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The instrument most commonly used to determine wind direction

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A chinooklike wind that occurs in the southern California

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Warm, dry winds sometimes move down the eastern slopes of Rockies

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Cooler air is denser than warm air, it drains down slope into the valley.

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Glides up along the slope

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Seasonal tendencies

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Cooler air over the water moves toward the warmer land

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Are small scale winds produced by a locally generated pressure gradient

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seasonal changes in wind direction.

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As the westerlies move pole ward, they encounter the cool polar easterlies in the region of the sub polar low.

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Some of the air travels equator ward and is deflected by the Coriolis effect, producing the reliable trade wind

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The center of this zone of subsiding dry air

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This region of low pressure is a zone where winds from the north and south converge

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Near the equator, the rising air is associated with the pressure zone.

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Are high pressure centers

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Are center of low pressure

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The most prominent featured of upper level flow

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Upper air winds generally

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The direction deviates as a result of earth rotation

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The spacing of isobars indicates the amount of pressure change occurring over a given distance.

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Measurements are shown on surface weather maps

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Provides s continuous record of pressure changes with the passage of time

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Makes a continuous record of air pressure.

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Vertical motion is, far more air moves horizontally, the phenomenon

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A smaller tube to measure air pressure

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The measure of air pressure date

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The pressure extend by the weight by the weight of air above.