{"title":"红外CO2 q -支线混合的实验观察","authors":"B. Gentry, L. Strow","doi":"10.1364/lors.1987.tuc19","DOIUrl":null,"url":null,"abstract":"The successful remote sensing of atmospheric temperature, humidity, pressure, and trace gas profiles depends upon a detailed knowledge of the radiative characteristics of atmospheric gases. For example, existing passive remote temperature and humidity sounders utilize infrared spectral channels that sense atmospheric CO2, N2O, O3, and H2O.","PeriodicalId":339230,"journal":{"name":"Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques","volume":"150 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1988-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Experimental Observations of Line-Mixing In A Infrared CO2 Q-Branch\",\"authors\":\"B. Gentry, L. Strow\",\"doi\":\"10.1364/lors.1987.tuc19\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The successful remote sensing of atmospheric temperature, humidity, pressure, and trace gas profiles depends upon a detailed knowledge of the radiative characteristics of atmospheric gases. For example, existing passive remote temperature and humidity sounders utilize infrared spectral channels that sense atmospheric CO2, N2O, O3, and H2O.\",\"PeriodicalId\":339230,\"journal\":{\"name\":\"Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques\",\"volume\":\"150 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1988-08-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1364/lors.1987.tuc19\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1364/lors.1987.tuc19","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Experimental Observations of Line-Mixing In A Infrared CO2 Q-Branch
The successful remote sensing of atmospheric temperature, humidity, pressure, and trace gas profiles depends upon a detailed knowledge of the radiative characteristics of atmospheric gases. For example, existing passive remote temperature and humidity sounders utilize infrared spectral channels that sense atmospheric CO2, N2O, O3, and H2O.
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