Energy Transfer in Mount Everest’s Ice: Radiation, Conduction, and More

Solar Radiation

Sunlight strikes the ice, and a portion is absorbed, warming the surface.

Conduction

The warmed ice transfers heat to adjacent air molecules through direct molecular collisions.

Convection

Heated air rises, creating convection currents that carry thermal energy away from the ice face.

Thermal Radiation

The ice itself emits infrared radiation, exchanging heat with surrounding rock and air.

Sublimation

At extreme altitude, low pressure and cold temperatures cause ice to transition directly to water vapor, a process that consumes latent heat.

Avalanches

When massive ice sheets destabilize, they release gravitational potential energy as kinetic energy, producing destructive avalanches.

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