that needs to be known in order to retrieve sea surface salinity. To provide an accurate correction, the effects of the surface roughness and the antenna gain pattern need to be included. We assess the impact of these effects on the reflected sky signal using the Aquarius radiometer as an example.