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COMET and MetEd offer many resources suitable for use in teaching geosciences to students in K-12.
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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2
Published in 2017
"All in a day's work for the people of NOAA as they put science, technology, and engineering to work for you. Every day, NOAA helps people with local weather forecasts, tornado warnings, oil spill cleanup, high quality seafood, navigation tools, and many other services. NOAA is also a leader in...
Grade Level   K 1 2 3 4 5 6 7 8
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3
These Instructional Modules provide K–12 teachers with high-quality, supplemental digital media resources for teaching about Earth’s systems—from weather phenomena to the development of land and water features. Resources include videos, images, data visualizations, interactives, and games from...
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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4
Published in 2010
"Trying to build a device to measure how fast the wind is blowing in this SciGirls engineering activity. You may have heard a weather reporter warn, """"Wind gusts are up to 30 mph!"""" Scientists measure wind speed using a weather instrument called an anemometer, which relies on cups attached to...
Grade Level   5 6 7 8
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5
SciJinks's Weather Science Fair web page offers middle level students project ideas in several categories; those that test a hypothesis (e.g., How does the temperature change during the day? One possible hypothesis: The temperature is lowest at midnight and highest at high noon.); those that review...
Grade Level   6 7 8
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6
Thunder is the result of the rapid expansion of super heated air caused by the extremely high temperature of lightning. Through a series of examples, the student will be able to determine the distance to a lightning strike.
Grade Level   6 7 8 9 10 11 12
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7
Rain and hail will be suspended by the updraft inside a thunderstorm until the weight of the hail and water can no longer by supported. Usually, the stronger the updraft in a thunderstorm, the more intense the storm and the larger size of hail that can be produced. Suspending a ping pong ball in th...
Grade Level   7 8 9 10 11 12
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8
The updrafts in thunderstorms can be extremely strong. The stronger the updraft, the more weight of rain and hair that can be supported. This experiment will show thta cotton balls, like clouds, hold a tremendous amount of water. In nature, once the weight of water is more than can be supported by...
Grade Level   7 8 9 10 11 12
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9
Clouds are divided into four basic forms (Cirro-form, Strato-form, Cumulo-form and Nimbo-form) at three basic levels (low, middle, and high) in the atmosphere. Many locations may experience all of these different types of clouds daily. The students will become better observers of the sky by...
Grade Level   3 4 5 6 7 8 9 10 11 12
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10
In a clean-air chamber (all solid particles are filtered out) a cloud will not form even with a relative humidity greater than 200%. While clouds are made up of droplets that are essentially distilled water, each droplet is not 100% pure. At the cloud droplet's core is a tiny water attracting...
Grade Level   6 7 8 9 10 11 12
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11
Collision and coalescence is the process by which cloud droplets grow large enough to fall as rain in clouds. You will suspend two ping pong balls in the stream of air supplied by a hair dryer. The balls will bump into each other, creating a clicking sound signifying the collision.
Grade Level   6 7 8 9 10 11 12
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12
Ocean water is salty and, in general, cold. Differences in the water density associated with temperature and salinity are vital in shaping the Great Ocean Conveyor. This lesson plan demonstrates how salinity and temperature affect density of water.
Grade Level   7 8 9 10 11 12
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13
The constant pushing of molecules into each other if the reason we feel wind. As one molecule bumps into another, it transfers energy into the next molecule. This constant pushing on the oceans surface also transfers energy to the water. This energy transfer is responsible for the motion of the...
Grade Level   7 8 9 10 11 12
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14
Onjects float if they weigh less than the weight o the water they displace. Conversely, onjects will sink if they weigh more than the weight of the water they displace. Students will observe how the added sigar in a can of soda affecs its ability to float in water by the change of density.
Grade Level   6 7 8 9 10 11 12
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15
What does up, must come down. Precipitation is the most commonly seen aspect of the hydrologic cycle. Students will learn how the water cycle works using 3-D paper craft activity. The students will see a demonstration of the concept of precipitation.
Grade Level   3 4 5 6 7 8 9 10 11 12
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16
Pressure is not only a matter of altitude but also dependent upon the temperature. As the temperature increases so does the pressure. The molecules and atoms that comprise the air we breathe gain energy as they absorb heat. That increase in energy results in faster moving atoms which we observe as...
Grade Level   7 8 9 10 11 12
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17
Bernoulli's principle states that in fluid flow, an increase in velocity occurs simultaneously with decrease in pressure. The students will discover that the faster air moves (air acting as a fluid), the lower the pressure beccomes within that air flow. They will see this effect blowing between two...
Grade Level   7 8 9 10 11 12
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18
To show that air has weight, the air is removed from one of two balanced balloons throwing the balance off.
Grade Level   5 6 7 8 9 10 11 12
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19
Demonstrate that AM radio signals can travel many 1000's of miles at night. The student will listen to as many radio stations as possible obtaining the call signs and places of origin during the evening (after sunset) hours.
Grade Level   7 8 9 10 11 12
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20
In this activity you will measure changing weather conditions prior to, during, and after a storm.
Grade Level   6 7 8 9 10 11 12
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