Transit spectroscopy involves observing the absorption or emission of light as an exoplanet passes in front of its host star, providing information about the composition and structure of the exoplanet's atmosphere.

Solar radiation absorbed by the exoplanet's atmosphere is the main driver of atmospheric circulation, leading to the formation of weather patterns and winds.

Seismic modeling involves analyzing the vibrations and oscillations of an exoplanet, similar to seismology on Earth, to infer information about its internal structure and composition.

The mass of an exoplanet plays a crucial role in determining its internal composition, with more massive exoplanets having denser cores and potentially different compositions compared to less massive ones.

Tidal locking occurs when an exoplanet's rotation period becomes synchronized with its orbital period, resulting in one side of the planet always facing the host star and the other side always facing away.

Mass transfer refers to the exchange of material between an exoplanet and its host star, which can occur through processes such as stellar winds or tidal interactions.

The transit method involves observing the periodic dimming of a star's light as an exoplanet passes in front of it, allowing astronomers to infer the presence and properties of the exoplanet.

Transit timing variations refer to the slight changes in the timing of an exoplanet's transits across its host star, which can be caused by the presence of additional planets or other objects in the system.

Hydrogen-dominated atmospheres are prevalent among exoplanets, particularly those that are larger and more massive, due to the abundance of hydrogen in the universe.

Orbital migration refers to the gradual change in an exoplanet's orbital parameters, such as its semi-major axis, eccentricity, or inclination, over time.

Zeeman splitting involves analyzing the splitting of spectral lines due to the presence of a magnetic field, allowing astronomers to infer the strength and structure of an exoplanet's magnetic field.

Atmospheric escape refers to the loss of an exoplanet's atmosphere into space, which can occur through various mechanisms such as stellar winds, high-energy radiation, or collisions with other objects.

Rocky cores are prevalent among exoplanets, particularly those that are smaller and less massive, due to the abundance of rocky materials in the universe.

Orbital circularization refers to the gradual reduction in the eccentricity of an exoplanet's orbit, resulting in a more circular orbit over time.