occurs when mountains act as barriers to the flow of air, forcing the air to ascend
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What happens when the air from orographic liftng cools adiabatically?
clouds and precipitation may result, rain generally falls in windward side of mountains, leeward side tends to be dry
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What happens during frontal wedging?
the front forces warm up over to cooler air, warm air cools and condensation occurs
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What is a front? (frontal wedging)
the boundary between two adjoining air masses having contrasting characteristics
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What is convergence?
when air flows together and rises
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What is localized convective lifting?
occurs where unequal surface heating causes pockets of air to rise becuase of their buoyancy
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What are the characteristics of stable air? (CHANGE QUESTION)
when air is forced upwards then sinks back down on it’s own, stable air remains in its original position, unstable air rises
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How do you tell if air is stable?
by measuring the temperature of the atmosphere at various heights
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What is the rate of change in air temperature with height called?
the environmental lapse rate
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What is a radiosonde?
device used to measure temperature, humidity, pressure, and other characteristics at various heights
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What is a temperature inversion?
it occurs in a layer of limited depth in the atmosphere where the temperature increases rather than decreases with height, it’s the most stable condition of the atmosphere
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What are condensation nuclei?
tiny bits of particulate matter that serve as surfaces on which water vapor condenses when condensation occurs in the air
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What are clouds?
visible mixture of water droplets and ice crystals in the atmosphere
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How are clouds classified?
the basis of their form (shape) and height
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What are the three basic cloud shapes?
cirrus (high, white and thin)
cumulus (clouds that consist of rounded individual cloud masses)
stratus (clouds best described as sheets or layers that cover much or all o the sky, no distinct cloud units)
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What is fog?
a cloud iwht its base at or very near the ground
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What is the Bergeron process?
a theory that relates the formation of precipitation to supercooled clouds, freezing nuclei, and the different saturation levels of ice and liquid water