At the core of the Wave Interaction and Propagation domain is the understanding of the behaviour of electromagnetic waves in a variety of media and environmental conditions, and the application of this understanding to the definition and exploitation of space missions.
The environment can be a source of perturbations in the use of electromagnetic waves from space. Radio signals from telecom satellites are disrupted by tropical rainstorms, satellite to mobile radio links in urban areas are disturbed by spurious reflections on buildings walls, navigation solutions are degraded by plasma layers in the upper atmosphere and optical images of the Earth surface acquired from space are modified by the atmosphere layer that lies in between. In order to circumvent these effects, they need to be understood, assessed and mitigated.
On the other hand, space provides a unique vantage point from which to probe the Earth or the other planets of the solar system. Remote sensing relies on the ability of electromagnetic waves to carry back to a spaceborne instrument relevant information about a physical or biological property of the natural environment in its field of view. This information is then used for science or applications (e.g. climate studies, meteorology, land use, pollution monitoring, planetology). The quantity of vegetation on a surface drives the response of near infrared channels of optical imagers, the centimetric radar backscatter from the ocean scales with the surface roughness, giving information on the local wind conditions, the radiometric emission of soils in decimetric waves depends on their moisture content, the presence of liquid water underneath Europa ice mantle would change the echo measured from a radar sounder. A thorough understanding of these relations is paramount to make a proper use of remote sensing techniques.