Zobrazeno 1 - 10
of 43
pro vyhledávání: '"E. A. Kryuchkov"'
Publikováno v:
Annales Geophysicae, Vol 37, Pp 405-415 (2019)
The objects of research in this work are evanescent wave modes in a gravitationally stratified atmosphere and their associated pseudo-modes. Whereas the former, according to the dispersion relation, rapidly decrease with distance from a certain surfa
Externí odkaz:
https://doaj.org/article/57bfa59e4ed248fda97be05d03290cc7
Publikováno v:
Kinematika i fizika nebesnyh tel (Online). 38:17-28
Publikováno v:
Kinematics and Physics of Celestial Bodies. 38:73-82
Autor:
Yu. O. Klymenko, A. K. Fedorenko, E. I. Kryuchkov, O. K. Cheremnykh, A. D. Voitsekhovska, Yu. O. Selivanov, I. T. Zhuk
Publikováno v:
Kinematics and Physics of Celestial Bodies. 37:273-283
Publikováno v:
Annales Geophysicae, Vol 33, Pp 101-108 (2015)
The article presents a summary of the main findings of the systematic study of acoustic-gravity waves (AGWs) in the polar thermosphere. This study was based on the in situ measurements made by the Dynamics Explorer 2 (DE2) spacecraft late in its m
Externí odkaz:
https://doaj.org/article/c58d4c14f89347db9610ae078682ce95
Publikováno v:
Kinematics and Physics of Celestial Bodies. 37:221-229
The attenuation of the acoustic-gravitational nondivergent f-mode and inelastic γ-mode in the Earth’s upper atmosphere due to viscosity and thermal conductivity is studied. To analyze the attenuation, a system of hydrodynamic equations is used, in
Publikováno v:
Kinematics and Physics of Celestial Bodies. 36:253-264
A new approach to the study of acoustic-gravity waves in the Earth’s atmosphere in the presence of vertical temperature inhomogeneity is proposed. Using this approach, the local AGW dispersion equation was obtained for the atmosphere with a small v
Publikováno v:
Kinematics and Physics of Celestial Bodies. 36:265-273
The theory of acoustic gravity waves (AGW) considers free disturbances of the atmosphere within the framework of a single-frequency approach. In this case, the theory implies the existence of two separate types of waves with different natural frequen
Publikováno v:
Kinematics and Physics of Celestial Bodies. 36:212-221
Within the model of a dissipative isothermal atmosphere, the attenuation of acoustic−gravity waves (AGWs) is studied on the basis of the modified Navier−Stokes and heat-transfer equations. Besides the usually considered velocity gradient, the mod
Publikováno v:
Kinematika i fizika nebesnyh tel (Online). 36:15-30