{"title":"威德尔海的雪湿度和Ssmii亮度温度","authors":"C. Garrity, R.O. Ramseier, I. Rubinstein","doi":"10.1109/IGARSS.1990.688792","DOIUrl":null,"url":null,"abstract":"During the Winter Weddell Gyre Study 1989, the RV ”Polarstern“ transected the Weddell Sea West to East. Detailed snow pit studies which included the determination of the amount of free water within the snow pack were correlated with the brightness temperatures from the Special Sensor Microwave/Imager. The results indicate a steep increase in brightness temperatures with increasing free water content from 0 to 1% by volume.","PeriodicalId":377626,"journal":{"name":"10th Annual International Symposium on Geoscience and Remote Sensing","volume":"22 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1990-05-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"6","resultStr":"{\"title\":\"Snow Wetness And Ssmii Brightness Temperatures For The Weddell Sea\",\"authors\":\"C. Garrity, R.O. Ramseier, I. Rubinstein\",\"doi\":\"10.1109/IGARSS.1990.688792\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"During the Winter Weddell Gyre Study 1989, the RV ”Polarstern“ transected the Weddell Sea West to East. Detailed snow pit studies which included the determination of the amount of free water within the snow pack were correlated with the brightness temperatures from the Special Sensor Microwave/Imager. The results indicate a steep increase in brightness temperatures with increasing free water content from 0 to 1% by volume.\",\"PeriodicalId\":377626,\"journal\":{\"name\":\"10th Annual International Symposium on Geoscience and Remote Sensing\",\"volume\":\"22 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1990-05-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"6\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"10th Annual International Symposium on Geoscience and Remote Sensing\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/IGARSS.1990.688792\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"10th Annual International Symposium on Geoscience and Remote Sensing","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/IGARSS.1990.688792","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Snow Wetness And Ssmii Brightness Temperatures For The Weddell Sea
During the Winter Weddell Gyre Study 1989, the RV ”Polarstern“ transected the Weddell Sea West to East. Detailed snow pit studies which included the determination of the amount of free water within the snow pack were correlated with the brightness temperatures from the Special Sensor Microwave/Imager. The results indicate a steep increase in brightness temperatures with increasing free water content from 0 to 1% by volume.