I think the ice is warmed from 10 degrees Fahrenheit to 32 degrees Fahrenheit. The ice then melts (I believe 333kj/kg K) and then it warms up to 305 K. For that this occurs the heat capacity of the water is 4.19 kj/kg K.
The ice on Mount Everest heats from -12.2 °C to 0 °C, absorbing heat until it melts, which requires latent heat. After melting, the water is then heated to approximately 31.85 °C, requiring additional heat energy. This process involves energy transfers from the environment that facilitate the temperature changes and phase transitions.
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