{"title":"卫星红外辐射差和透射率","authors":"A. Neuendorffer","doi":"10.1364/sam.1980.wp1","DOIUrl":null,"url":null,"abstract":"The TIROS High Resolution Sounder1 (HIRS), like previous atmospheric sounders, relys heavily upon CO2 v2 15 micron R branch (675–715 cm−1) absorption and adjacent CO2 (v1 – v2) \"hot\" band absorption (at 721 cm−1 and 742 cm−1) for tire purpose of obtaining atmospheric temperature retrievals.2 Although this region is somewhat complicated by a weak 710 cm−1 ozone band, it is near the Planck function peak and (unlike the P branch) is relatively unaffected by water and CO2 heavy isotope absorption.","PeriodicalId":199214,"journal":{"name":"Topical Meeting on Spectroscopy in Support of Atmospheric Measurements","volume":"8 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Satellite IR Radiance Deficits and Transmittances\",\"authors\":\"A. Neuendorffer\",\"doi\":\"10.1364/sam.1980.wp1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The TIROS High Resolution Sounder1 (HIRS), like previous atmospheric sounders, relys heavily upon CO2 v2 15 micron R branch (675–715 cm−1) absorption and adjacent CO2 (v1 – v2) \\\"hot\\\" band absorption (at 721 cm−1 and 742 cm−1) for tire purpose of obtaining atmospheric temperature retrievals.2 Although this region is somewhat complicated by a weak 710 cm−1 ozone band, it is near the Planck function peak and (unlike the P branch) is relatively unaffected by water and CO2 heavy isotope absorption.\",\"PeriodicalId\":199214,\"journal\":{\"name\":\"Topical Meeting on Spectroscopy in Support of Atmospheric Measurements\",\"volume\":\"8 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Topical Meeting on Spectroscopy in Support of Atmospheric Measurements\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1364/sam.1980.wp1\",\"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 Spectroscopy in Support of Atmospheric Measurements","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1364/sam.1980.wp1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The TIROS High Resolution Sounder1 (HIRS), like previous atmospheric sounders, relys heavily upon CO2 v2 15 micron R branch (675–715 cm−1) absorption and adjacent CO2 (v1 – v2) "hot" band absorption (at 721 cm−1 and 742 cm−1) for tire purpose of obtaining atmospheric temperature retrievals.2 Although this region is somewhat complicated by a weak 710 cm−1 ozone band, it is near the Planck function peak and (unlike the P branch) is relatively unaffected by water and CO2 heavy isotope absorption.