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During summer, land heats up more quickly than water due to its lower specific heat capacity, meaning it requires less energy to increase its temperature. Consequently, land surfaces can reach higher temperatures than bodies of water. In contrast, water absorbs heat more slowly and retains it longer, resulting in cooler temperatures during the day and warmer temperatures at night. This difference creates a moderating effect on coastal climates, where land temperatures can fluctuate more dramatically than those over the sea.

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