Noctilucent cloud particle size determination based on multi-wavelength all-sky analysis

@article{Ugolnikov2016NoctilucentCP,
  title={Noctilucent cloud particle size determination based on multi-wavelength all-sky analysis},
  author={Oleg S. Ugolnikov and A. A. Galkin and Sergey Vasilyevich Pilgaev and Alexey V. Roldugin},
  journal={Planetary and Space Science},
  year={2016},
  volume={146},
  pages={10-19}
}

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References

SHOWING 1-10 OF 40 REFERENCES

On microphysical processes of noctilucent clouds (NLC): observations and modeling of mean and width of the particle size-distribution

Abstract. Noctilucent clouds (NLC) in the polar summer mesopause region have been observed in Norway (69° N, 16° E) between 1998 and 2009 by 3-color lidar technique. Assuming a mono-modal Gaussian

Noctilucent cloud polarimetry: Twilight measurements in a wide range of scattering angles

Scattering phase functions and particle sizes in noctilucent clouds

The MIDAS‐DROPPS campaign conducted in Norway in 1999 provided a comprehensive study of the high‐latitude summer mesopause region with rocket‐borne and ground‐based instrumentation. Optical

In situ measurements of the vertical structure of a noctilucent cloud

During the NLC‐93 rocket campaign at Esrange, Sweden, the vertical structure of a noctilucent cloud layer has been investigated in situ. As in earlier rocket flights, combinations of scattered light

Particle properties and water content of noctilucent clouds and their interannual variation

[1] Noctilucent clouds (NLC) have been observed by a multicolor lidar in northern Norway (69°N, 16°E). From three backscatter coefficients we calculate the parameters of a monomodal particle size

Latitudinal dependence of noctilucent cloud growth

The latitudinal variation of NLC particle sizes is studied using scattered solar radiation spectra from the OSIRIS instrument onboard the Odin satellite obtained during the austral summer period 1

Microphysical and optical properties of noctilucent clouds

Vertical variation of NLC particle sizes retrieved from Odin/OSIRIS limb scattering observations

The vertical variation of noctilucent cloud (NLC) particle sizes is derived from limb scattering observations in the UV‐B spectral range performed with the Optical Spectrograph and InfraRed Imager