The video tutorial revisits concepts from the second quarter, focusing on heat transfer methods: conduction, convection, and their applications in ocean currents. The teacher uses real-life examples, such as the wind patterns in Alaska, to illustrate these concepts. The session concludes with a reminder for students to prepare for the next class discussion.

What are the three main processes of heat transfer?

• Conduction, Convection, Radiation

• Conduction, Convection, Insulation

• Convection, Radiation, Insulation

• Radiation, Conduction, Insulation

Tags

NGSS.MS-PS1-4

Why does metal feel colder than wood at the same temperature?

• Metal reflects heat more than wood

• Heat transfers more quickly through metal

• Wood is a better conductor of heat

• Metal absorbs heat faster than wood

Tags

NGSS.MS-PS3-4

Which method of heat transfer occurs in solids?

• Convection

• Radiation

• Insulation

• Conduction

How does convection relate to ocean currents?

• It has no effect on ocean currents

• It only affects the surface of the ocean

• It creates a circular movement of water

• It causes water to evaporate

Tags

NGSS.MS-ESS2-6

What happens to cold water as it warms up?

• It sinks to the bottom

• It stays at the same level

• It evaporates

• It rises to the top

Tags

NGSS.MS-PS1-4

NGSS.MS-PS3-4

What natural phenomenon was described in the Alaska example?

• A glacier windstorm

• A volcanic eruption

• A forest fire

• A hurricane

Tags

NGSS.MS-ESS3-2

Why was there no wind in the tree line near the glacier?

• The trees blocked the wind

• The wind was too weak to reach the tree line

• The air was warmer in the tree line

• The wind was only at the glacier's base

Tags

NGSS.MS-ESS2-5

What causes the cold air from the glacier to push down towards the ground?

• The glacier's movement

• The warm air pushes it down

• The cold air is more dense

• The cold air is less dense

Tags

NGSS.MS-ESS2-5

What is the main reason for the constant wind at the glacier's base?

• The glacier's melting ice

• The dense cold air from the glacier

• The surrounding forest

• The warm air from the sun

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6

What should students be ready to discuss in the next class?

• The Coriolis effect

• The three types of heat transfer

• The Alaska example

• The reflective container experiment

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6