Atmospheric Turbulence and Internal Gravity Waves Examined by the Method of Artificial Periodic Irregularities

被引：15

作者：

Bakhmet'eva, N. V. ^{[1
]}

Grigoriev, G. I. ^{[1
]}

Tolmacheva, A. V. ^{[1
]}

Kalinina, E. E. ^{[1
]}

机构：

[1] Lobachevsky Nizhny Novgorod State Univ, Radiophys Res Inst, Nizhnii Novgorod 603930, Russia

来源：

RUSSIAN JOURNAL OF PHYSICAL CHEMISTRY B | 2018年 / 12卷 / 03期

关键词：

Earth's atmosphere; mesosphere; lower thermosphere; internal gravity waves; artificial periodic irregularities; turbulence; vortex structures; SASKATCHEWAN MF RADAR; LOWER IONOSPHERE; SPORADIC-E; LOWER THERMOSPHERE; MIDDLE ATMOSPHERE; TURBOPAUSE; PARAMETERS; MESOSPHERE; UNIVERSITY; FACILITY;

D O I：

10.1134/S1990793118030041

中图分类号：

O64 [物理化学（理论化学）、化学物理学]; O56 [分子物理学、原子物理学];

学科分类号：

070203 ; 070304 ; 081704 ; 1406 ;

摘要：

A method for studying the Earth's ionosphere at altitudes of the mesosphere and lower thermosphere based on creating artificial periodic irregularities in the ionospheric plasma by means of powerful radio waves is breafly described. Methods for determining the temperature and density of the neutral component and the velocity of vertical and turbulent motions by measuring the characteristics of the signal backscattered by the irregularities are described. The results of experiments performed on a SURA heating facility aimed at a comprehensive investigation of the natural processes occurring in the Earth's lower ionosphere due to the propagation of atmospheric waves and turbulent phenomena are examined. Based on measurements of the amplitude and phase of the signal scattered by periodic irregularities, the most important characteristics of the neutral and plasma components of the Earth's atmosphere at altitudes of the mesosphere and lower thermosphere are determined. Further research on the subject is discussed.

引用

页码：510 / 521

页数：12

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