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Earth Science · Climate and Energy

The Greenhouse Effect: How Does Earth's Atmosphere Keep It Warm?

Grade 6 greenhouse effect lesson on solar and infrared energy, greenhouse gases, evidence for warming, model limitations and human influences. Includes a virtual energy-budget challenge, independent worksheet, answer key and teacher presentation.

Read the science notes ↓

A quick look inside this lesson

What happens in class?

Read the full 5E plan

Question to start with

Is there any energy leaving Earth at night?

What students actually do

Suggest incoming and outgoing energy paths.

Evidence of learning

Clear interpretation of new indexes and a question.

One question from the printable worksheet

Why is a transparent glass box not a perfect model of Earth's greenhouse effect?

See the whole worksheet

Lesson plan

The Greenhouse Effect: How Does Earth's Atmosphere Keep It Warm?

A step-by-step guide to help you teach this lesson.

Extra context for teachers

Science notes: The Greenhouse Effect: How Does Earth's Atmosphere Keep It Warm?

A short concept refresher and teaching perspective. The full procedure, printable materials, and student tasks are available in the lesson resources above.

Science in context

The greenhouse effect is an energy-flow explanation, not a claim that Earth sits under a pane of glass. Sunlight warms the surface; the warmer surface emits infrared radiation. Greenhouse gases absorb radiation at certain infrared wavelengths and emit it in different directions, changing how readily energy escapes to space.

An energy-budget model helps students identify where energy arrives, leaves or is redirected, but it does not by itself measure a particular amount of global warming. It is important to distinguish the natural greenhouse effect, which makes Earth habitable, from extra warming when greenhouse-gas concentrations increase and the balance of energy changes.

Science reference: NASA — Climate and Earth's Energy Budget

What makes the idea observable?

Sunlight warms dark pavement. After sunset the ground cools. Where does its energy go? Why is Earth's average surface warmer with an atmosphere than it would be without greenhouse gases?

Differentiate visible sunlight arriving from the Sun and infrared energy emitted by warm Earth. Greenhouse gases do not form a solid barrier.

A misconception worth addressing

  • Earth is not inside glass.
  • An energy-card model is not evidence that global temperature increased by a particular number.

A practical teaching move

Use two different arrow styles in an Earth-energy drawing: one for incoming solar radiation and one for outgoing infrared. Ask students to explain what each arrow represents.

Verified curriculum references

Plan with confidence

Lesson overview

What students will learn

  • Use a model to distinguish incoming sunlight from infrared energy emitted by the warmed surface.
  • Explain why greenhouse gases absorb and emit some outgoing infrared energy and how increasing their amount can warm Earth's surface.

Key science ideas

  • Sunlight reaches the atmosphere; some is reflected toward space by clouds, the atmosphere and light-colored surfaces.
  • Land and ocean absorb some sunlight and warm.
  • The warmed surface emits longwave infrared radiation in many directions, including upward.

Lesson at a glance

  • Grade 6
  • 55 min
  • ~15 min prep
  • 5 materials

What’s included

  • Lesson Plan
  • Investigation
  • Teacher Slides
  • Printable Worksheet
  • Teacher Answer Key
  • Interactive Activity
  • Vocabulary