A new study, based on data from NASA sounding rockets, has for the first time revealed the internal structure of sporadic E layers, plasma metallic "clouds" that form in Earth's upper atmosphere. These layers, composed of vaporized meteoritic dust, are known for their unpredictable appearance and dissipation, and can interfere with radio and GPS signals. The research offers an unprecedented insight into how these formations affect communications and the ionosphere.

Sounding rockets, suborbital vehicles designed for short-duration research missions, allowed scientists to take multipoint measurements within these layers. By launching multiple instruments through the same sporadic E layer, a detailed profile of its density and composition could be obtained. This method has been crucial for understanding the spatial and temporal variability of these layers, which until now could only be observed remotely or with single-point measurements.

The results of this mission are fundamental for improving models of Earth's ionosphere and more accurately predicting communication disruptions. Understanding the dynamics of sporadic E layers not only has implications for navigation and radio transmissions, but also contributes to the study of how near-Earth space interacts with the upper atmosphere, a critical area of research for space weather.