PurposeTo observe the temperature, dew point, and relative humidity over a 24-hour period. OverviewIn this activity, students will measure the temperature, dew point, and relative humidity at Selva Verde for 24 hours. Students will then examine the data and discuss the reasons for any changes or abnormalities that occur. Background InformationHumidity is a measure of the water vapor in the air. As water molecules evaporate, the humidity of the air increases. Certain climate regions on earth, such as deserts and the Arctic, have very low humidity, while other regions, such as tropical rainforests, have moderate to high humidity. In general, the amount of water vapor that a given volume of air can hold increases as the temperature increases. A higher temperature allows more water to evaporate. As the temperature goes down, the amount of water vapor in the air goes down because the vapor can condense into a liquid, dropping the humidity. EquipmentData Collection Procedure 1. Plug the PASPORT Humidity/Temp/Dew Point Sensor into the port on the GLX.
Equipment Setup:1. Place the GLX and Humidity/Temp/Dew Point Sensor outside in an area where it will not be exposed to water or direct sunlight.Record Data:1. Press s to begin recording data.2. Allow the GLX to collect data for 24 hours. 3. Press s to stop recording data. Data Analysis1. From the Home screen, press F to access the Graph display. Conclusions and Extensions
1. Compare the graph of Temperature vs. Time with the graph of Relative Humidity vs. Time. How does a change in temperature affect relative humidity? Back to Costa Rica Summary -- October 2002
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