2. Conduction: The warmed ice then transfers some of its heat to the surrounding air through conduction. This occurs when the molecules of the ice collide with the molecules of the air, transferring thermal energy.
3. Convection: As the air warmed by the ice rises, it creates convection currents. This warm air carries heat away from the ice and transfers it to other parts of the mountain.
4. Radiation: The ice also emits its own thermal radiation, which travels through the air and transfers heat to other objects in the environment.
5. Sublimation: At very high altitudes, such as on Mount Everest, the air pressure is lower and the temperature is colder. This can cause the ice to sublime, which is the process by which a solid directly transforms into a gas without passing through the liquid phase.
6. Avalanches: When large masses of ice on Mount Everest become unstable, they can break away and cause avalanches. Avalanches can release a significant amount of energy, which can damage infrastructure and injure or kill people.
