Climatology of Mid-latitude Ionospheric Disturbances from the Very Large Array Low-frequency Sky Survey

TL;DR

This study analyzes ionospheric disturbances using VLA Low-frequency Sky Survey data, revealing seasonal, diurnal, and activity-related variations in TEC fluctuations across multiple spatial and temporal scales.

Contribution

It provides a comprehensive climatological analysis of ionospheric disturbances using VLA data, including multi-scale fluctuation spectra and their dependence on geomagnetic and solar activity.

Findings

Detection of wavelike structures between 35 and 250 km wavelengths.

Ionospheric turbulence more active during winter days and summer nights.

Weak correlation between turbulence levels and geomagnetic or solar activity.

Abstract

The results of a climatological study of ionospheric disturbances derived from observations of cosmic sources from the Very Large Array (VLA) Low-frequency Sky Survey (VLSS) are presented. We have used the ionospheric corrections applied to the 74 MHz interferometric data within the VLSS imaging process to obtain fluctuation spectra for the total electron content (TEC) gradient on spatial scales from a few to hundreds of kilometers and temporal scales from less than one minute to nearly an hour. The observations sample nearly all times of day and all seasons. They also span latitudes and longitudes from 28 deg. N to 40 deg. N and 95 deg. W to 114 deg. W, respectively. We have binned and averaged the fluctuation spectra according to time of day, season, and geomagnetic (Kp index) and solar (F10.7) activity. These spectra provide a detailed, multi-scale account of seasonal and intraday variations in ionospheric activity with wavelike structures detected at wavelengths between about 35 and 250 km. In some cases, trends between spectral power and Kp index and/or F10.7 are also apparent. In addition, the VLSS observations allow for measurements of the turbulent power spectrum down to periods of 40 seconds (scales of ~0.4 km at the height of the E-region). While the level of turbulent activity does not appear to have a strong dependence on either Kp index or F10.7, it does appear to be more pronounced during the winter daytime, summer nighttime, and near dusk during the spring.