1. Science Thoughts 11/6
What are the two ways that water becomes a gas in the atmosphere? Evaporation and Transpiration

2. Atmosphere and Weather
1.1 Composition and Layers of the Earth’s Atmosphere
1.6 Air Quality
1.2 Water Cycle, Precipitation, Clouds
1.5 Winds
1.3 Air Movement and Patterns
1.4 Weather Prediction
Severe Weather Project

3. Today in class
Pretest Water Cycle (3:35)

5. Precipitation
Water falls to the earth from clouds. Mainly as rain, but sometimes as snow and hail.
This is called precipitation.

6. Transpiration
Transpiration is the process by which plants lose water out of their leaves. 
Transpiration gives evaporation a bit of a hand in getting the water vapor back up into the air.

7. Condensation Transpiration Precipitation Evaporation
The Clouds form
Transpiration
The movement through plants
Precipitation
The rain falls
Evaporation
The vapor rises

8. Types of precipitation
(2:49)

9. Science Thoughts 11/7
In what conditions does precipitation fall as hail? Ice pellets in the cloud, move up and down getting bigger, then falls to earth.

10. How Clouds Form, Humidity Notes and Relative humidity calculations
Today in class
How Clouds Form, Humidity Notes and Relative humidity calculations

11. Humidity

12. Humidity
We already know that evaporation allows water to change into a gas and rise into our atmosphere. Eventually, it will condense into clouds when cooler temperatures are near. Well, what happens if the water vapor stays close to the ground where we are?
We use the term humidity to describe the evaporated water or water vapor in the air.

13. Humidity
Humidity can vary from place to place. The amount of water vapor that air can hold depends on temperature. The warmer the air, the more water vapor it can hold. Think about it, warm air is less dense so it has more room for water vapor.
High Humidity Low Humidity

14. Saturation
When the air is holding as much water vapor as possible at a certain temperature it has reached saturation. Think about a sponge, at some point it can no longer hold any more water. Well, the air has its limits too and the deciding factor is the temperature. The temperature at which this saturated air starts to condense onto surfaces or into precipitation is called the dew point.

15. Dew and Fog
Early in the morning, the air temperature usually cools, which allows water to condense. When this cooling and condensing causes water to form on grass and other surfaces, we call it ________. If there is enough water vapor that condenses you can get clouds close to the ground which are called __________.
Dew Fog

16. Clouds
Similar to dew forming on grass, water vapor must have something to condense on to form clouds in the upper layers of the troposphere. As water vapor rises into cooler air, it condenses on dust and other particles. The water drops and ice crystals are so light, they stay afloat and collect more water forming clouds. The droplets/crystals continue to stay aloft until they become too heavy and fall as precipitation.

18. One final aspect of humidity that we are probably all familiar with is relative humidity which measure how much water vapor is actually there compared to how much water vapor air can actually hold. Think about your grade on a test. Your grade is a comparison of how many you got right to how much you could have earned. So, an 86% means you got 86 out of 100 possible points. Relative humidity is similar. 86% relative humidity means the air is holding 86% of the water it could hold at that particular temperature. The warmer the air, the more water vapor it can hold.

20. Sling Psychrometer
Relative humidity is measured with a sling psychrometer. It compares two thermometers, one with a dry bulb and one with a wet bulb. As water evaporates from the wet bulb, it cools the thermometer. When you compare the two thermometers, the bigger the temperature difference, the less humid the air is because humid air doesn’t have a lot of room for water to evaporate. You need to know the temperature difference and the dry bulb reading in order to calculate relative humidity.

22. Science Thoughts 11/8
What causes the air masses to rise and fall in the atmosphere? Density of the air changes with temperature.

23. Read and discuss Article
Today in class
Read and discuss Article

24. Science Thoughts 11/9
When calculating relative humidity, why does the thermometer with the wet wick change temperature while the one without the wick does not? When water evaporates, it takes energy with it and therefor the thermometer will show a cooler temperature.

25. I WONDER… WISER PROJECT INTRODUCTION
Today in class
I WONDER… WISER PROJECT INTRODUCTION