Have you ever noticed that on some summer days, the air is so humid that it feels like you can barely breathe? This is because the air is holding a lot of water vapor, and when the temperature drops, some of that water vapor condenses into tiny droplets of water, which we call dew. The temperature at which this happens is called the dew point.
The dew point is an important meteorological concept because it tells us how much moisture is in the air and how likely it is to rain, fog, or snow. It is also used to calculate the relative humidity, which is a measure of how humid the air feels.
Now that we know what the dew point is, let's take a closer look at how it relates to weather and climate.
What is Dew Point
The dew point is the temperature at which water vapor in the air condenses into liquid water.
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The dew point is an important meteorological concept because it tells us how much moisture is in the air and how likely it is to rain, fog, or snow.