Exam 3: Air Temperature

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The diurnal insolation patterns illustrated on this figure most closely resemble those from: The diurnal insolation patterns illustrated on this figure most closely resemble those from:

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Examine the monthly mean air temperature patterns shown in this figure. The curve for the city of Hamburg at 54ᵒ N latitude is labeled: Examine the monthly mean air temperature patterns shown in this figure. The curve for the city of Hamburg at 54ᵒ N latitude is labeled:

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Which of the following areas would tend to have the warmest air temperatures on a given day, assuming all receive the same insolation?

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On a warm summer day, latent heat transfers will tend to:

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During the daytime, net radiation at the ground surface tends to be positive.

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Average temperatures tend to increase with elevation in the troposphere , at a given latitude.

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The temperature change in coastal regions from January to July is __________ the change in continental regions.

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Temperature tends to ______ with elevation in the mesosphere, and ________ with elevation in the stratosphere.

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The average environmental lapse rate in the troposphere is about:

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Locations near the equator experience two peaks in annual insolation that coincide with the equinoxes.

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For mid-latitude locations, total daily insolation tends to highest on the:

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The two lowest layers of the atmosphere are separated by the:

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Identify the anthropogenic factors that influence global warming

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Heat energy transferring from a warm object to a cold object when placed in direct contact is a form of conduction.

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Heat that is absorbed and stored in a gas or liquid during the processes of evaporation, melting, or sublimation is:

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The temperature of the ground surface and the near surface layer of air tends to reach a maximum at the local solar noon, when insolation levels are at their highest.

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Which of the following does not contribute to global warming?

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Over the past 30 years, the temperature of the Earth :

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The ozone layer is found in the troposphere.

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Temperature inversions often occur at night, as the ground surface radiatively cools and in turn cools the layer of air immediately above it.

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