{"title":"飞机大气光谱热发射的测量","authors":"G. Finger, F. Kneubühl","doi":"10.1109/ICSWA.1981.9335138","DOIUrl":null,"url":null,"abstract":"The measurement of the atmospheric thermal emission is important for several reasons. Remote sensing working in the wavelength regions from λ = 3 μm to λ = 5 μm and from λ = 8 μm to λ = 14 μm, with high atmospheric transparency is hampered by absorption and thermal emission of the intervening atmosphere. Furthermore, both the global energy balance and the radiative heating loss of the outdoor surface of building envelopes crucially depend on atmospheric thermal emission |1|.","PeriodicalId":254777,"journal":{"name":"1981 International Conference on Submillimeter Waves and Their Applications","volume":"72 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1981-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Measurement of the Spectral Thermal Emission of the Atmosphere from an Aircraft\",\"authors\":\"G. Finger, F. Kneubühl\",\"doi\":\"10.1109/ICSWA.1981.9335138\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The measurement of the atmospheric thermal emission is important for several reasons. Remote sensing working in the wavelength regions from λ = 3 μm to λ = 5 μm and from λ = 8 μm to λ = 14 μm, with high atmospheric transparency is hampered by absorption and thermal emission of the intervening atmosphere. Furthermore, both the global energy balance and the radiative heating loss of the outdoor surface of building envelopes crucially depend on atmospheric thermal emission |1|.\",\"PeriodicalId\":254777,\"journal\":{\"name\":\"1981 International Conference on Submillimeter Waves and Their Applications\",\"volume\":\"72 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1981-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"1981 International Conference on Submillimeter Waves and Their Applications\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/ICSWA.1981.9335138\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"1981 International Conference on Submillimeter Waves and Their Applications","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICSWA.1981.9335138","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Measurement of the Spectral Thermal Emission of the Atmosphere from an Aircraft
The measurement of the atmospheric thermal emission is important for several reasons. Remote sensing working in the wavelength regions from λ = 3 μm to λ = 5 μm and from λ = 8 μm to λ = 14 μm, with high atmospheric transparency is hampered by absorption and thermal emission of the intervening atmosphere. Furthermore, both the global energy balance and the radiative heating loss of the outdoor surface of building envelopes crucially depend on atmospheric thermal emission |1|.
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