1 edition of User"s guide for the solar backscattered ultraviolet (SBUV) and the total ozone mapping spectrometer (TOMS) RUT-S and RUT-T data sets found in the catalog.
User"s guide for the solar backscattered ultraviolet (SBUV) and the total ozone mapping spectrometer (TOMS) RUT-S and RUT-T data sets
by National Aeronautics and Space Administration, Scientific and Technical Information Branch, For sale by the National Technical Information Service] in Washington, D.C, [Springfield, Va
Written in English
|Statement||A.J. Fleig ... [et al.].|
|Series||NASA reference publication -- 1112.|
|Contributions||Flieg, A. J., United States. National Aeronautics and Space Administration. Scientific and Technical Information Branch., Goddard Space Flight Center.|
|The Physical Object|
|Pagination||1 v. (various pagings) :|
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Get this from a library. User's guide for the solar backscattered ultraviolet (SBUV) and the total ozone mapping spectrometer (TOMS) RUT-S and RUT-T data sets: Octo to November 1, [A J Fleig; United States.
National Aeronautics and Space Administration. Scientific and Technical Information Branch.; Goddard Space Flight Center.;]. User's guide for the Solar Backscattered Ultraviolet (SBUV) instrument first-year ozone-S data set.
Washington, D.C.: National Aeronautics and Space Administration, Scientific and Technical Information Service], (OCoLC) Material Type: Government publication, National government publication: Document Type: Book: OCLC Number. NOAA Polar-orbiting Operational Environmental Satellites (POES) Radiometer Data Landing Page Dataset landing page with general information and access links for the dataset.
Associated Resources: NOAA Polar Orbiter Data User's Guide, SectionAVHRR Level 1b Data Base. NOAA Polar Orbiter Data User's Guide, SectionAVHRR Level 1b Data Base. The time line of historic, present and future space-borne instruments measuring ultraviolet and visible backscattered solar radiation designed to quantify atmospheric trace gases is presented.
We describe the instruments technological evolution and the basic concepts of retrieval by: 3. Since the first satellite ozone measurements inbasically three methods have been developed: backscattered solar ultraviolet, infrared emission, and occultation. In a review article by Krueger et al.
(, Phil. Trans. Soc. Lond.A, ), the authors examine the above satellite methods and data covering the period up to about Cited by: Richter A., Wagner T.
() The Use of UV, Visible and Near IR Solar Back Scattered Radiation to Determine Trace Gases. In: Burrows J., Borrell P., Platt U. (eds) The Remote Sensing of Tropospheric Composition from Space.
Physics of Earth and Space Environments. Springer, Berlin, Heidelberg. First Online 22 September Cited by: Sensitivity of UV Erythemally Effective Irradiance and Daily Dose to Spatial Variability in Total Ozone Article in Photochemistry and Photobiology 84(5) February with 60 Reads.
Kidwell KB () NOAA polar orbiter data users guide. National Oceanic and Atmospheric Administration/National Environmental Satellite Data and Information Service Washington DC Google Scholar Kiehl JT, Hack JJ, Zhang MH, Cess RD () Sensitivity of a GCM to enhanced shortwave cloud by: The solar backscattered ultraviolet (SBUV) and the Total Ozone Mapping Spectrometer (TOMS) instruments were first flown on Nimbus 7.
TOMS, by scanning from side to side, provided maps with complete global coverage of the total column amounts of ozone.
The effects of horizontally extended clouds on backscattered ultraviolet sunlight, "J Geophys Res,"(). Wengraitis S., Benedetta D., Sliney D.H., Intercomparison of effective erythemal irradiance measurements from two types of broad-band instruments during June"Photochem Photobiol," 68(2) ().
Search the leading research in optics and photonics applied research from SPIE journals, conference proceedings and presentations, and eBooks. FOA Reference Guide To Fiber Optic Testing Answers to Chapter Questions The purpose of this book is to provide a reference guide to those involved with the testing of fiber optic cable plants and networks or those teaching the personnel who will do this work.
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[The Day 1 solar spectra are a set of spectra used in the algorithm to compute the radiance/irradiance ratios. The algorithm/processing initially used a set of pre‐launch estimates for these and then after real solar measurements were taken new estimates were made (system updates in June for the OMPS NM and July for the OMPS NP).Cited by: Lidar (/ ˈ l aɪ d ɑːr /, also LIDAR, LiDAR, and LADAR) is a method for measuring distances by illuminating the target with laser light and measuring the reflection with a sensor.
Differences in laser return times and wavelengths can then be used to make digital 3-D representations of the target.
It has terrestrial, airborne, and mobile applications. The Solar Backscatter Ultraviolet Spectral Radiometer (SBUV/2) was designed for a two-year NOAA-9 ( words) [view diff] exact match in snippet view article find links to article Sounding Unit Search and Rescue Satellite-Aided Tracking System Solar Backscatter Ultraviolet Stratospheric Sounding Unit SEM/Medium energy proton detector.
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The book helps newcomers to obtain a quick start into the practical value and benefits of multi-sensor image fusion. Experts will find this book useful to obtain an overview on the state of the art and. In extreme cases cloud cover can decrease UV irradiance by over 90%.
Estimates of the average reduction of UVB due to clouds (relative to cloudless skies) based on satellite measurements of backscattered solar UV are 30% at 60 degrees latitude, 10%. NASA Images Solar System Collection Ames Research Center Brooklyn Museum Full text of " [ Keith Lovegrove, Wes Stein] Concentrating Solar P(Book ) ".
You can write a book review and share your experiences. Other readers will always be interested in your opinion of the books you've read. Whether you've loved the book or not, if you give your honest and detailed thoughts then people will find new books that are right for them., Free ebooks since Lidar 1 Lidar A FASOR used at the Starfire Optical Range for lidar and laser guide star experiments is tuned to the sodium D2a line and used to excite sodium atoms in the upper atmosphere.
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