Software for experimental studies of the atmospheric turbulence structure; Proceedings of SPIE; Vol. 11560 : Atmospheric and Ocean Optics: Atmospheric Physics

Dades bibliogràfiques
Parent link:Proceedings of SPIE.— .— Bellingham: SPIE
Vol. 11560 : Atmospheric and Ocean Optics: Atmospheric Physics.— 2020.— 115608Z, 5 p.
Altres autors: Bogushevich A. Ya., Sherstnev V. S. Vladislav Stanislavovich, Sherstneva A. I. Anna Igorevna, Botygin I. A. Igor Aleksandrovich
Sumari:Title screen
The results of mathematical and software development for experimental studies of the surface atmospheric turbulence structure are presented. High-frequency measurements of ultrasonic thermoanemometer are used as data. Data processing and calculation of atmospheric turbulence parameters were carried out according to the schemes of sampling and scaling of meteorological parameters under study using semi-empirical methods of describing heat, moisture, amount of motion in the surface layer and Monin-Obukhov's theory of similarity. The calculated prognostic values of parameters are sufficient to estimate the dynamic regime of turbulence in the surface layer of the atmosphere, including estimates of the possibility of temperature inversion formation in the atmosphere and determination of the stability class of atmospheric stratification
Текстовый файл
AM_Agreement
Idioma:anglès
Publicat: 2020
Matèries:
Accés en línia:https://doi.org/10.1117/12.2576027
Статья на русском языке
Format: Electrònic Capítol de llibre
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=679985

MARC

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330 |a The results of mathematical and software development for experimental studies of the surface atmospheric turbulence structure are presented. High-frequency measurements of ultrasonic thermoanemometer are used as data. Data processing and calculation of atmospheric turbulence parameters were carried out according to the schemes of sampling and scaling of meteorological parameters under study using semi-empirical methods of describing heat, moisture, amount of motion in the surface layer and Monin-Obukhov's theory of similarity. The calculated prognostic values of parameters are sufficient to estimate the dynamic regime of turbulence in the surface layer of the atmosphere, including estimates of the possibility of temperature inversion formation in the atmosphere and determination of the stability class of atmospheric stratification 
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610 1 |a small-scale turbulence 
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701 1 |a Sherstnev  |b V. S.  |c specialist in the field of Informatics and computer engineering  |c associate Professor of Tomsk Polytechnic University, candidate of technical Sciences  |f 1974-  |g Vladislav Stanislavovich  |9 17137 
701 1 |a Sherstneva  |b A. I.  |c mathematician  |c associate Professor of Tomsk Polytechnic University, candidate of physico-mathematical Sciences  |f 1974-  |g Anna Igorevna  |9 18721 
701 1 |a Botygin  |b I. A.  |c specialist in the field of Informatics and computer engineering  |c Associate Professor of Tomsk Polytechnic University, candidate of technical sciences  |f 1947-  |g Igor Aleksandrovich  |9 17356 
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