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Convection in the Atmosphere and Oceans

Authored by Lisa Thompson

Science

8th Grade

NGSS covered

Convection in the Atmosphere and Oceans
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25 questions

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1.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

The transfer of heat energy through liquids and gasses due to uneven heating is called:

Convection

Conduction

Radiation

Revolution

Tags

NGSS.MS-ESS2-6

2.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

In coastal areas, at night, the breeze moves:

From the ocean to land (Sea Breeze)

From the clouds to water due to precipitation

From the land towards the ocean (Land Breeze)

From the surface to the stratosphere

Tags

NGSS.MS-ESS2-6

NGSS.MS-ESS2-5

3.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Ocean currents move warm water:

From the equator to the poles

From the poles to the equator

From the Atlantic to the Pacific

Along the Antarctic flow

Tags

NGSS.MS-ESS2-6

4.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

The deep ocean current that moves water around the globe is known as:

The Thermocline

The Pycnocline

The Thermohaline

The Halocline

Tags

NGSS.MS-ESS2-6

5.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Media Image

Warm air rises and the cool air sinks demonstrates this type of heat transfer. 

conduction

convection

radiation

Insolation 

Tags

NGSS.MS-ESS2-6

NGSS.MS-ESS2-5

6.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Media Image

A

B

C

D

Answer explanation

Media Image

Warm air rise and cool air sinks

warm air is less dense

cool air is more dense so it sinks

Tags

NGSS.MS-ESS2-6

7.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Media Image

A student models convection currents in a laboratory activity. How are the convection currents in the student's model different from the convection currents in Earth's atmosphere and oceans?

The warm air in Earth's atmosphere and the warm water in Earth's oceans sink instead of rise.

The heat source for Earth's atmosphere and oceans is the sun, which heats from above instead of below.

Convection cells in Earth's atmosphere and oceans flow in the same direction instead of opposite directions.

Cold air in Earth's atmosphere and cold water in Earth's oceans are less dense that warm air and warm water instead of being more dense.

Tags

NGSS.MS-ESS2-6

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