Glaciers in Norway, even at low altitudes like 300 meters above sea level, do not melt entirely despite temperatures reaching 20°C for several months due to several factors. The significant mass of glacial ice compared to the surrounding air means that a considerable amount of heat is required to melt it, as water has a higher specific heat than air. Additionally, glaciers are dynamic systems that can gain ice from snowfall and freezing rain at higher elevations, which compensates for any melting at lower levels. The melting ice can also evaporate and refreeze, contributing to the glacier's mass. Furthermore, glaciers can create their own microclimates, leading to cooler air outflows that can enhance snowfall and further support glacier growth. The reflective nature of ice helps minimize heat absorption from sunlight, although contamination from dust or soot can increase melting rates. Overall, while glaciers may be melting, they are also continually replenished, allowing them to persist even in warmer conditions.