Exam 5: Global Atmospheric and Oceanic Circulation

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Geostrophic winds flow parallel to isobars in the upper atmosphere.

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An anticyclonic flow in the northern hemisphere is illustrated in part _____ of this figure. An anticyclonic flow in the northern hemisphere is illustrated in part _____ of this figure.

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The Coriolis effect is caused by:

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In the Asiatic monsoon:

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There is a permanent __________ centered over Antarctica.

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An anticyclone is a center of _____ pressure.

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In an anticyclone located in the northern hemisphere winds :

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The Coriolis effect deflects winds and ocean currents to the right in the southern hemisphere.

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A cyclone is a:

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The Coriolis effect is caused by the ________ of the Earth.

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In the northern hemisphere, anticyclonic winds spiral outwards in a clockwise direction.

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Pressure gradients occur at right angles to isobars.

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In warm areas, pressure tends to ___________ with height than in cold areas.

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Rossby waves form in the westerlies marking the boundary between cold polar and warmer tropical air.

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Land breezes flow from land to water during the night.

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The gulf stream carries __________ water to the _________.

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

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The direction of wind motion on this figure is labeled: The direction of wind motion on this figure is labeled:

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The device shown in this figure is called a: The device shown in this figure is called a:

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The southern hemisphere subtropical high pressure belt is characterized by two large anticyclones centered over the oceans.

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