The temperature of land near water is different than inland due to the phenomenon known as the "marine effect" or "coastal effect." This effect is primarily caused by the differences in specific heat capacities and thermal conductivity between land and water.
Specific heat capacity refers to the amount of heat energy required to raise the temperature of a substance. Water has a higher specific heat capacity compared to land, which means it can absorb and store more heat energy. As a result, it takes longer for water to heat up or cool down.
Additionally, water has higher thermal conductivity compared to land. This means that heat can transfer more easily and quickly through water than through land. So, the water near the coast absorbs heat during the day more efficiently than the adjacent land.
During the day, the land near water heats up more slowly than inland because the water moderates the temperature, acting as a heat sink. The water absorbs the sun's energy, which keeps the air temperature cooler near the coast. Conversely, inland areas heat up faster because there is no such heat sink to moderate the temperature.
At night, the situation reverses. The land loses heat more rapidly than water due to its lower specific heat capacity and thermal conductivity. As a result, the land near the water cools down slower than inland, as the water releases some of the stored heat, keeping the air temperature relatively warmer near the coast.
These differences in heating and cooling rates create the temperature variation between land near water and inland areas.
Which of the following explains why the temperature of land near water is different than inland
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