Exam 5: Global Atmospheric and Oceanic Circulation

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The flow of surface wind from ocean to land that commonly occurs during late afternoon is called a _______ .

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The surface wind system known as the doldrums is labeled: The surface wind system known as the doldrums is labeled:

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In a cyclone located in the southern hemisphere winds:

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Which of the following is not a component of upper air circulation?

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Valley breezes flow from:

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Geostrophic winds are found at:

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The zone where air masses converge along the equatorial trough is called the _________.

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The Santa Ana is a local wind that can exacerbate wildfires in southern California.

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The magnitude of the Coriolis force:

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The Coriolis effect results from the rotation of the earth about its axis.

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Air pressure is caused by the:

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The differences between northern and southern hemisphere circulation patterns is strongly influenced by differences in:

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In the northern hemisphere, air flow in a cyclone moves in a _________.

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The changing weather conditions of monsoon circulation are associated with shifts in the position of the:

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In the northern hemisphere, cyclonic winds spiral inwards in a clockwise direction.

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Pressure gradients in the upper troposphere result from sloping isobaric surfaces.

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Mountain breezes occur during the night as cold, dense air flows down mountainsides towards valleys.

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Which of the following is not a characteristic change associated with El Niño conditions?

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The high-speed air flow in narrow bands within the upper-air westerlies are known as _______.

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Surface ocean currents in the northern hemisphere tend to flow:

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