In the mid-latitude ionospheric region, sporadic-E layers (Es layers) have often been observed, revealing multiple layers. The Es layers observed during the SEEK-2 rocket campaign showed double electron density peaks; namely, there are stable lower peaks and relatively unstable upper peaks. We examined the effects of wind shear and the electric fields on the generation of the multiple layer structure, in comparison with the electron density profile, the neutral wind, and the DC electric field observed by the S310 rocket experiments. The results showed that the neutral wind shear is mainly responsible for the generation of the lower layer, while the DC electric field makes a significant contribution to the formation of the upper la...
The electron temperature (Te), electron density (Ne), and two components of the electric field were...
The importance of electric field in formation of sporadic E (Es) at the equatorial region is investi...
Sporadic E is itself a stratification within the E-region. The seasonal, diurnal and geographic dist...
International audienceIn the mid-latitude ionospheric region, sporadic-E layers (Es layers) have oft...
Electric field and plasma density data gathered on a sounding rocket launched from Uchinoura Space ...
Observational campaigns of the mid-latitude ionospheric E-region with sounding rockets and ground...
The starting point of this investigation is the partially transparent echo from midlatitude sporadi...
The descent of a narrow sporadic E layer near 95 km altitude over Poker Flat Research Range in Alas...
International audienceThe SEEK-2 campaign was carried out over Kyushu Island in Japan on 3 August 20...
A study of the formation and movement of sequential Sporadic-E layers observed during the night-tim...
We present data from nighttime sounding rocket flights in the low latitude E region. The payloads ca...
Electron density data obtained over the dip equator using rocket-borne high resolution Langmuir prob...
This paper investigates the roles of electric field and neutral wind in the generation of sporadic-...
The characteristics of different types of Sporadic E (E<SUB>S</SUB>) layers and the associated plasm...
Data obtained with rockets flown over New Mexico, U.S.A. and Manitoba, Canada have always shown the ...
The electron temperature (Te), electron density (Ne), and two components of the electric field were...
The importance of electric field in formation of sporadic E (Es) at the equatorial region is investi...
Sporadic E is itself a stratification within the E-region. The seasonal, diurnal and geographic dist...
International audienceIn the mid-latitude ionospheric region, sporadic-E layers (Es layers) have oft...
Electric field and plasma density data gathered on a sounding rocket launched from Uchinoura Space ...
Observational campaigns of the mid-latitude ionospheric E-region with sounding rockets and ground...
The starting point of this investigation is the partially transparent echo from midlatitude sporadi...
The descent of a narrow sporadic E layer near 95 km altitude over Poker Flat Research Range in Alas...
International audienceThe SEEK-2 campaign was carried out over Kyushu Island in Japan on 3 August 20...
A study of the formation and movement of sequential Sporadic-E layers observed during the night-tim...
We present data from nighttime sounding rocket flights in the low latitude E region. The payloads ca...
Electron density data obtained over the dip equator using rocket-borne high resolution Langmuir prob...
This paper investigates the roles of electric field and neutral wind in the generation of sporadic-...
The characteristics of different types of Sporadic E (E<SUB>S</SUB>) layers and the associated plasm...
Data obtained with rockets flown over New Mexico, U.S.A. and Manitoba, Canada have always shown the ...
The electron temperature (Te), electron density (Ne), and two components of the electric field were...
The importance of electric field in formation of sporadic E (Es) at the equatorial region is investi...
Sporadic E is itself a stratification within the E-region. The seasonal, diurnal and geographic dist...