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Includes: Jason-Mission 2 - Fog, Dew, Frost/Water Vapor on Air, and p.28-31notes

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Question
Answer
phase change   change in a solid, liquid, or gas, to another state  
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melting   change from solid to liquid  
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evaporation   change of liquid to gas  
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sublimation   change of solid to gas w/o the liquid state  
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condensation   change of gas to liquid  
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freezing   change of liquid to solid  
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deposition   change of gas to a solid w/o the liquid state  
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transfer   any gain or loss of heat  
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fog   low-lying stratus clouds; at ground level; formed by condensation  
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dew   water vapor condenses to liquid on objects near ground; ground cold; air temp below dew pt. temp = not enough energy to keep water as vapor  
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frost   water vapor into ice (deposition) on objects near ground  
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humidity   amount of water vapor in air; higher temp = more energy to evap. water and to keep more water as vapor; higher temp = higher humidity possible (depends on water available); ave. humidity = water 2-3% of molecules in air  
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absolute humidity   mass of water vapor per volume of air (g/m cubed)  
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relative humidity   ratio in % that compares water vapor in air to total amount the air could hold at that temp.  
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dew point   temp. at which water vapor loses enough energy to condense (meas. in degrees)  
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