Exam 3: Energy Balance Essentials

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Why do the tropics have a positive net radiation while the poles have a negative value? How is the energy difference equalized?

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A stove that circulates heated air to uniformly cook food is an example of__________ heat transfer.

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The Celsius scale

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Which of the following is a nonradiative transfer of longwave radiation to the atmosphere?

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The albedo of a surface is a measure of which of the following processes?

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Where should you move to if you wanted to live an a region with the greatest annual range of temperatures? If you changed your mind and wanted to live in the region with the lowest annual temperature range where should you go? What are the qualities that create each of these situations?

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The average building in the United States does not receive enough solar energy required to heat the inside of the building.

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In equatorial and tropic regions,energy surpluses prevail,whereas energy deficits prevail at higher latitudes.

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The intensity of solar radiation decreases away from the equator and poleward.

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Most evaporation occurs over large land masses influenced by continentality.

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When light passes from one medium to another,resulting in a change in its speed and direction

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The land-water heating difference that specifically relates to opaqueness is

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Between the tropics,low angle of insolation,variable day lengths,and high seasonal variations create an energy deficit.

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As it pertains to differences in land-water heating,transparency

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Net radiation (NET R)refers to

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The effect of wind and temperature on the human skin is called the

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  -Which of the following is TRUE? -Which of the following is TRUE?

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Snow line elevation increases with increasing latitude.

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  -The relationship between the insolation curve and the air temperature curve on a graph of daily surface energy -The relationship between the insolation curve and the air temperature curve on a graph of daily surface energy

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Average air temperatures at higher elevations are generally higher,with smaller differences between areas of direct sunlight and shadow.

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