The increase in temperatures from climate change leads to a greater melting of snow and ice, particularly noticeable at the North Pole. This results in a decrease in Earth's overall albedo, causing the planet to absorb a greater amount of solar energy. With less heat being reflected back into space, the Earth warms up, intensifying the melting of ice. This, in turn, amplifies the cycle, causing further melting of snow and ice and a continual reduction in the Earth's reflectivity.