The yearly temperature ranges of interior regions of the us are larger than coastal temperature ranges because rock and soil have a lower heat capacity as compared to water. It is because of the thermal difference between land and water.
Because water absorbs heat more slowly than land, it holds heat longer. Constant sea breezes also make beaches and coastal areas cooler in the summer and warmer in the winter. Water also heats up and cools down more slowly than land. In essence, the water serves as a massive natural heater in the winter and a massive natural air conditioner in the summer.
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