Ice Melting

Ice melting occurs when solid ice absorbs heat energy, causing its temperature to rise until it reaches 0 degrees Celsius (32 degrees Fahrenheit), the melting point. At this temperature, the ice's rigid structure breaks down, and it transitions into liquid water. This process is influenced by factors like ambient temperature and pressure. Melting ice is a natural part of the water cycle, playing a crucial role in ecosystems. Increased global temperatures due to climate change are leading to accelerated ice melting in polar regions, contributing to rising sea levels and impacting habitats and weather patterns.