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Cloud droplet size distribution reconstruction by the phase function. / Kablukova, Evgeniya G.; Prigarin, Sergei M.; Zabinyako, Gerard I.

24th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics. ed. / Oleg A. Romanovskii; Gennadii G. Matvienko. SPIE-INT SOC OPTICAL ENGINEERING, 2018. 1083325 (Proceedings of SPIE - The International Society for Optical Engineering; Vol. 10833).

Research output: Chapter in Book/Report/Conference proceedingConference contributionResearchpeer-review

Harvard

Kablukova, EG, Prigarin, SM & Zabinyako, GI 2018, Cloud droplet size distribution reconstruction by the phase function. in OA Romanovskii & GG Matvienko (eds), 24th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics., 1083325, Proceedings of SPIE - The International Society for Optical Engineering, vol. 10833, SPIE-INT SOC OPTICAL ENGINEERING, 24th International Symposium on Atmospheric and Ocean Optics - Atmospheric Physics, Tomsk, Russian Federation, 02.07.2018. https://doi.org/10.1117/12.2504467

APA

Kablukova, E. G., Prigarin, S. M., & Zabinyako, G. I. (2018). Cloud droplet size distribution reconstruction by the phase function. In O. A. Romanovskii, & G. G. Matvienko (Eds.), 24th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics [1083325] (Proceedings of SPIE - The International Society for Optical Engineering; Vol. 10833). SPIE-INT SOC OPTICAL ENGINEERING. https://doi.org/10.1117/12.2504467

Vancouver

Kablukova EG, Prigarin SM, Zabinyako GI. Cloud droplet size distribution reconstruction by the phase function. In Romanovskii OA, Matvienko GG, editors, 24th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics. SPIE-INT SOC OPTICAL ENGINEERING. 2018. 1083325. (Proceedings of SPIE - The International Society for Optical Engineering). doi: 10.1117/12.2504467

Author

Kablukova, Evgeniya G. ; Prigarin, Sergei M. ; Zabinyako, Gerard I. / Cloud droplet size distribution reconstruction by the phase function. 24th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics. editor / Oleg A. Romanovskii ; Gennadii G. Matvienko. SPIE-INT SOC OPTICAL ENGINEERING, 2018. (Proceedings of SPIE - The International Society for Optical Engineering).

BibTeX

@inproceedings{d99ca93f7cc843cba799a47a6201f9b0,
title = "Cloud droplet size distribution reconstruction by the phase function",
abstract = "This paper deals with an ill-posed problem to determine a size distribution for water drops in a cloud from a given scattering phase function. Numerical experiments show that a numerical method based on non-negative least squares with additional requirements of smoothness can be used to solve the ill-posed problem.",
keywords = "ill-posed problem, numerical method, scattering phase function, water drop clouds in the atmosphere, size distribution of water droplets",
author = "Kablukova, {Evgeniya G.} and Prigarin, {Sergei M.} and Zabinyako, {Gerard I.}",
year = "2018",
month = jan,
day = "1",
doi = "10.1117/12.2504467",
language = "English",
series = "Proceedings of SPIE - The International Society for Optical Engineering",
publisher = "SPIE-INT SOC OPTICAL ENGINEERING",
editor = "Romanovskii, {Oleg A.} and Matvienko, {Gennadii G.}",
booktitle = "24th International Symposium on Atmospheric and Ocean Optics",
note = "24th International Symposium on Atmospheric and Ocean Optics - Atmospheric Physics ; Conference date: 02-07-2018 Through 05-07-2018",

}

RIS

TY - GEN

T1 - Cloud droplet size distribution reconstruction by the phase function

AU - Kablukova, Evgeniya G.

AU - Prigarin, Sergei M.

AU - Zabinyako, Gerard I.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - This paper deals with an ill-posed problem to determine a size distribution for water drops in a cloud from a given scattering phase function. Numerical experiments show that a numerical method based on non-negative least squares with additional requirements of smoothness can be used to solve the ill-posed problem.

AB - This paper deals with an ill-posed problem to determine a size distribution for water drops in a cloud from a given scattering phase function. Numerical experiments show that a numerical method based on non-negative least squares with additional requirements of smoothness can be used to solve the ill-posed problem.

KW - ill-posed problem

KW - numerical method

KW - scattering phase function

KW - water drop clouds in the atmosphere

KW - size distribution of water droplets

UR - http://www.scopus.com/inward/record.url?scp=85061101508&partnerID=8YFLogxK

U2 - 10.1117/12.2504467

DO - 10.1117/12.2504467

M3 - Conference contribution

T3 - Proceedings of SPIE - The International Society for Optical Engineering

BT - 24th International Symposium on Atmospheric and Ocean Optics

A2 - Romanovskii, Oleg A.

A2 - Matvienko, Gennadii G.

PB - SPIE-INT SOC OPTICAL ENGINEERING

T2 - 24th International Symposium on Atmospheric and Ocean Optics - Atmospheric Physics

Y2 - 2 July 2018 through 5 July 2018

ER -

ID: 18648388