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The Clausius-Clapeyron relationship leads us
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to the concept of relative humidity. Relative
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humidity
is defined as the ratio of the amount
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of water vapor in the air to the amount of
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water vapor that air would hold if it were
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saturated. So completely
saturated air has a
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relative humidity of 100%.
If the air has half
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as much water vapor as it can hold, the
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relative
humidity is 50%.
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