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TRANSCRIPT
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The Atmosph
ere
WeatherHeat
TransferMoveme
ntGrab Bag
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DIRECTIONS:1. Select a value in any category.
2. Read the answer
3. First teammate to properly phrase the question earns the money
4. Click the Home Button to return to main page
5. Most $ at end wins game
6. Or just use it for fun and learning!
This is created by swirling
gases or liquids in a spiral.
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Satellite pictures reveal that
clouds in the atmosphere
form these patterns.
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Air above this surface moves
down.
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This layer of the atmosphere
is eight miles thick and
contains most of the Earth’s
weather.
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This current is formed by the
movement of gasses or
liquids between hot and cold
areas.
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This object fuels the Earth’s
weather.
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This phenomenon occurs
when air rushes from high to
low pressure.
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This is created when hot,
moist air meets with cold, dry
air in the central states.
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These form when warm air
front meets cold air front
head-on over land.
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Light, warm air is associated
with this kind of pressure
system.
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This substance heated faster
during the heat rate
investigation in lesson 2.
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This substance stayed warm
longer during the heat rate
investigation.
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This breeze is most common
during the evening along
beaches.
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This breeze forms most
commonly along beaches
during the day.
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These massive rotating
storms begin over warm
tropical waters.
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These air fronts move
quickly and create unstable
air masses.
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These are responsible for the
movement of warm tropical
waters toward the poles.
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As observed by the “punk”
experiment, the movement of
this air did not permit the
smoke to enter the funnel.
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At night, warm air over a
body of water causes this
kind of wind.
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This atmospheric phenomena
can be used to help planes
travel large distances.
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Blame Canada! Tornadoes
often form here when cold,
dry from Canada meets warm,
moist air from the Gulf of
Mexico.Click the Home Button after Question
This is the spiraling mass of
air in the center of a storm.
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This process recycles the
Earth’s water through
evaporation and
condensation.
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These phenomena effect the
global climate by distributing
warm or cold water around
the world.
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This causes sunlight to travel
through more air to reach the
poles and less to reach
equator.
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