{"title":"COHMEX期间激光雷达湿度测量","authors":"S. Melfi, D. Whiteman, R. Ferrare","doi":"10.1364/lors.1987.thb4","DOIUrl":null,"url":null,"abstract":"Water vapor is one of the most important state variables of the atmosphere. Its concentration and distribution with height influences atmospheric circulation and dynamics, and figures prominently in a number of atmospheric processes including: 1) atmospheric stability, 2) cloud formation, 3) radiative transfer, 4) storm development, to mention only a few.","PeriodicalId":339230,"journal":{"name":"Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques","volume":"27 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Lidar Moisture Measurements During COHMEX\",\"authors\":\"S. Melfi, D. Whiteman, R. Ferrare\",\"doi\":\"10.1364/lors.1987.thb4\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Water vapor is one of the most important state variables of the atmosphere. Its concentration and distribution with height influences atmospheric circulation and dynamics, and figures prominently in a number of atmospheric processes including: 1) atmospheric stability, 2) cloud formation, 3) radiative transfer, 4) storm development, to mention only a few.\",\"PeriodicalId\":339230,\"journal\":{\"name\":\"Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques\",\"volume\":\"27 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 Laser and Optical Remote Sensing: Instrumentation and Techniques\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1364/lors.1987.thb4\",\"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.thb4","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Water vapor is one of the most important state variables of the atmosphere. Its concentration and distribution with height influences atmospheric circulation and dynamics, and figures prominently in a number of atmospheric processes including: 1) atmospheric stability, 2) cloud formation, 3) radiative transfer, 4) storm development, to mention only a few.