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@article{79ece4ca074d404ca7c5357caaf583e8,
title = "Influence of solar activity on penetration of traveling planetary-scale waves from the troposphere into the thermosphere",
abstract = "In this study, numerical simulations of planetary-scale waves (PSWs), generated in the troposphere, were performed for altitudes from the Earth's surface up to 300 km. The influence of thermospheric effects of solar activity (SA) on the amplitudes and phases of westward traveling PSWs with zonal wave numbers 1 and 2 and periods 4–16 days propagating from the troposphere was simulated. Such simulations for a large number of PSW modes in the thermosphere were made for the first time. The effects of SA changes at altitudes above 100 km were involved in the general circulation model MUAM. The ionospheric conductivities for minimum and maximum SA levels were included into the MUAM. The simulation results were averaged over two ensembles of model runs with different PSW phases for conditions corresponding to the high and low SA levels for January–February. PSW atmospheric refractivity index and Eliassen-Palm flux were calculated. They correspond to simulated changes in PSW amplitudes. Changes in the zonal velocity and temperature caused by the SA variations can modify spatial distributions of the westward traveling PSWs. Wave amplitudes significantly (up to 100%) decrease at the thermospheric heights under high SA, which is accompanied by decreasing vertical component of the Eliassen-Palm flux. The 7-, 10-, and 16-day PSWs could have larger partial reflection and worse propagation conditions than the 4- and 5-day waves in the Southern Hemisphere under the high SA. At altitudes below 100 km, minor differences in zonal velocity and PSW amplitudes between high and low SA are found.",
keywords = "atmospheric dynamics, general circulation, modeling, planetary waves, solar activity, MESOSPHERE, CIRCULATION, MIDDLE ATMOSPHERE, TIDAL EQUATIONS, MODEL, VARIABILITY, NORTHERN-HEMISPHERE, GRAVITY-WAVE, IONOSPHERE SYSTEM, PROPAGATION",
author = "Коваль, {Андрей Владиславович} and Гаврилов, {Николай Михайлович} and Погорельцев, {Александр Иванович} and Шевчук, {Никита Олегович}",
note = "Koval, A. V., Gavrilov, N. M., Pogoreltsev, A. I., & Shevchuk, N. O. (2018). Influence of solar activity on penetration of traveling planetary-scale waves from the troposphere into the thermosphere. Journal of Geophysical Research: Space Physics, 123. (8), 6888-6903, doi: 10.1029/2018JA025680",
year = "2018",
month = aug,
doi = "10.1029/2018JA025680",
language = "English",
volume = "123",
pages = "6888--6903",
journal = "Journal of Geophysical Research: Biogeosciences",
issn = "0148-0227",
publisher = "American Geophysical Union",
number = "8",

}

RIS

TY - JOUR

T1 - Influence of solar activity on penetration of traveling planetary-scale waves from the troposphere into the thermosphere

AU - Коваль, Андрей Владиславович

AU - Гаврилов, Николай Михайлович

AU - Погорельцев, Александр Иванович

AU - Шевчук, Никита Олегович

N1 - Koval, A. V., Gavrilov, N. M., Pogoreltsev, A. I., & Shevchuk, N. O. (2018). Influence of solar activity on penetration of traveling planetary-scale waves from the troposphere into the thermosphere. Journal of Geophysical Research: Space Physics, 123. (8), 6888-6903, doi: 10.1029/2018JA025680

PY - 2018/8

Y1 - 2018/8

N2 - In this study, numerical simulations of planetary-scale waves (PSWs), generated in the troposphere, were performed for altitudes from the Earth's surface up to 300 km. The influence of thermospheric effects of solar activity (SA) on the amplitudes and phases of westward traveling PSWs with zonal wave numbers 1 and 2 and periods 4–16 days propagating from the troposphere was simulated. Such simulations for a large number of PSW modes in the thermosphere were made for the first time. The effects of SA changes at altitudes above 100 km were involved in the general circulation model MUAM. The ionospheric conductivities for minimum and maximum SA levels were included into the MUAM. The simulation results were averaged over two ensembles of model runs with different PSW phases for conditions corresponding to the high and low SA levels for January–February. PSW atmospheric refractivity index and Eliassen-Palm flux were calculated. They correspond to simulated changes in PSW amplitudes. Changes in the zonal velocity and temperature caused by the SA variations can modify spatial distributions of the westward traveling PSWs. Wave amplitudes significantly (up to 100%) decrease at the thermospheric heights under high SA, which is accompanied by decreasing vertical component of the Eliassen-Palm flux. The 7-, 10-, and 16-day PSWs could have larger partial reflection and worse propagation conditions than the 4- and 5-day waves in the Southern Hemisphere under the high SA. At altitudes below 100 km, minor differences in zonal velocity and PSW amplitudes between high and low SA are found.

AB - In this study, numerical simulations of planetary-scale waves (PSWs), generated in the troposphere, were performed for altitudes from the Earth's surface up to 300 km. The influence of thermospheric effects of solar activity (SA) on the amplitudes and phases of westward traveling PSWs with zonal wave numbers 1 and 2 and periods 4–16 days propagating from the troposphere was simulated. Such simulations for a large number of PSW modes in the thermosphere were made for the first time. The effects of SA changes at altitudes above 100 km were involved in the general circulation model MUAM. The ionospheric conductivities for minimum and maximum SA levels were included into the MUAM. The simulation results were averaged over two ensembles of model runs with different PSW phases for conditions corresponding to the high and low SA levels for January–February. PSW atmospheric refractivity index and Eliassen-Palm flux were calculated. They correspond to simulated changes in PSW amplitudes. Changes in the zonal velocity and temperature caused by the SA variations can modify spatial distributions of the westward traveling PSWs. Wave amplitudes significantly (up to 100%) decrease at the thermospheric heights under high SA, which is accompanied by decreasing vertical component of the Eliassen-Palm flux. The 7-, 10-, and 16-day PSWs could have larger partial reflection and worse propagation conditions than the 4- and 5-day waves in the Southern Hemisphere under the high SA. At altitudes below 100 km, minor differences in zonal velocity and PSW amplitudes between high and low SA are found.

KW - atmospheric dynamics

KW - general circulation

KW - modeling

KW - planetary waves

KW - solar activity

KW - MESOSPHERE

KW - CIRCULATION

KW - MIDDLE ATMOSPHERE

KW - TIDAL EQUATIONS

KW - MODEL

KW - VARIABILITY

KW - NORTHERN-HEMISPHERE

KW - GRAVITY-WAVE

KW - IONOSPHERE SYSTEM

KW - PROPAGATION

UR - http://www.scopus.com/inward/record.url?scp=85052450435&partnerID=8YFLogxK

U2 - 10.1029/2018JA025680

DO - 10.1029/2018JA025680

M3 - Article

VL - 123

SP - 6888

EP - 6903

JO - Journal of Geophysical Research: Biogeosciences

JF - Journal of Geophysical Research: Biogeosciences

SN - 0148-0227

IS - 8

ER -

ID: 36336796