1987
DOI: 10.1126/science.235.4784.37
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Laser Remote Sensing of the Atmosphere

Abstract: Laser beams can be used as long-range spectroscopic probes of the chemical composition and physical state of the atmosphere. The spectroscopic, optical, and laser requirements for atmospheric laser remote sensing are reviewed, and the sensitivity and limitations of the technique are described. A sampling of recent measurements includes the detection of urban air pollution and toxic chemicals in the atmosphere, the measurement of global circulation of volcanic ash in the upper atmosphere, and the observation of… Show more

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Cited by 85 publications
(35 citation statements)
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References 49 publications
(40 reference statements)
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“…Molecular extinction in the near UV is primarily an elastic scattering process, since the Rayleigh scattering of light by molecular nitrogen ðN 2 Þ and oxygen ðO 2 Þ dominates inelastic scattering and absorption [34]. For example, the Raman scattering cross sections of N 2 and O 2 are approximately 10 À30 cm À2 between 300 nm and 420 nm [35], much smaller than the Rayleigh scattering cross section of air ($10 À27 cm À2 ) at these wavelengths [36].…”
Section: The Optical Depth Of Moleculesmentioning
confidence: 99%
“…Molecular extinction in the near UV is primarily an elastic scattering process, since the Rayleigh scattering of light by molecular nitrogen ðN 2 Þ and oxygen ðO 2 Þ dominates inelastic scattering and absorption [34]. For example, the Raman scattering cross sections of N 2 and O 2 are approximately 10 À30 cm À2 between 300 nm and 420 nm [35], much smaller than the Rayleigh scattering cross section of air ($10 À27 cm À2 ) at these wavelengths [36].…”
Section: The Optical Depth Of Moleculesmentioning
confidence: 99%
“…Lidar has been used in optical remote sensing technique to study atmospheric particulate and gas pollutants over half of the century (Grant, 1987;Killinger and Menyuk, 1987;Killinger and Mooradian, 1983;Measures, 1984). Lidar has the ability to measure remotely atmospheric aerosols (Carswell, 1983;Fiocco and Smullin, 1963).…”
Section: Lidarmentioning
confidence: 99%
“…where P͑R͒ is the range-received power ͑W͒, ␤͑R͒ is the range-dependent volume backscatter coefficient of the atmosphere ͑m Ϫ1 sr Ϫ1 ͒, ␣͑R͒ is the rangedependent extinction coefficient ͑m Ϫ1 ͒, R is the range ͑m͒, and A is the system constant ͑W m 3 …”
Section: P͑r͒ ϭmentioning
confidence: 99%
“…Consequently, it is possible to retrieve information about the physical state of the atmosphere along the exploration beam path. [1][2][3] In particular, estimation of the atmospheric optical parameters, namely, extinction and backscatter, based on pulsed elastic-backscatter lidars ͑i.e., with no wavelength shift in reception͒ has been investigated in the literature. 4 -6 The single-scattering range-return power for an elastic-backscatter lidar system can be expressed as 2 …”
Section: Introductionmentioning
confidence: 99%