拉曼激光雷达测量的水汽作为地面真实的被动遥感

S. Melfi, D. Whiteman, R. Ferrare, K. Evans
{"title":"拉曼激光雷达测量的水汽作为地面真实的被动遥感","authors":"S. Melfi, D. Whiteman, R. Ferrare, K. Evans","doi":"10.1109/COMEAS.1995.472320","DOIUrl":null,"url":null,"abstract":"The WMO regularily distributes data from the upper-air balloon-sonde network made up of sites in participating countries around the world, but the quality varies significantly from country to country. Satellite observations of global water vapor hold the promise to meet the needs of the scientific community. At present passive sensors operating in the infrared and microwave are the only data source from which to derive atmospheric moisture information. A ground-based Raman lidar is an ideal sensor to obtain ground-truth data to compare with the satellite data. The Raman lidar provides vertical profiles of water vapor mixing ratio which can be used to directly compare with both the satellite derived data and aircraft versions of future satellite passive sensors. The lidar profiles can provide an important measure of atmospheric moisture variability. Knowledge of moisture variability is absolutely essential for a proper validation of passive sensors because ofthe errors associated with beam-filling. In general the measurement beam of a satellite-based IR or a microwave instrument is several 10s of kilometers at the Earth's surface. The upwelling radiation within this footprint is influenced not only by the total concentration of the species being measured but also by the distribution of that species in the instantaneous field-of-view. We must know both to perform a valid inversion. The Raman lidar developed at the Goddard Space Flight Center consists of an xenon fluoride excimer laser and a 0.75 meter telescope. The lidar in able, through the use of beamsplitters, to simultaneously measure laser scattering from aerosols, nitrogen, oxygen and water vapor. The ratio of the water vapor signal to the nitrogen signal after a small differential attenuation correction is proportional to water vapor mixing ratio. The ratio measured versus the time of flight of the laser pulse is easily converted into an altitude profile of moisture. A detailed description of the system along with data showing moisture and it's variability are given.<<ETX>>","PeriodicalId":274878,"journal":{"name":"Conference Proceedings Second Topical Symposium on Combined Optical-Microwave Earth and Atmosphere Sensing","volume":"8 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1995-04-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Raman lidar measurements of water vapor as ground-truth for passive remote sensors\",\"authors\":\"S. Melfi, D. Whiteman, R. Ferrare, K. Evans\",\"doi\":\"10.1109/COMEAS.1995.472320\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The WMO regularily distributes data from the upper-air balloon-sonde network made up of sites in participating countries around the world, but the quality varies significantly from country to country. Satellite observations of global water vapor hold the promise to meet the needs of the scientific community. At present passive sensors operating in the infrared and microwave are the only data source from which to derive atmospheric moisture information. A ground-based Raman lidar is an ideal sensor to obtain ground-truth data to compare with the satellite data. The Raman lidar provides vertical profiles of water vapor mixing ratio which can be used to directly compare with both the satellite derived data and aircraft versions of future satellite passive sensors. The lidar profiles can provide an important measure of atmospheric moisture variability. Knowledge of moisture variability is absolutely essential for a proper validation of passive sensors because ofthe errors associated with beam-filling. In general the measurement beam of a satellite-based IR or a microwave instrument is several 10s of kilometers at the Earth's surface. The upwelling radiation within this footprint is influenced not only by the total concentration of the species being measured but also by the distribution of that species in the instantaneous field-of-view. We must know both to perform a valid inversion. The Raman lidar developed at the Goddard Space Flight Center consists of an xenon fluoride excimer laser and a 0.75 meter telescope. The lidar in able, through the use of beamsplitters, to simultaneously measure laser scattering from aerosols, nitrogen, oxygen and water vapor. The ratio of the water vapor signal to the nitrogen signal after a small differential attenuation correction is proportional to water vapor mixing ratio. The ratio measured versus the time of flight of the laser pulse is easily converted into an altitude profile of moisture. A detailed description of the system along with data showing moisture and it's variability are given.<<ETX>>\",\"PeriodicalId\":274878,\"journal\":{\"name\":\"Conference Proceedings Second Topical Symposium on Combined Optical-Microwave Earth and Atmosphere Sensing\",\"volume\":\"8 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1995-04-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Conference Proceedings Second Topical Symposium on Combined Optical-Microwave Earth and Atmosphere Sensing\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/COMEAS.1995.472320\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Conference Proceedings Second Topical Symposium on Combined Optical-Microwave Earth and Atmosphere Sensing","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/COMEAS.1995.472320","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

摘要

WMO定期发布由世界各地参与国家的站点组成的高空气球探空网络的数据,但各国的质量差异很大。对全球水蒸气的卫星观测有望满足科学界的需要。目前,红外和微波被动传感器是获取大气湿度信息的唯一数据源。地基拉曼激光雷达是一种理想的获取地面真值数据并与卫星数据进行比较的传感器。拉曼激光雷达提供水汽混合比的垂直剖面,可用于直接与卫星衍生数据和未来卫星无源传感器的飞机版本进行比较。激光雷达剖面可以提供大气湿度变异性的重要测量。由于与光束填充相关的误差,湿度变化的知识对于被动传感器的正确验证是绝对必要的。一般来说,基于卫星的红外或微波仪器的测量光束在地球表面的几十公里处。该足迹内的上涌辐射不仅受到被测量物种的总浓度的影响,而且还受到该物种在瞬时视场中的分布的影响。我们必须知道两者才能进行有效的反转。戈达德太空飞行中心研制的拉曼激光雷达由一个氟化氙准分子激光器和一个0.75米的望远镜组成。该激光雷达通过使用分束器,能够同时测量气溶胶、氮、氧和水蒸气的激光散射。经过小的差分衰减校正后,水汽信号与氮信号的比值与水汽混合比成正比。测量到的与激光脉冲飞行时间的比值很容易转换成湿度的高度分布。给出了系统的详细描述以及显示湿度及其变化的数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
Raman lidar measurements of water vapor as ground-truth for passive remote sensors
The WMO regularily distributes data from the upper-air balloon-sonde network made up of sites in participating countries around the world, but the quality varies significantly from country to country. Satellite observations of global water vapor hold the promise to meet the needs of the scientific community. At present passive sensors operating in the infrared and microwave are the only data source from which to derive atmospheric moisture information. A ground-based Raman lidar is an ideal sensor to obtain ground-truth data to compare with the satellite data. The Raman lidar provides vertical profiles of water vapor mixing ratio which can be used to directly compare with both the satellite derived data and aircraft versions of future satellite passive sensors. The lidar profiles can provide an important measure of atmospheric moisture variability. Knowledge of moisture variability is absolutely essential for a proper validation of passive sensors because ofthe errors associated with beam-filling. In general the measurement beam of a satellite-based IR or a microwave instrument is several 10s of kilometers at the Earth's surface. The upwelling radiation within this footprint is influenced not only by the total concentration of the species being measured but also by the distribution of that species in the instantaneous field-of-view. We must know both to perform a valid inversion. The Raman lidar developed at the Goddard Space Flight Center consists of an xenon fluoride excimer laser and a 0.75 meter telescope. The lidar in able, through the use of beamsplitters, to simultaneously measure laser scattering from aerosols, nitrogen, oxygen and water vapor. The ratio of the water vapor signal to the nitrogen signal after a small differential attenuation correction is proportional to water vapor mixing ratio. The ratio measured versus the time of flight of the laser pulse is easily converted into an altitude profile of moisture. A detailed description of the system along with data showing moisture and it's variability are given.<>
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Moisture in a grass canopy from SSM/I radiobrightness Identification method on mathematical model of terrain profile section and experimental results by the millimeter wave altimeter X-band Doppler-radar and radiometer system Remote sensing of scattering surface if phase information in registered data is distorted or absent A preliminary design procedure to find the aperture diameter and other basic parameters of a feed able to satisfy radiometric requirements
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1