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Pattern of pressure in the eastern and western Pacific ocean.

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Event where the central and eastern Pacific ocean has colder temperatures.

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Event where the eastern Pacific ocean gets warmer during December or January.

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Chinook wind that occurs in southern California

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Winds created when strong pressure gradients are present in mountainous areas.

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Cool air that moves downward in a valley.

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Warm air rising upwards in a valley.

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The opposite of sea breeze. Happens at night.

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When cool air from water travels to warmer land. Happens at day.

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Pressure gradients create these small scale winds.

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Monsoons happen when winds travel in opposite directions in winter and summer.

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Location where cold air moves towards the equator.

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Belt formed by warm and cool winds reacting with each other.

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Area of low pressure near the Arctic and Antarctic Circle latitude.

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Cool trade winds that move to the east.

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The remaining trade winds that travel poleward.

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The Coriolis effect deflects air to make this type of wind.

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Center zone where dry air surrounds the 30° latitude in the north and south.

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Region where winds from north to south merge at low air pressure.

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Area where moist air has great amounts of precipitation.

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We can have an indication of whether if pressure is rising, falling, or steady.

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Wind that flows inward due to friction.
Divergence is wind that flows outward.

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Region with low air pressure.
Highs are high pressured areas.

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Air that moves from 120 to 240 kilometers per hour from west to east.

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Upper winds that are parallel to isobars.

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All objects moving in the northern hemisphere deflect to the right. Objects deflect in the southern hemisphere.

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Spaces in isobars measuring pressure.

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Lines on weather maps connecting places of equal air pressure.

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Air that moves horizontally.

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Machine that records air pressure as it changes with time.

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Barometer that changes form due to air pressure.

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It is a glass tube with mercury that measures air pressure.

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The weight of air acting on an object.