1998
DOI: 10.1175/1520-0426(1998)015<0174:sisfat>2.0.co;2
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Shortwave Infrared Spectroradiometer for Atmospheric Transmittance Measurements

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Cited by 7 publications
(8 citation statements)
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“…Short‐wave infrared (SWIR) typically refers to the photons in the wavelength range from 1 to 3 micrometers. Applications in this wavelength window exploit various advantages such as long penetration length in biological tissue, spectral coverage of the atmospheric nightglow, and the characteristic excitation energy of certain molecular vibration modes . SWIR photodetectors are thus the key technological components to achieve optical communication, environmental gas sensing, biodiagnostics, and passive night vision .…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…Short‐wave infrared (SWIR) typically refers to the photons in the wavelength range from 1 to 3 micrometers. Applications in this wavelength window exploit various advantages such as long penetration length in biological tissue, spectral coverage of the atmospheric nightglow, and the characteristic excitation energy of certain molecular vibration modes . SWIR photodetectors are thus the key technological components to achieve optical communication, environmental gas sensing, biodiagnostics, and passive night vision .…”
Section: Introductionmentioning
confidence: 99%
“…Applications in this wavelength window exploit various advantages such as long penetration length in biological tissue, spectral coverage of the atmospheric nightglow, and the characteristic excitation energy of certain molecular vibration modes. [1][2][3] SWIR photodetectors are thus the key technological components to achieve optical communication, environmental gas sensing, biodiagnostics, and passive night vision. [4] Current SWIR technologies mainly rely on low-bandgap compound semiconductors, such as InGaAs, InSb, PbS, and HgCdTe.…”
Section: Introductionmentioning
confidence: 99%
“…The method is generally applied to a monochromatic radiance signal, the change of which is modeled following the Beer-Bouguer-Lambert law. 22 The most important assumption is that the atmosphere does not change with time, and it is common practice to perform these measurements from sunrise to sunset and obtain a large variation in air mass values. Note that extension of the measurements to low Sun altitudes requires careful modeling of the observed radiance, which can no longer be accounted for by considering a plane-parallel atmosphere.…”
Section: B Radiometric Calibrationmentioning
confidence: 99%
“…A high altitude calibration site at which these measurements can be performed helps to mitigate the possible inaccuracy of radiance theoretical modeling and the effects of atmospheric turbulence. 22 Application of this kind of calibration procedure to our instrument requires knowledge of a reliable theoretical signal model that describes the evolution of monochromatic irradiance during the day as a function of the Sun's position ͑relative air mass in the direct light path͒. The free parameters of the model are then assessed with a fitting algorithm by use of experimental data.…”
Section: B Radiometric Calibrationmentioning
confidence: 99%
“…Irradiance measurements of higher spectral resolution are mostly restricted to ground-based instruments (Harrison et al, 1999;Meywerk and Ramanathan, 1999;Michalsky et al, 1999;Wendisch et al, 2001) and to the ultraviolet or near-infrared spectral range (e.g. Ramaswamy and Freidenreich, 1998;Sicard et al, 1998). Spectral actinic irradiances, which are related to the surface of a unit sphere instead of a horizontal unit area like in the case of common irradiances, are also mostly measured at the ground (Hofzumahaus et al, 1999).…”
Section: Introductionmentioning
confidence: 99%