Back to Topic 6.1 — Introduction to the atmosphere
6.1.3ESS SL15 flashcards

Albedo & heat redistribution

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Card 1 of 156.1.3
Question

Define albedo (include how it is expressed).

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All 15 Flashcards — Albedo & heat redistribution

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Card 1definition

Question

Define albedo (include how it is expressed).

Answer

Albedo is the proportion of incoming solar radiation reflected by a surface, expressed as a decimal (0–1) or a percentage.

💡 Hint

0–1 or %.

Card 2definition

Question

What is the key idea linking albedo to climate?

Answer

Albedo controls how much solar energy is reflected vs absorbed, influencing surface temperature and climate patterns.

💡 Hint

Reflect vs absorb.

Card 3example

Question

Why is heat unevenly distributed across Earth?

Answer

The equator receives more direct sunlight while the poles receive sunlight at a low angle spread over a larger area, so the tropics gain more energy.

💡 Hint

Angle of sunlight.

Card 4definition

Question

Name two major mechanisms that redistribute heat globally.

Answer

Atmospheric circulation (convection and global wind patterns) and ocean currents (surface and deep circulation).

💡 Hint

Air + ocean.

Card 5example

Question

Give one example of a high-albedo surface and one low-albedo surface.

Answer

High albedo: fresh snow/ice. Low albedo: open ocean/dark asphalt.

💡 Hint

Snow vs ocean.

Card 6example

Question

State the direction of the ice–albedo feedback loop.

Answer

Warming → ice melt → lower albedo → more absorption → more warming (positive feedback).

💡 Hint

Write the loop.

Card 7definition

Question

What is convection in the atmosphere?

Answer

Convection is the movement where warm air rises, cools, and sinks, transferring heat and driving circulation and weather.

💡 Hint

Warm rises, cool sinks.

Card 8definition

Question

What is the ice–albedo feedback loop?

Answer

Warming melts ice, lowering albedo so more solar energy is absorbed, causing more warming and further ice melt (a positive feedback).

💡 Hint

Melting ice → more absorption.

Card 9definition

Question

Where does heat generally move from and to in global redistribution?

Answer

Heat moves from regions of surplus energy near the equator toward regions of deficit energy near the poles.

💡 Hint

Surplus → deficit.

Card 10example

Question

Is the ice–albedo feedback positive or negative? Explain briefly.

Answer

It is a positive feedback because the initial warming leads to changes (lower albedo) that amplify the warming.

💡 Hint

Amplifies the change.

Card 11definition

Question

Name three processes that redistribute heat globally.

Answer

Convection (atmosphere), ocean currents, and latent heat transfer (evaporation/condensation).

💡 Hint

Convection + currents + latent heat.

Card 12definition

Question

What is latent heat transfer?

Answer

Latent heat is energy absorbed during evaporation and released during condensation, moving heat with water vapour in the atmosphere.

💡 Hint

Evaporation stores energy.

Card 13example

Question

Exam tip: For “temperature regulation” answers, what should you include?

Answer

Include both atmospheric (convection/circulation) and oceanic (currents/latent heat) heat redistribution mechanisms.

💡 Hint

Mention air + ocean.

Card 14example

Question

Exam skill: In albedo questions, what should you always link together?

Answer

Link surface colour/type to reflectivity (albedo) and then to energy absorbed and temperature change.

💡 Hint

Surface → albedo → temp.

Card 15example

Question

Exam skill: How do you write a good “feedback” explanation?

Answer

State whether it is positive or negative, then show a clear loop with arrows (cause → effect → amplifies or reduces the cause).

💡 Hint

Say type + show loop.

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