Weather Activities - Partnerships for Environmental …peer.tamu.edu/NSF_Files/DLC750_All about the...

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Weather Activities Sea and Land Breezes Lab Activity…………………….page 2 Cloud in a Jar Lab Activity……………………………..page 6 Make Your Own Barometer…………………………….page 9 Make Your Own Snowflake…………………………….page 12 Acid Rain Lab Activity…………………………………page 16

Transcript of Weather Activities - Partnerships for Environmental …peer.tamu.edu/NSF_Files/DLC750_All about the...

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Weather Activities

Sea and Land Breezes Lab Activity…………………….page 2

Cloud in a Jar Lab Activity……………………………..page 6

Make Your Own Barometer…………………………….page 9

Make Your Own Snowflake…………………………….page 12

Acid Rain Lab Activity…………………………………page 16

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Sea and Land Breezes

Activity Summary: Students may conduct this experiment in groups of three or four to help them understand the movement of air over land and water. They will be able to explain what happens when air is heated or cooled. They will discover how temperature of the air affects air pressure. Using what they learned in the experiment, the students will be able to explain how temperature and changes in air pressure causes wind and summarize why the direction of the wind at the seashore changes.

Subject: Science: Unifying Concepts and Processes, Earth Science, Science as Inquiry

Grade Level: Target Grade: _6th__ Upper Bound: _7th__ Lower Bound: _5th__ Time Required: _30-45 minutes__

Activity Team/Group Size: _3-4__

Reusable Activity Cost Per Group [in dollars]: _$20__

Expendable Activity Cost Per Group [in dollars]: _$2__

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Activity Introduction / Motivation: Ask the students if they have ever been to the beach. Do they remember which way the wind was blowing? Ask if anyone might know why the wind blows in a certain direction. Then give the students this brief introduction:

Wind is air in motion. On a sunny day, warm air rising from land heated by the sun flows toward the cooler water when the air sinks. The cooler air then rushes in toward land again to replace the warm air that is rising. This cycle continues as long as the daytime heating continues from the sun. Since air moves inland from the water, the wind is called a sea breeze. At night, the opposite cycle occurs. Since the land cools more quickly than water, air over the warmer water rises and flows toward cooler land where the air sinks. This reverse cycle of wind blowing out to sea is called a land breeze.

Materials List: 2 small containers, such as 200 mL beakers per groupRoom-temperature waterSand or potting soil2 thermometers per groupRing standString1 lamp with 60 W or higher bulb (if it is a bright day and have access to outdoors, may

substitute lamp for sunlight)

Activity Plan:

1. Fill one container with room-temperature potting soil or sand.2. Place the bulb of one of the thermometers in the soil to a depth of 1 inch.3. Fill the other container with room-temperature water.4. Use string to tie the thermometer to a ring stand. The bulb of the thermometer should hang

in the water to a depth of 1 inch.5. Allow the thermometers to adjust to the temperatures of the soil and water. Record the

temperature of each on a piece of paper.6. Place the lamp directly above the containers of soil and water so that it is an equal distance

from each.7. Turn the lamp on and begin recording the temperature from the 2 containers once every

minute.8. After 10 minutes, turn the lamp off and continue recording the temperatures every minute

for 10 more minutes.9. Graph the information you recorded.

Assessment: 1. Did the soil or water absorb heat faster? How can you explain this?

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2. Which substance lost heat faster? How do you explain this?3. According to this experiment, what would happen to the land and water during a sunny day

at the beach?4. What would happen to the land and water at the beach at night?5. Which would be hotter during the day, the air above the land or the air above the sea?6. What happens to air when it is heated?7. What happens to air when it is cooled?8. During the day at the beach, would the wind blow from the sea to the land or from the land

to the sea? Why?9. Which way would the wind blow at night? Why?

Learning Objectives: TEKS 6th Grade Science Objectives:6.2 (B) Collect data by observing and measuring6.2 (E) Construct graphs, tables, maps, and charts to evaluate data6.4 (A) Collect, analyze, and record information using scientific tools6.14 (C) Describe components of the atmosphere and its role in weather change

Background & Concepts for Teachers: During the day, the sun heats both land and water. Because of its lower specific heat value (the heat in calories required to raise the temperature of one gram of a substance one degree Celsius), land heats faster and cools more rapidly than water. Since land takes in more heat and releases it more rapidly than does water, the air above land heats more rapidly than the air above water. The heated air above land rises, which creates an area of low pressure. The air above the sea is cooler, creating an area of higher pressure. The cooler air in the area of high pressure above the sea moves to the area of low pressure over land. This is called a "sea breeze" because the breeze is coming from the sea.At night, land continues to cool more rapidly than water, which means the sea is now warmer than the shore. Now the air above the sea becomes warmer than the air above the land. The warm, rising sea air creates an area of low pressure, and the cooler air above land creates an area of higher pressure. The air again moves from higher (over the land) to lower (over the sea) pressure. This breeze is called a "land breeze."

Activity Extensions: This activity can be used in conjunction with other activities in order to explain in more depth the impact of wind and convection current on temperature.

Safety Issues: ___ If the thermometers are glass, remind the students to be careful with them. ___ If using a lamp for a heat source, remind the students that the bulb gets very hot.

Activity Scaling:

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___ If you want to shorten the activity because of time constraints, you could have the students only record the temperature of the water and soil when the temperature is rising after 3, 6, 9, and 12 minutes. Discuss with the students why the temperature of the soil rose faster than the water.

References: http://www.carolina.com/earth/sea_breeze.asphttp://archive.ncsa.uiuc.edu/edu/RSE/RSEred/Lesson3Activity2.html

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Cloud in a Jar

Activity Summary: Where does rain come from? Most people realize that it has something to do with clouds, but what causes clouds to form in the first place? When rising water vapor rises, it cools and condenses. But temperature is not the only factor that determines how fast a cloud forms. In this experiment, students will discover if dust present in the air has an effect on cloud formation as well.

Subject: Science: ___ Unifying Concepts and Processes, Earth and Space Science, Science as Inquiry

Grade Level: Target Grade: _6th__ Upper Bound: _7th__ Lower Bound: _5th__ Time Required: _ approximately 20 minutes__

Activity Team/Group Size: _2-3__

Reusable Activity Cost Per Group [in dollars]: _$3.00__ .

Expendable Activity Cost Per Group [in dollars]: _$3.00__

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Activity Introduction / Motivation: Write on the board “April Showers Bring May Flowers”. Then ask the students, what brings April showers? Most people realize that it has something to do with clouds, but what causes clouds in the first place. Next, have the students form a hypothesis on whether dust in the air helps clouds form.

Materials List: 2 clean, large glasses or jars of the same size (pickle or mayonnaise jars work well) 2 large (12-inch) latex balloonsscissorswarm watersome chalk dust or smoke (from erasers)4 to 6 large thick rubber bandsred markera freezer, refrigerator, ice chest, or cold day

Activity Plan: 1. Cut off the ends of the latex balloons, and have the dusty erasers ready.2. Pour about 50 mL of warm water into the bottom of each jar. 3. Take one cut balloon and stretch it completely over the top of the first jar. Wrap 2 or 3 rubber bands around the top edge to make sure the balloon makes a tight seal.4. Over the second jar, clap the dusty chalkboard eraser so the chalk dust goes into the bottle. Quickly seal up the second jar the same way as the first. Using the red marker, label the jar with an X.5. Place both jars in a cool place for 10 minutes.6. When the time is up, take the two jars out and compare the insides.

Assessment: Ask the students to compare the cloud formation to the presence or absence of dust. What relationship, if any, do they notice?How did the results compare with their hypothesis?

Learning Objectives: 6.14 (C) Describe components of the atmosphere and its role in weather change

Background & Concepts for Teachers: When rising water vapor cools due to changes in temperature and air pressure, it needs a surface on which to condense. These surfaces are small particles of dust, smoke, or salt in the air. Another name for these particles is condensation nuclei. They are most abundant in the lower troposphere over urban areas, and are quite small relative to the size of a raindrop. The troposphere is the lowest layer of the atmosphere, and contains approximately 95% of the mass of air in the Earth’s atmosphere. It extends about 10 to 15 kilometers above the Earth’s surface, and all weather processes take place here.

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Activity Extensions: Have the students write a short answer to the following question: How might this experiment help meteorologists predict the weather?

Troubleshooting Tips: If it is difficult to see the “cloud”, try darkening the classroom and shining a flashlight at the top of the bottle.

Activity Scaling: This lab may also be done as a class demonstration to shorten the time.

References: This activity was modified from the following website: http://teacher.scholastic.com/dirt/weather.htm

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Make Your Own Barometer

Activity Summary: A barometer is a weather instrument that measures atmospheric pressure. Generally, a

drop in pressure indicates a storm is approaching, while a rise in pressure is indicative of good weather. In this experiment, students will make simple barometers and record data over the course of a week to determine the relationship between air pressure and weather.

Subject: Unifying Concepts and Processes, Earth and Space Science, Science as Inquiry

Grade Level: Target Grade: _6th__ Upper Bound: _7th__ Lower Bound: _5th__ Time Required: _~30 minutes (with data collection over 5 days)__

Activity Team/Group Size: _3-4__

Reusable Activity Cost Per Group [in dollars]: _$3.00__

Expendable Activity Cost Per Group [in dollars]: _$3.00__

Activity Introduction / Motivation: Have the students make a hypothesis on the relationship between air pressure and weather.

Materials List: glass or beaker with straight sides12 inch ruler

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tapestick of chewing gumone foot of clear plastic tubingwater

Activity Plan: 1. Stand the ruler in the glass and hold it against one side. Tape the ruler to the inside of the glass, while making sure the numbers are visible.2. Stand the plastic tubing against the ruler in the glass. Make sure the tubing is not touching the bottom of the glass by positioning the tubing ½ inch up the ruler. Secure the tubing by taping it to the ruler.3. Chew the stick of gum so it is soft. 4. Fill the glass halfway up with water. Use the plastic tube like a straw and draw water about halfway up the tube. Quickly move the gum over the top of the tube to seal it. 5. Make a mark on the ruler to record where the water level is in the tube. For the next five days, keep the barometer in a relatively safe place (on a windowsill or protected area outside) and chart the water level in the tube.

Assessment: Have the students answer the following questions:1. Was the air pressure most often high or low?2. Compare the type of weather to the amount of air pressure. What kind of relationship, if any, do you notice?3. How did the results compare with your hypothesis?4. What conclusions about the relationship between air pressure and weather can you draw based on this experiment?5. If the barometer shows high pressure, what kind of weather might you expect?6. If the barometer shows low pressure, what kind of weather might you expect?

Learning Objectives: TEKS 6th Grade Science Objectives:6.2 (B) Collect data by observing and measuring6.2 (E) Construct graphs, tables, maps, and charts to evaluate data6.4 (A) Collect, analyze, and record information using scientific tools6.14 (C) Describe components of the atmosphere and its role in weather change

Background & Concepts for Teachers: The water in the tube rises and falls because of air pressure exerted on the water in the glass. As the air presses down (increased atmospheric pressure) on the water in the glass, more water is pushed into the tube, causing the water level to rise. When the air pressure decreases on the water in the glass, some of the water will move down out of the tube, causing the water level to fall. This change in barometric pressure corresponds with forecasting weather. Decreasing air pressure often indicates the approach of a low pressure area, which often brings clouds and precipitation. Increasing air pressure often means that a high pressure area is approaching, bringing with it clearing or fair weather.

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Safety:You must stress that students are not allowed to eat in the science lab at any time, and this will be the only time they will be able to chew gum in the classroom!

Activity Extensions: To extend this activity, have the students check the barometer periodically and then predict the forecast for the next day based on low or high pressure. Another suggestion is to have the students explore the relationship between pressure and elevation by researching weather forecasts in regions of high and low elevation.

References: This activity was modified from the following website: http://www.fi.edu/weather/todo/barometer.html

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Make Your Own Snowflake

Activity Summary: If there are no snowflakes on the ground, cook one up in the lab! Use this experiment as a fun, inexpensive activity that brings physical science concepts into earth science curriculum. This experiment introduces students to crystal formation and structure, precipitation, solutions, and safe lab practices. It works equally well as a demonstration or as a hands-on activity for middle school students.

Subject: Science: Earth and Space Science, Science as Inquiry, Science and Technology, Physical Science

Grade Level: Target Grade: _6th__ Upper Bound: _7th__ Lower Bound: _5th__ Time Required: __45 minutes to an hour (must sit overnight)_

Activity Team/Group Size: _2-3__

Reusable Activity Cost Per Group [in dollars]: $35

Expendable Activity Cost Per Group [in dollars]: $8

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Activity Introduction / Motivation: Start the experiment by asking the students introductory questions about snow. What makes up snow?What causes snow?Why are no two snowflakes the same?Quickly provide some background information on snow.

Background & Concepts for Teachers: What makes up snow? Snowflakes are made up of many ice crystals clumped together that form when water vapor changes directly from a gas to a solid. In very cold air, water molecules cling on to particles, forming tiny ice crystals. As more water molecules freeze onto the crystal, they join at angles to form a unique six sided structure. Nearly all snow crystals have six sides, but they vary in shape. The ice crystals also contain tiny bits of dirt that the wind has blown around the atmosphere (scientists even believe some specks come from space). These ice crystals cluster together to form individual snowflakes. One snowflake can be made up of anywhere between two and 200 separate snow crystals. What causes snow?Snowflakes come from clouds, which are really just big clusters of water vapor. This water vapor scatters and forms ice crystals or rain in the clouds, depending on the temperature. The temperature must be below zero degrees Celsius (32 degrees F) for the water to turn into ice crystals. As the crystals grow, they fall with increasing speed. They may collide with one another to create snowflakes. The particles of snow may vary in size, from crystals almost invisible to the unaided eye to snowflakes one inch or more in diameter

Why are there no two snowflakes that are the same?Factors such as humidity, wind, and temperature affect the growth of each snowflake as it falls. The pattern or structure may change as it falls from the sky. A crystal needs atmospheric conditions of no hotter than -15 °C to grow. These six sided hexagonal crystals are shaped in the high clouds. In the middle height clouds, ice crystals are shaped in needle-like or flat, six sided forms. A wide variety of six sided shapes are formed in low clouds. The colder the temperature, the sharper the ice crystals are. At warmer temperatures, the ice crystals grow slower and smoother.

Materials List: (per group)500 mL glass beakerBunsen burner or hotplatering stand (if using Bunsen burner)one white pipe cleanertablespoonwooden pencil or dowel ~ 8 inches long~ 4 grams of alumsafety gogglescissorsthread

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~350 mL water

Activity Plan:

1. Put on safety goggles, and apron (if available).2. Using scissors, cut the pipe cleaner into 3 pieces of equal length.3. Create a 6-spoked figure by twisting the pieces together (see figure 1).4. Attach a piece of thread around the outer edges of the figure to form a snowflake pattern

(see figure 1). Creativity counts!5. Tie one end of a piece of thread to the center of the snowflake pattern and the other end to

the center of a wooden pencil or dowel. Adjust the length of the thread so that the pattern is suspended about 1 inch above the bottom of the beaker when the pencil or dowel is placed across the beaker's mouth (see figure 2).

6. Remove the pattern from the beaker prior to heating.7. Place the beaker on the ring stand or hotplate.8. Add 350 mL water to the beaker and bring it to a boil. Turn off the Bunsen burner or

hotplate.9. Add alum to the beaker, one tablespoon at a time, and stir until the solution becomes

saturated. It should take about 2–3 grams of alum to do this. The solution is saturated when the alum no longer dissolves but settles at the bottom of the beaker.

10. Place the pattern in the beaker and leave it undisturbed overnight.11. Pull the pattern out of the solution the following morning and you will have a 6-spoked

crystal snowflake.  

Figure 1 Figure 2

Activity Closure: Q: How were the snowflakes formed in this experiment?A: Heating the water to a boil allows it to hold much more alum in solution than it could at room temperature. As the water cools its ability to hold the alum in solution diminishes. This causes the excess alum in the solution to precipitate (form a solid) on the walls of the beaker on the snowflake pattern suspended in the beaker.

Assessment:

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1. What would take up more space, liquid water or ice? 2. If a snowflake melted on the ground and then froze again, would it retain its pattern?

Why or why not?3. What determines whether rain or snow will fall?4. If it was -15 degrees Celsius in the clouds and 45 degrees Celsius on the ground, would

ice crystals form in the clouds? Would we see them?

Learning Objectives: TEKS 6th Grade Science Objectives:6.4 (A) Collect, analyze, and record information using scientific tools6.14 (C) Describe components of the atmosphere and its role in weather change

Safety Issues: Alum is harmful if swallowed or inhaled. Tell the students not to smell it, eat it, or put the snowflake in their mouths. Review lab safety with your students before they begin work. Use caution around Bunsen burners, hotplates, and boiling water.

References: This activity was modified from the following: http://www.carolina.com/earth/snowflake.asp

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Acid Rain

Activity Summary: Acid rain is precipitation that has been made acidic by certain pollutants in the air. Acid rain falls on buildings, cars, trees, plants, and water sources. In this experiment, students will discover how exactly acid rain affects plant growth, and in turn be able to predict the detrimental effects that acid rain has on the environment.

Subject: Science: Earth and Space Science, Science as Inquiry

Grade Level: Target Grade: _6th__ Upper Bound: _7th__ Lower Bound: _5th__

Time Required: __2 weeks (recording data every other day)_

Activity Team/Group Size: This activity can be done in groups of four or as a class demonstration.

Reusable Activity Cost Per Group [in dollars]: $5.00

Expendable Activity Cost Per Group [in dollars]: $10.00

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Activity Introduction / Motivation: Ask the students if they know any way that human being affect weather. Ask if they know how different pollutants get in the air (examples include factories, power plants, exhaust from cars, trucks, buses, burning of fossil fuels, etc.) and what might be the consequences of these actions.

Materials List: (as per group or class demonstration)

4 cups or jars distilled water white vinegar measuring cups stirring spoon 2 cuttings of a philodendron plant (1 leaf and small amount of stem) 2 cuttings of a begonia or coleus plant (1 leaf and small amount of stem) notebook and pencil

Activity Plan: 1. Pour 1 teaspoon of vinegar into 2 cups of distilled water, stir well, and check the pH with either pH paper or a garden soil pH testing kit. The pH of the vinegar/water mixture should be about 4. If it is below pH 4, add a sprinkle of baking soda, or a drop of ammonia, stir well, and recheck the pH. If it is above pH 4, add a drop or two of vinegar and again recheck the pH.

2. Measure the pH of the distilled water using either pH paper or a garden soil pH testing kit. If the pH is below 7, add about 1/8 teaspoon baking soda, or a drop of ammonia, stir well, and check the pH of the water with the pH indicator. If the water is still acidic, repeat the process until pH 7 is reached. Should you accidentally add too much baking soda or ammonia, either start over again or add a drop or two of vinegar, stir, and recheck the pH.

3. Put one of the following labels on each cup or jar:-- water philodendron -- acid philodendron -- water begonia (or coleus) -- acid begonia (or coleus)

4. Pour about a cup of distilled water into the water-philodendron and water-begonia cups.

5. Pour about a cup of the vinegar/water mixture into the acid-philodendron and acid-begonia cups.

6. Put one philodendron cutting into each philodendron labeled cup, covering the stem and part of the leaf with the liquid.

7. Put one begonia cutting into each begonia-labeled cup, covering the stem and part of the leaf with the liquid.

8. Set the cups where they are not likely to be spilled and where they will receive some daylight.

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9. About every 2 days, check to be sure that the plant cuttings are still in the water or vinegar/water. You may need to add more liquid if the cups become dry.

10. After 1 week, compare the new root growth of each plant in distilled water with the new root growth of its corresponding plant in acid water. Record the results.

11. After 2 weeks, again observe the plant cuttings for new root growth, and record the results.

Assessment: Have the students graph the data they collected and discuss the effects of acid rain by answering the following questions as a class.

Did you observe any differences in physical characteristics between the acid and water plants?

Which plants had the fastest root growth?What do you think the acid did to hurt the plant?

Learning Objectives: TEKS 6th Grade Science Objectives:6.2 (B) Collect data by observing and measuring6.2 (E) Construct graphs, tables, maps, and charts to evaluate data6.4 (A) Collect, analyze, and record information using scientific tools6.14 (C) Describe components of the atmosphere and its role in weather change

Background & Concepts for Teachers: What is acid rain?’

Acid rain is a broad term used to describe several ways that acids fall out of the atmosphere. A more precise term is acid deposition, which has two parts: wet and dry. Wet deposition refers to acidic rain, fog, and snow. As this acidic water flows over and through the ground, it affects a variety of plants and animals. Dry deposition refers to acidic gases and particles. Dry deposited gases and particles can also be washed from trees and other surfaces by rainstorms. When that happens, the runoff water adds those acids to the acid rain, making the combination more acidic than the falling rain alone.What causes acid rain?

Scientists have discovered that sulfur and nitrogen oxides are the primary causes of acid rain. In the US, About 2/3 of all sulfur and 1/4 of all nitrogen oxides comes from electric power generation that relies on burning fossil fuels like coal. Acid rain occurs when these gases react in the atmosphere with water, oxygen, and other chemicals to form various acidic compounds. Sunlight increases the rate of most of these reactions, and the result is a mild solution of sulfuric acid and nitric acid.Why does acid rain hurt plants?

Acid rain causes slower growth, injury, or death of plants. Acid rain does not usually kill plants directly. Instead, it is more likely to weaken them by damaging their leaves, limiting the nutrients available to them, or exposing them to toxic substances slowly released from the soil. Most commonly, injury or death of trees and plants is a result of these effects of acid rain in combination with one or more additional threats.

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Activity Extensions: For a further investigation, find out if you have acid rain in your area. Place plastic containers outside to collect rainwater, and then measure the pH of this water with your pH paper.

Safety Issues: It is important to remind the students to wash their hands after handling any of the plants in acidic solution, as acid can be damaging to both skin and eyes. References: This activity was modified from an activity on the following website.http://yucky.kids.discovery.com/noflash/fun_n_games/activities/experiments/experiment_acid_rain.htmlhttp://www.epa.gov/acidrain/

Additional information may be found at:http://peer.tamu.edu/curriculum_modules/Ecosystems/hazards/acid_rain.htmhttp://peer.tamu.edu/curriculum_modules/ Ecosystems/hazards/acid_rain2.htmhttp://peer.tamu.edu/curriculum_modules/Ecosystems/Module_4/index.htm