What is hypothesis for ice melting?

The hypothesis for ice melting is that when ice is exposed to temperatures above its melting point (0 degrees Celsius or 32 degrees Fahrenheit), the heat energy from the surroundings is transferred to the ice, causing the ice molecules to gain enough kinetic energy to overcome the intermolecular forces holding them in a solid state. This results in the ice transitioning into a liquid state. The hypothesis can be tested through controlled experiments where ice is subjected to different temperatures and the rate of melting is observed and measured.