Originally Posted by KevinF
Ok calling all Epic meteorologists. One thing I've always noticed is that Colorado "cold" doesn't feel that cold. i.e., I was walking around Silverthorne the other week when it was -6F in a light sweater and thin fleece glove liners and felt perfectly comfortable. If it's -6F here in New England, I dread getting out of the car as it hurts to breathe. Why is that -- i.e., why does Western cold air feel so much warmer than Eastern cold air? I've heard it's the amount of moisture in the air, but really -- how much moisture is there in the air when it's below zero Fahrenheit?
humidity, moisture content of the atmosphere, a primary element of climate. Humidity measurements include absolute humidity, the mass of water vapor per unit volume of natural air; relative humidity (usually meant when the term humidity alone is used), the ratio of the actual water-vapor content of the air to its total capacity at the given temperature; specific humidity, the mass of water vapor per unit mass of natural air; and the mixing ratio, the mass of water vapor per unit mass of dry air. Absolute humidity finds greatest application in ventilation and air-conditioning problems. Humidity is measured by means of a hygrometer. The rate of evaporation decreases as the moisture content of the air increases and approaches saturation. In addition, the saturation point (moisture-holding capacity of the air) increases rapidly as the temperture of the air rises (see dew). Thus cold air, while its moisture content is necessarily quite low (low absolute humidity), may be almost saturated with respect to the maximum amount of water vapor it is capable of holding (high relative humidity). Cold air with high relative humidity “feels” colder than dry air of the same temperature because high humidity in cold weather increases the conduction of heat from the body. Conversely, hot air attended by high relative humidity “feels” warmer than it actually is because of an increased conduction of heat to the body combined with a lessening of the cooling effect afforded by evaporation. On the other hand, a low relative humidity “modifies” the effect of temperature extremes on the human body. Humidity decreases with altitude
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