Background Information

What is Relative Humidity?

Relative Humidity is a measurement of the moisture in the air. It is expressed as a percentage. Relative humidity describes the percentage of water vapor in the air in relation to the total amount of water vapor that the air can hold. The amount of water vapor that the air can hold changes as the temperature changes.

Relative humidity affects how you feel on a warm day. If the relative humidity is low on a hot day, say 90-degrees, then it is easy for the body to cool itself by perspiring. However, when the relative humidity is high, the air does not want take any additional water vapor, so it's more difficult for your body to cool itself by perspiring.

What is Evapotranspiration?

Evapotranspiration (ET) is the process by which water returns to the atmosphere due to evaporation and plant transpiration. Evaporation is the process by which water molecules go from the liquid state to the gas form, known as water vapor. Transpiration is the process in which plants release water molecules through the stomas of their leaves. The rate of evapotranspiration is determined by a complicated calculation based on temperature, solar radiation, humidity, and wind conditions. It is calculated for a reference plant crop, such as alfalfa. At Jackson Bottom Wetlands Preserve, there are several different plant communities. So the evapotranspiration rate should be used for general understanding and for comparing one time with another.

Links to Satellite & Radar Images

Satellite Image from NOAA
Radar Image from Unisys Corp

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