The wind-shear theory of sporadic E predicts that when only one ion species is present, and the peak electron density is a factor R times the ambient, the minimum electron density is 1/R of the ambient. With two species present, the minimum electron density is greater than this and approaches the ambient when the ratio of recombination coefficients is large and the more rapidly recombining ion predominates in the ambient ionsphere. The peak density depends only on the recombination coefficient of the slowly recombining ion and the gradient in the vertical drift motion. The problem of nighttime sporadic E is considered, but no satisfactory solution is offered
This paper presents a theory for the asymptotically steady-state solar wind electron velocity distri...
A model of the spectrum of the electron density turbulent fluctuations in the Earth's midlatitude lo...
The electron distribution functions from the solar corona to the solar wind are determined in this p...
Theoretical and experimental work since 1970 is summarized. Mid-latitude sporadic-E is most likely d...
A seasonally dependent total neutral wind model obtained from experimental data is used to evaluate...
366-369The redistribution of charged particles in the lower ionosphere in the presence of wind shear...
The wind shear theory is widely accepted as an explanation for the formation of a sporadic E (Es) la...
A model of the ionospheric E-region between 90 and 130 km altitude is constructed with normal molecu...
The starting point of this investigation is the partially transparent echo from midlatitude sporadi...
The importance of electric field in formation of sporadic E (Es) at the equatorial region is investi...
Ion convergence rates at various latitudes are calculated and discussed in relation to the formation...
The formation of the mid-latitude sporadic E layers (Es layers) by an atmospheric vortical perturba...
On the basis of quasi-hydrodynamic equations we consider formation of electron-density uctuations b...
235-239The occurrence of sporadic E at temperate latitudes in the eastern zone is found to be more f...
On the assumption that the ion production rate at E-layer maximum varies diurnally with the cosine o...
This paper presents a theory for the asymptotically steady-state solar wind electron velocity distri...
A model of the spectrum of the electron density turbulent fluctuations in the Earth's midlatitude lo...
The electron distribution functions from the solar corona to the solar wind are determined in this p...
Theoretical and experimental work since 1970 is summarized. Mid-latitude sporadic-E is most likely d...
A seasonally dependent total neutral wind model obtained from experimental data is used to evaluate...
366-369The redistribution of charged particles in the lower ionosphere in the presence of wind shear...
The wind shear theory is widely accepted as an explanation for the formation of a sporadic E (Es) la...
A model of the ionospheric E-region between 90 and 130 km altitude is constructed with normal molecu...
The starting point of this investigation is the partially transparent echo from midlatitude sporadi...
The importance of electric field in formation of sporadic E (Es) at the equatorial region is investi...
Ion convergence rates at various latitudes are calculated and discussed in relation to the formation...
The formation of the mid-latitude sporadic E layers (Es layers) by an atmospheric vortical perturba...
On the basis of quasi-hydrodynamic equations we consider formation of electron-density uctuations b...
235-239The occurrence of sporadic E at temperate latitudes in the eastern zone is found to be more f...
On the assumption that the ion production rate at E-layer maximum varies diurnally with the cosine o...
This paper presents a theory for the asymptotically steady-state solar wind electron velocity distri...
A model of the spectrum of the electron density turbulent fluctuations in the Earth's midlatitude lo...
The electron distribution functions from the solar corona to the solar wind are determined in this p...