Ed
Wehling
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Topic 4: Water vapor in the atmosphere
Please note: the questions
listed are not the only items that you need to know. The questions point
out basic information to help understand some topics, some concepts that
may not be obvious to all students, and some of the more difficult
concepts.
Saturation, Unsaturation,
Supersaturation D2L Explanation
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If we take a
close-up look at the surface of liquid water, what is
happening in terms of evaporation and condensation?
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How can you describe
the relative amount of evaporation and condensation if the
atmosphere is unsaturated, saturated, or supersaturated?
Saturation curve
Humidity
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Vapor pressure and
mixing ratio
--How do these describe the amount of water vapor in the
air?
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Relative humidity
--How does RH describe the amount of water vapor in the air?
--Applications
--Change in RH as days warms, and as night cools
--Why does your house feel very dry inside in the
winter?
--Why does a humidifier make your house more
comfortable in the winter?
--Why does your basement feel more humid than the
upstairs in the summer?
--Why does the air feel drier when you run the
a/c?
--What are conditions like if the RH=100%
--Relative
humidity interactive
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Dewpoint
--How can the atmosphere cool to the dewpoint?
--What happens to the RH of a parcel of air with RH<100% if
you lift it?
--What happens to the RH of a parcel of air with RH=100% if
you lift it?
--Describe how the atmosphere can reach the dewpoint if two
parcels of air mix together.
--What happens if the air temperature cools below
the dewpoint?
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How are vapor
pressure, mixing ratio, relative humidity, and dewpoint
different from each other? How are the similar? [To make
this easier, just pick 2 to start. How are they different?
Similar?]
How does the air get
saturated?
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