Numerical Investigation on the Height and Intensity Variations of Sporadic E Layers at Mid-Latitude

In previous studies, various physical parameters, such as vertical wind shear null, vertical ion velocity null (IVN), and maximum gradient of vertical ion velocity, have been used as an indicator of Es layer height in light of the wind shear theory. Using a numerical Es layer model, we investigated which parameter represents the height of Es layer over Wuhan (114.4 degrees E, 30.5 degrees N) most precisely. The simulation results show that the height of Es layer above 110 km depends most strongly on the height of vertical IVN. However, below 110 km, the height of vertical IVN does not always agree with the height of Es layer. The analysis of simulation results suggests that the vertical gradient of the ratio of the ion-neutral collision frequency (nu(i)) to the ion gyrofrequency (omega(i)) affects the Es layer formation at lower altitudes (below 110 km). We also examined the effect of electric fields on the height and intensity of Es layers over Wuhan. It is found that eastward/upward electric fields can lift the Es layer height and reduce the Es layer intensity.

Automated summary

Previous studies have used various physical parameters as indicators of Es layer height, but this study found that vertical ion velocity null (IVN) most accurately represents the height of Es layer over Wuhan. The simulation results also suggest that the vertical gradient of the ratio of ion-neutral collision frequency to ion gyrofrequency affects the formation of Es layer at lower altitudes. Additionally, the effect of electric fields on the height and intensity of Es layers was examined, showing that eastward/upward electric fields can lift the Es layer height and reduce intensity.