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Just as increasing the temperature decreases relative humidity, decreasing the temperature increases the relative humidity. If you keep on decreasing the temperature without changing the air’s moisture content significantly, eventually you’ll reach 100 percent relative humidity, and then water vapor will start to condense to form dew. The temperature when this happens is called the dew point, and this phenomenon is what causes dew to form on the grass on chilly mornings.<\/p>\n<\/div>\n","protected":false},"excerpt":{"rendered":"
Meteorologists measure or talk about humidity in a number of different ways. One of the key measurements they use is … <\/p>\n
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