1. Bell work
Observe two glasses of water. One is filled with ice water, and one is filled with warm water.
Why do water droplets form on the outside of the cold glass?
Where do the water beads come from?
Why don’t the water beads form on the warm glass?
Have you seen this happen before on other containers? On your soda can? On a coffee cup or a soup bowl?

2. Weather Introduction

3. Objectives for today! Explain how water moves through the water cycle.
Describe how relative humidity is affected by temperature and levels of water vapor.
Describe the relationship between dew point and condensation.

4. A quick tongue twister!
Whether the weather be hot, or whether the weather be cold. We’ll weather the weather, whatever the weather whether we like it or not.

5. What is weather?
Weather is the condition of the atmosphere at a certain time and place.
The condition of the atmosphere is affected by the amount of water in the air.

6. How is that different from Climate?
Climate is the condition of the atmosphere over a long period of time.
Like a season.
Remember weather is a one particular time and place.

7. What is the Water Cycle?
The water cycle is the continuous movement of water from sources on Earth's surface—such as lakes, oceans, and plants—into the air, onto and over land, into the ground, and back to the surface.

8. The Water Cycle- A water cycle is the way water moves from the air to land and back again.

9. Condensation
The water vapor rises into the air, cools, and condenses into tiny droplets of water.
The drops of water come together to form clouds.
Water Cycle
Precipitation
Evaporation is when a liquid changes to a gas.
The water drops become heavy and fall as rain, sleet, snow, or hail.
The sun’s heat makes water evaporate into water vapor.
The rain falls or snow melts and flows to rivers, lakes, and oceans.

10. What is Humidity?

11. Humidity
As water evaporates from lakes, oceans, and plants, it becomes water vapor, or moisture in the air.
Humidity refers to the amount of moisture (water vapor) in the surrounding air.
As water evaporates and becomes water vapor, the humidity of the air increases.

12. The air's ability to hold water vapor changes as the temperature of the air changes.
As the temperature of the air increases, the air's ability to hold water vapor also increases.

13. Objectives for today! Explain how water moves through the water cycle.
Describe how relative humidity is affected by temperature and levels of water vapor.
Describe the relationship between dew point and condensation.

14. Relative Humidity
Relative Humidity is a measure of the amount of moisture in the air compared with the amount of moisture the air can hold.
Relative humidity is expressed as a percentage of how much moisture the air could possibly hold at the temperature it happens when you measure it.

15. Relative Humidity
When air holds all of the water that it can at a given temperature, it is said to be saturated. Saturated air has a relative humidity of 100%.
If air holds all the water vapor it can, it is at 100% RH and is said to be “saturated.”

16. We are very sensitive to humidity
We are very sensitive to humidity. Sweating keeps our body cool and maintain its current temperature.
If the air is at 90% relative humidity, sweat will not evaporate into the air. As a result, we feel much hotter than the actual temperature when the relative humidity is high.
If the relative humidity is low, we can feel much cooler than the actual temperature because our sweat evaporates easily, cooling the body.

17. Relative Humidity
Two factors that affect relative humidity are amount of water vapor and temperature.
At constant temperature and pressure, as the amount of water vapor in air changes, the relative humidity changes.
The more water vapor there is in the air, the higher the relative humidity is.
If the amount of water vapor in the air stays the same but the temperature changes, the relative humidity changes.
The relative humidity decreases as the temperature rises and increases as the temperature drops.

18. Measuring Relative Humidity
A psychrometer (sie KRAHM uht uhr) is an instrument that is used to measure relative humidity.
A psychrometer consists of two thermometers, one of which is a wet-bulb thermometer. The bulb of a wet-bulb thermometer is covered with a damp cloth.
The other thermometer is a dry-bulb thermometer.

19. Measuring RH
Using the difference between the two (“wet bulb depression”) and charts allow calculation of the relative humidity.
“Hygrometers” also measure RH
[Sources: and

20. Measuring Relative Humidity
As air passes over the wet-bulb thermometer, the water in the cloth evaporates.
As the water evaporates, the cloth cools.
If the humidity is low, the water will evaporate more quickly and the temperature reading on the wet-bulb thermometer will drop.
If the humidity is high, only a small amount of water will evaporate from the cloth of the wet-bulb thermometer and the change in temperature will be small.

21. Measuring Relative Humidity
The difference in temperature readings between the thermometers indicates the amount of water vapor in the air.
The larger the difference between the two readings is, the less water vapor the air contains and thus the lower the humidity is.

22. Wet- and Dry Bulb Psychrometer Psychrometric Chart.
If the difference between wet and dry bulb is 6º F and the temperature is 72º F (dry bulb), then the RH is 54%.

23. Objectives for today! Explain how water moves through the water cycle.
Describe how relative humidity is affected by temperature and levels of water vapor.
Describe the relationship between dew point and condensation.

24. What is Condensation?
The water came from the surrounding air, and droplets formed as a result of condensation.
Condensation is the process by which a gas, such as water vapor, becomes a liquid.
The air must be saturated, which means that the air must have a relative humidity of 100%.
Condensation occurs when saturated air cools.

25. Air can become saturated when water vapor is added to the air through evaporation.
Air can also become saturated when it cools to its dew point.
The dew point is the temperature at which a gas condenses into a liquid. At its dew point, air is saturated.

26. The ice in the glass of water causes the air surrounding the glass to cool to its dew point.
Before water vapor can condense, though, it must have a surface to condense on.

27. Objectives for today! Explain how water moves through the water cycle.
Describe how relative humidity is affected by temperature and levels of water vapor.
Describe the relationship between dew point and condensation.