International audienceThis paper investigates the role of neutral winds in the generation of relatively large polarization electric fields across patchy sporadic-E layers, which then map upward to the F region, to create conditions for medium-scale spread-F. The calculations are based on an analytical model that uses the current continuity equation and field-aligned current closures to the F region in order to describe quantitatively a Hall polarization process inside sporadic-E plasma patches during nighttime. In applying this model we use experimentally known values for E and F region, conductances, the ambient electric fields and prevailing neutral winds, in order to estimate the polarization fields that build up inside sporadic-E. It is...
This work will present an advancement of the physical understanding of medium-scale traveling ionosp...
During the last two years Doppler shift observations of the 6300A atomic oxygen line were carried ou...
The E-region dynamo functions because at heights of about 100-150 kin the ions and electrons move di...
This paper investigates the role of neutral winds in the generation of relatively large polarizatio...
This paper provides a review on some of the electrostatic coupling effects relevant for generating/m...
Almost no new theoretical work has been conducted in the area of mid-latitude F-region plasma instab...
The thermospheric neutral wind and ionospheric layer conductance at latitudes higher than 45 degrees...
This paper investigates the roles of electric field and neutral wind in the generation of sporadic-...
The importance of electric field in formation of sporadic E (Es) at the equatorial region is investi...
In the mid-latitude E-region there is now evidence suggesting that neutral winds play a significa...
In the mid-latitude ionospheric region, sporadic-E layers (Es layers) have often been observed, rev...
International audienceThe generic equilibrium configuration of the nighttime midlatitude ionosphere ...
An anomalous polarization electric field may be set-up in the lower auroral E-region in response to ...
The temporal and spatial variations in thermospheric neutral winds at an altitude of 400 km in respo...
Ionospheric electric fields play fundamental roles in the dynamics of the Earth\u27s ionosphere and ...
This work will present an advancement of the physical understanding of medium-scale traveling ionosp...
During the last two years Doppler shift observations of the 6300A atomic oxygen line were carried ou...
The E-region dynamo functions because at heights of about 100-150 kin the ions and electrons move di...
This paper investigates the role of neutral winds in the generation of relatively large polarizatio...
This paper provides a review on some of the electrostatic coupling effects relevant for generating/m...
Almost no new theoretical work has been conducted in the area of mid-latitude F-region plasma instab...
The thermospheric neutral wind and ionospheric layer conductance at latitudes higher than 45 degrees...
This paper investigates the roles of electric field and neutral wind in the generation of sporadic-...
The importance of electric field in formation of sporadic E (Es) at the equatorial region is investi...
In the mid-latitude E-region there is now evidence suggesting that neutral winds play a significa...
In the mid-latitude ionospheric region, sporadic-E layers (Es layers) have often been observed, rev...
International audienceThe generic equilibrium configuration of the nighttime midlatitude ionosphere ...
An anomalous polarization electric field may be set-up in the lower auroral E-region in response to ...
The temporal and spatial variations in thermospheric neutral winds at an altitude of 400 km in respo...
Ionospheric electric fields play fundamental roles in the dynamics of the Earth\u27s ionosphere and ...
This work will present an advancement of the physical understanding of medium-scale traveling ionosp...
During the last two years Doppler shift observations of the 6300A atomic oxygen line were carried ou...
The E-region dynamo functions because at heights of about 100-150 kin the ions and electrons move di...