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NmF2 Variability at Different Longitudes in Mid-Latitudes: The Role of Geomagnetic Activity

Geomagnetism and Aeronomy, 2024-06, Vol.64 (3), p.360-368

2024

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Seasonal Features of the NmF2 Variability for Different Longitudes of the Middle Latitudes during Enhanced Geomagnetic Activity

Geomagnetism and Aeronomy, 2024-08, Vol.64 (4), p.512-520

2024

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Properties of the Variability of the Maximum Density of the F 2-Layer over Almaty at Different Levels of Solar and Geomagnetic Activity

Geomagnetism and Aeronomy, 2023-09, Vol.63 (5), p.595-601

2023

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The Relationship of the IG and T Ionospheric Indices to the Solar and Geomagnetic Activity Indices

Geomagnetism and Aeronomy, 2022-08, Vol.62 (4), p.382-387

2022

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Relation of the Monthly Mean Ionospheric T Index to Solar and Geomagnetic Activity Indices

Geomagnetism and Aeronomy, 2021-11, Vol.61 (6), p.830-835

2021

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Perturbation Features Imprinted on Ionosphere by Successive Clusters of Strong Earthquakes: Role of Atmospheric Coupling Dynamics

Geomagnetism and Aeronomy, 2019-12, Vol.59 (8), p.955-970

2019

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Anomalous total electron content (TEC) and atmospheric refractivity prior to the very strong China earthquake of May 2008

International journal of remote sensing, 2010-07, Vol.31 (13), p.3589-3599

2010

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Storm Time Ionospheric-Tropospheric Dynamics: a Study Through Ionospheric and Lower Atmospheric Variability Features of High/Mid and Low Latitudes

Geomagnetism and Aeronomy, 2018-12, Vol.58 (7), p.857-870

2018

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Synchronous NmF2 and NmE daytime variations as a key to the mechanism of quiet-time F2-layer disturbances

Annales geophysicae (1988), 2007-01, Vol.25 (2), p.483-493

2007

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Main phenomenological features of ionospheric precursors of strong earthquakes

Journal of atmospheric and solar-terrestrial physics, 2003-11, Vol.65 (16), p.1337-1347

2003

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Quiet time F2-layer disturbances: seasonal variations of the occurrence in the daytime sector

Annales geophysicae (1988), 2009-01, Vol.27 (1), p.329-337

2009

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Daytime F2-layer negative storm effect: what is the difference between storm-induced and Q-disturbance events?

Annales geophysicae (1988), 2007-01, Vol.25 (7), p.1531-1541

2007

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The anomaly of plasmapause and ionospheric trough positions from DEMETER data

Geomagnetism and Aeronomy, 2014-11, Vol.54 (6), p.763-772

2014

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Preliminary results of TEC measurements in Guwahati, India

Advances in space research, 2008-08, Vol.42 (4), p.753-756

2008

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A global empirical model of the ionospheric topside electron density

Advances in space research, 2004, Vol.34 (9), p.2016-2020

2004

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Reaction of the critical frequency of the F2 layer to a sharp depletion in atmospheric pressure

Geomagnetism and Aeronomy, 2010-12, Vol.50 (6), p.804-813

2010

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Properties of the Variability of the Maximum Density of the F2-Layer over Almaty at Different Levels of Solar and Geomagnetic Activity

Geomagnetizm i aėronomija, 2023-09, Vol.63 (5), p.630-637

2023

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Intercosmos-19 observations of an additional topside ionization layer: the F3 layer

Advances in Space Research, 2001-01, Vol.27 (6), p.1289-1292

2001

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Mechanism of formation of Q-disturbances in the F 2 region of the equatorial ionosphere

Geomagnetism and aeronomy, 2008-02, Vol.48 (1), p.89-97

2008

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Recent advances in topside profile modeling

Advances in Space Research, 2002-01, Vol.29 (6), p.815-823

2002

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Role of Equatorial Anomaly in Earthquake time precursive features: A few strong events over West Pacific zone

Advances in space research, 2018-03, Vol.61 (6), p.1444-1455

2018

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Dependence of the F2-layer critical frequency median at midlatitudes on geomagnetic activity

Solnečno-zemnaâ fizika, 2017-12, Vol.3 (4), p.74-81

2017

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Diurnal variations of the peak electron density distribution pattern at low latitudes derived from intercosmos-19 topside sounding data

Advances in space research, 2003, Vol.31 (3), p.521-530

2003

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Electron density profile changes in a pre-earthquake period

Advances in space research, 1996, Vol.18 (6), p.115-118

1996

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Global distribution of night-time F2 peak density (INTERCOSMOS-19 data)

Advances in space research, 2000, Vol.25 (1), p.105-108

2000

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NmF2 Variability at Different Longitudes in Mid-Latitudes: The Role of Geomagnetic Activity

Seasonal Features of the NmF2 Variability for Different Longitudes of the Middle Latitudes during Enhanced Geomagnetic Activity

Properties of the Variability of the Maximum Density of the F 2-Layer over Almaty at Different Levels of Solar and Geomagnetic Activity

The Relationship of the IG and T Ionospheric Indices to the Solar and Geomagnetic Activity Indices

Relation of the Monthly Mean Ionospheric T Index to Solar and Geomagnetic Activity Indices

Perturbation Features Imprinted on Ionosphere by Successive Clusters of Strong Earthquakes: Role of Atmospheric Coupling Dynamics

Anomalous total electron content (TEC) and atmospheric refractivity prior to the very strong China earthquake of May 2008

Storm Time Ionospheric-Tropospheric Dynamics: a Study Through Ionospheric and Lower Atmospheric Variability Features of High/Mid and Low Latitudes

Synchronous NmF2 and NmE daytime variations as a key to the mechanism of quiet-time F2-layer disturbances

Main phenomenological features of ionospheric precursors of strong earthquakes

Quiet time F2-layer disturbances: seasonal variations of the occurrence in the daytime sector

Daytime F2-layer negative storm effect: what is the difference between storm-induced and Q-disturbance events?

The anomaly of plasmapause and ionospheric trough positions from DEMETER data

Preliminary results of TEC measurements in Guwahati, India

A global empirical model of the ionospheric topside electron density

Reaction of the critical frequency of the F2 layer to a sharp depletion in atmospheric pressure

Properties of the Variability of the Maximum Density of the F2-Layer over Almaty at Different Levels of Solar and Geomagnetic Activity

Intercosmos-19 observations of an additional topside ionization layer: the F3 layer

Mechanism of formation of Q-disturbances in the F 2 region of the equatorial ionosphere

Recent advances in topside profile modeling

Role of Equatorial Anomaly in Earthquake time precursive features: A few strong events over West Pacific zone

Dependence of the F2-layer critical frequency median at midlatitudes on geomagnetic activity

Diurnal variations of the peak electron density distribution pattern at low latitudes derived from intercosmos-19 topside sounding data

Electron density profile changes in a pre-earthquake period

Global distribution of night-time F2 peak density (INTERCOSMOS-19 data)

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