Skip to content  

The albedo effect has significant implications for the Earth's climate:

On a global scale, Earth's average albedo is approximately , meaning roughly one-third of the sunlight reaching our planet is reflected away. Types of Albedo

The loss of reflective white surfaces exposes darker ocean water or land beneath.

This loop explains why the Arctic is warming two to three times faster than the rest of the planet—a phenomenon known as Arctic amplification.

While we focus on Earth, albedo is a universal planetary diagnostic tool used by astronomers.