Optical Remote Sensing of the Atmosphere最新文献_第8页

Performance Calculations and Test of SCIAMACHY Detector Modules SCIAMACHY探测器模块的性能计算与测试

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1993.fa.2

A. Goede, R. Hoogeveen, R. van der A, J. de Vries

引用次数: 1

Derivation of CLAES Filter Shapes CLAES滤波器形状的推导

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1993.the.11

J. Mergenthaler, J. Potter, J. Kumer, T. C. James, A. Roche

{"title":"Derivation of CLAES Filter Shapes","authors":"J. Mergenthaler, J. Potter, J. Kumer, T. C. James, A. Roche","doi":"10.1364/orsa.1993.the.11","DOIUrl":"https://doi.org/10.1364/orsa.1993.the.11","url":null,"abstract":"The Cryogenic Limb Array Etalon Spectrometer, CLAES, was launched on September 12, 1991 aboard the NASA Upper Atmosphere Research Satellite (UARS) and has been acquiring data on stratospheric composition since October 1, 1991. Overviews of the CLAES experiment and hardware are given by Roche et al (1) and Burriesci et al. (2). In the OSA Topical Meeting on Optical Remote Sensing of the Atmosphere in 1990 we presented three papers, (3,4,5) that described our progress up to that time in defining the system spectral transmission. In this paper, we describe refinements to CLAES characterization since then. These have come from further work with the pre-launch cold test data and from on-flight data. The spectral transmission characterization described here is currently being used in CLAES retrieval software. Figure (1) shows a schematic diagram of the spectrometer. In normal operation the CLAES instrument achieves a 0.2-0.65 cm-1 spectral resolution by passing the radiation through one of nine passband blocking filters (FWHM ~10 cm-1) mounted in a filter wheel, and one of four Fabry-Perot etalons which are mounted in a paddle wheel to provide for spectral scanning by tilting. The transmitted radiation then falls on a focal plane array consisting of a main array of 20 elements and an HCI array of 3 elements. The main detector array is used by eight spectral channels from 5.3 to 12.8 μm and takes atmospheric data in 20-2.5 km vertical increments. The 3-element HCL array is used only by the 3.5 μm channel where each detector spans approximately 16 km for S/N augmentation.","PeriodicalId":320202,"journal":{"name":"Optical Remote Sensing of the Atmosphere","volume":"10 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114852921","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Raman/Rayleigh lidar measurements during a major stratwarm in Greenland 格陵兰岛主要层温期间的拉曼/瑞利激光雷达测量

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1991.otua4

R. Farley, J. Meriwether, R. McNutt, P. Dao, W. Moskowitz, G. Davidson, I. Mikkelsen, M. Larsen

{"title":"Raman/Rayleigh lidar measurements during a major stratwarm in Greenland","authors":"R. Farley, J. Meriwether, R. McNutt, P. Dao, W. Moskowitz, G. Davidson, I. Mikkelsen, M. Larsen","doi":"10.1364/orsa.1991.otua4","DOIUrl":"https://doi.org/10.1364/orsa.1991.otua4","url":null,"abstract":"Rayleigh lidar observations of atmospheric temperatures below 30 km are contaminated by the Mie backscattering from the sulphate stratospheric aerosols that normally exist between 12 and 25 km. Consequently, the fact that nitrogen Raman lidar returns for vibrational and rotational Raman backscattering are red-shifted offers the opportunity to extend the Rayleigh lidar measurements to lower altitudes by joining the two relative density profiles at a height where the Mie backscattering contamination may be ignored. This technique was applied by us previously with the aim of providing an improved means of normalizing lidar measurements of upper atmosphere densities against simultaneous balloon measurements. Because lower stratosphere temperatures below 195 °K will support the production of polar stratospheric clouds (PSC) designated as Type 2 nitric acid trihydrate (NAT) and for temperatures below the frost point, nominally 190 °K, the production of Type 1 water ice PSCs. To study the possible formation and evolution of these polar stratospheric clouds, we undertook to make measurements of temperatures in the winter Arctic with a Raman augmentation of our mobile Rayleigh lidar facility. While the results did not show any indications of the production of PSCs, the profiles did show substantial dynamic activity in connection with the progression of a major stratospheric warming.","PeriodicalId":320202,"journal":{"name":"Optical Remote Sensing of the Atmosphere","volume":"38 2 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124268078","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

A compact CO2-lidar system for the detection of atmospheric pollutants 用于探测大气污染物的紧凑型二氧化碳激光雷达系统

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1995.tuc18

T. Stuffler, H. W. Schrötter

引用次数: 0

Development of an All-Solid-State Raman Laser for Ozone DIAL Measurements 用于臭氧DIAL测量的全固态拉曼激光器的研制

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1997.owc.14

C. L. McCray, T. Chyba

引用次数: 0

NDSC Infrared Observations at Mauna Loa, Hawaii 夏威夷莫纳罗亚的NDSC红外观测

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1993.thc.4

F. Murcray, D. Murcray, S. David, R. Blatherwick, J. Kosters, F. Murcray, A. Goldman, C. Rinsland

引用次数: 0

A Combined Lidar, Long-path Extinction and In-situ Aerosol Experiment in Southern Ontario 安大略省南部激光雷达、长径消光和原位气溶胶联合实验

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1993.tub.1

R. Hoff

引用次数: 0

Trace Gas Remote Sounding with the High Resolution Dynamics Limb Sounder (HERDLS) 利用高分辨率动态边缘测深仪(HERDLS)远程探测微量气体

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1997.otha.1

J. Gille

引用次数: 0

Microwave observations of precipitable water 可降水量的微波观测

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1990.wd10

S. Tjemkes, G. Stephens

引用次数: 0

Recent Profiles of Atmospheric Backscatter 大气后向散射的最新概况

Optical Remote Sensing of the Atmosphere Pub Date : 1900-01-01 DOI: 10.1364/orsa.1990.tud11

M. Post, A. Weickmann, G. Mcnice

{"title":"Recent Profiles of Atmospheric Backscatter","authors":"M. Post, A. Weickmann, G. Mcnice","doi":"10.1364/orsa.1990.tud11","DOIUrl":"https://doi.org/10.1364/orsa.1990.tud11","url":null,"abstract":"The prevalence of atmospheric aerosols on a global basis has recently become a topic of great importance for climatologists and for researchers attempting to establish the feasibility of satellite-based measuring systems that use aerosols as tracers, as well as for those attempting to explain the interfering effects of aerosols on their measurements. In 1981 we began acquiring a large set of backscatter profiles with our 10.6 μm wavelength pulsed, coherent lidar near Boulder, Colorado. By 1984 more than 600 profiles were archived and analyzed, and several papers1-2 summarized the findings. Between 1985 and 1988 a void occurred in our data taking because we upgraded the transceiver from a lower powered hybrid design3 to a higher powered injection-seeded design4, and because of a change in our program objectives. Fortunately during this period the Jet Propulsion Laboratory began taking similar data5. In 1987 we renewed our systematic observations at the behest of NASA for its Laser Atmospheric Wind System (LAWS) studies6, and in the fall of 1988 we traveled to the Mauna Loa volcano in Hawaii to study the clean Pacific troposphere, in conjunction with the Global Backscatter Experiment (GLOBE7) program. Concurrently, our group operated a pulsed ruby lidar8 to acquire biweekly profiles of backscatter in the troposphere and stratosphere over Boulder. Recently we coordinated data taking between the two lidar systems, and we combined our observations on one occasion with observations from the University of Wyoming’s balloon backscatter instrument9.","PeriodicalId":320202,"journal":{"name":"Optical Remote Sensing of the Atmosphere","volume":"39 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132352921","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0