2015
DOI: 10.5194/acp-15-2521-2015
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A new method for measuring the imaginary part of the atmospheric refractive index structure parameter in the urban surface layer

Abstract: Abstract. The atmospheric refractive index consists of both real and imaginary parts. The intensity of refractive index fluctuations is generally expressed as the refractive index structure parameter, with the real part reflecting the strength of atmospheric turbulence and the imaginary part reflecting absorption in the light path. A large aperture scintillometer (LAS) is often used to measure the structure parameter of the real part of the atmospheric refractive index, from which the sensible and latent heat … Show more

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Cited by 10 publications
(24 citation statements)
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“…The contribution of the real part of the AERI corresponds to the high frequencies, whereas the contribution of the imaginary part of the AERI corresponds to the low frequencies, suggesting that the variances resulting from the real and imaginary parts are independent. Therefore, the light intensity variances induced by the real and imaginary parts can be detected separately at high frequencies and low frequencies from the LAS measurements (Yuan et al, 2015). The real part of the AERISP (C 2 n, Re ) can be calculated from the variance of the high-frequency part, and the imaginary part of the AERISP (C 2 n, Im ) can be calculated from the variance of the low-frequency part.…”
Section: R M Yuan Et Al: a New Methods For Estimating Aerosol Mass mentioning
confidence: 99%
See 4 more Smart Citations
“…The contribution of the real part of the AERI corresponds to the high frequencies, whereas the contribution of the imaginary part of the AERI corresponds to the low frequencies, suggesting that the variances resulting from the real and imaginary parts are independent. Therefore, the light intensity variances induced by the real and imaginary parts can be detected separately at high frequencies and low frequencies from the LAS measurements (Yuan et al, 2015). The real part of the AERISP (C 2 n, Re ) can be calculated from the variance of the high-frequency part, and the imaginary part of the AERISP (C 2 n, Im ) can be calculated from the variance of the low-frequency part.…”
Section: R M Yuan Et Al: a New Methods For Estimating Aerosol Mass mentioning
confidence: 99%
“…C 2 n, Re and C 2 n, Im can be measured by a specially made LAS (Yuan et al, 2015). After a spherical wave propagates over a distance in a turbulent atmosphere, the light intensity on the receiving end will fluctuate.…”
Section: R M Yuan Et Al: a New Methods For Estimating Aerosol Mass mentioning
confidence: 99%
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