At colder temperatures, the air can hold more water because the air molecules are closer together and thus more capable

At colder temperatures, the air can hold more water because the air molecules are closer together and thus more capable of supporting water.

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  1. At -40 °C (-40 °F), however, it can hold no more than 0.2 percent. When a volume of air at a given temperature holds the maximum amount of water vapour, the air is said to be saturated. Relative humidity is the water-vapour content of the air relative to its content at saturation.

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