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Thermal energy transfer in the hydrologic cycle occurs primarily through the processes of evaporation and condensation. When water evaporates from the surface of oceans, lakes, and rivers, it absorbs heat energy from the surroundings, cooling them down. As the water vapor rises and condenses to form clouds, this heat energy is released back into the atmosphere, influencing weather patterns and the overall climate.

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Q: How does thermal energy transfer in the hydrologic cycle?
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