Arctic sea ice, a key component in our planet’s climate system, acts as a reflective barrier that modulates the energy exchange between the atmosphere and the ocean. Its extent and volume are sensitive indicators of climate change. The predictability of Arctic sea ice is of paramount importance for understanding future climate scenarios, as well as for the navigation and ecosystems that depend on its seasonal patterns. The rapid loss of Arctic sea ice in recent decades, especially during the summer, has attracted growing interest in the predictability and prediction practices of sea ice on seasonal timescales.