Earth’s surface is mostly covered by water. Areas not covered by water—the continents—are surrounded by water. If land and water had the same specific heat, we would expect the land and surrounding water to heat up and cool down at the same rate. From experience, we know this is not the case. In this Activity, you will investigate the heat capacities of sand and water as a simple model of land and a body of water.
Details
Type Book ChapterPub Date 9/20/2011Stock # PB298X3_4a