Specific Heat Capacity and Coastal Microclimates: Why Beaches Warm Faster Than Seawater

比热容与沿海微气候：为何沙滩升温快于海水

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Sand heats approximately four times faster than seawater under identical solar irradiance—not because of darker color or surface texture, but due to its specific heat capacity being roughly 0.8 J/g·K versus water’s 4.18 J/g·K.
This thermodynamic property dictates how much energy a substance absorbs before its temperature rises, explaining why coastal cities experience delayed summer warming compared to inland counterparts.

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