
The dayside of a planet is the hemisphere facing its star, typically receiving direct stellar radiation.The dayside of a planet is the hemisphere that faces its star and receives direct stellar radiation. This is the side where it is 'day' — the sun is above the horizon, and the surface is bathed in starlight. The opposite hemisphere, the nightside, faces away and is dark. For planets that rotate slowly or are tidally locked (always showing the same face to their star), the contrast between dayside and nightside can be extreme, shaping the planet's climate, atmosphere, and even its geology.
The concept of a planetary dayside is as old as astronomy itself, but the term became particularly important with the discovery of tidally locked exoplanets in the 1990s and 2000s, when scientists began modeling their extreme day-night contrasts.
The dayside receives the bulk of the star's energy, which drives heating of the surface and atmosphere. This energy input powers atmospheric circulation, weather patterns, and can evaporate volatile materials. On tidally locked planets, the dayside is permanently hot, while the nightside is permanently cold, creating strong temperature gradients that drive powerful winds and may cause exotic phenomena like 'rocky waves' in magma oceans or atmospheric collapse on the nightside.
Understanding the dayside is crucial for interpreting observations of exoplanet atmospheres, as telescopes often measure the combined light from both hemispheres, and for modeling the habitability of planets around red dwarf stars.
On some tidally locked exoplanets, the dayside is so hot that it melts rock, creating global magma oceans with waves driven by the relentless stellar heat.












