The process that describes the warm ocean transferring heat to the air above it is called evaporation.
As the surface of the ocean warms due to solar radiation, water molecules at the surface gain energy and transition into the vapor phase. This process not only involves the release of heat into the atmosphere but also contributes to humidity. The warm, moist air can rise, cool, and lead to processes such as cloud formation and precipitation. Additionally, this heat transfer is an essential component of larger atmospheric circulation patterns and plays a critical role in weather systems and climate regulation.
In a broader context, this process is part of the ocean-atmosphere interaction, which is critical for understanding weather, climate change, and ocean circulation patterns.
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