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spring and summer, and mixing of upper cooler water with lower warmer water reduces the rate of cooling during the fall and winter. c. Evaporation: As we will see in much more detail in Laboratory 7, evaporation uses energy and is a cooling process; there is much more evaporation over water surfaces than over land surfaces; this results in slower warming of water surfaces than of land surfaces as much of the energy that would be used for heating the surface is instead used for evaporation. d. Specific heat: Specific heat is the amount of energy required to raise the temperature of a given substance; the specific heat of water is about three times greater than that of land; even ignoring the other factors listed above, this would result in a slower rate of warming of water than of land. e. Heat capacity: Water can store heat energy better than can land; a given volume of water having the same temperature as the same volume of land will be storing more heat energy than the land; as a result, more heat energy must be lost from a given volume of water for it to cool a given number of degrees than must be lost from the same volume of land for it to cool the same amount. (B-1) Match each of the five factors listed below, with the appropriate statement A, B, or C. Statement A: This factor results in a water surface heating more slowly than a land surface. Statement B: This factor results in a water surfice cooling down more slowly than a land surface. Statement C: This factor results in a water surface both heating more slowly and cooling down more slowly than a land surface. The differential heating of land and water has a major influence on global temperature patterns. All else being equal, areas far removed from a large water body experience the greatest annual temperature ranges (i.e., the greatest differences between summer and winter temperatures). These land areas far from the influence of water are referred to as continental. Areas near the moderating water bodies are referred to as being marine. (B-2) The two temperature graphs below are for locations that are similar in terms of their latitude and the other temperature controls that we will discuss shortly. However, one of these graphs is for a continental location, while the other is for a marine location. Which of the graphs is for a continental location? Briefly explain. C: Ocean Currents A series of surface currents exist in the world's oceans. These currents are generally strongest near the coasts. Especially in the mid-latitudes, the water temperatures associated with these currents tend to differ greatly on the opposite sides of the oceans. These currents are labeled as being either cold currents or warm currents. Although there are exceptions, cold currents are usually found along west coasts (the eastern side of the ocean) and warm currents are usually found along east coasts (the western side of the ocean). Because the air is heated and cooled primarily from being in contact with.
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