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Science lesson plan · 12th grade (Year 13 in England) · 45 minutes

Climate feedbacks and natural climate cycles

Weather and climate

CCSS NGSS.HS-ESS2-2CCSS NGSS.HS-ESS2-4England: A level Geography: The carbon and water cycles (extension)England: GCSE Combined Science: Chemistry of the atmosphere

Objective and success criteria

Students will: Climate feedbacks and natural climate cycles.

  • I can answer questions on today's skill on my own, without help.
  • I can explain each step and say why it works.
  • I can check my answer and spot a mistake.

Before and after

Needs first: Analyse climate data: COâ‚‚ records and temperature trends

Leads to: the next skill in this area.

Materials: Weather maps, Thermometers, Mini whiteboards, A diagram or short video clip of the idea, Printed student sheet (below).

Warm-up · 5 min

  • Quick retrieval from earlier learning (Analyse climate data: COâ‚‚ records and temperature trends). Students answer on mini whiteboards.
  • Show answers together and note who needs support in the main task.
  1. Annual mean CO₂ at the Mauna Loa observatory was about 354 ppm in 1990 and about 414 ppm in 2020. What was the mean rate of increase, in ppm per year? Give 1 decimal place. → 2Prompt: rate = change in CO₂ ÷ change in time
  2. The CO₂ record from Mauna Loa rises every year but also goes up and down within each year. Why the yearly wiggle? (People burn no fuel in summer / The instruments are faulty / Northern Hemisphere plants absorb CO₂ in spring and summer and release it in autumn and winter / Volcanoes erupt every winter) → Northern Hemisphere plants absorb CO₂ in spring and summer and release it in autumn and winterPrompt: Most land, and so most plants, is in the Northern Hemisphere.
  3. Climate evidence: which statement is NOT true? (Sea level is rising as oceans warm and land ice melts. / Arctic sea ice in summer has shrunk since satellite records began in 1979. / Global average surface temperature has risen by more than 1 °C since the late 1800s. / A cold winter in one city disproves global warming.) → A cold winter in one city disproves global warming.Prompt: What is the difference between weather and climate?

Hook · 5 min

  • Show today's forecast and ask what it means for the class and how forecasters know.
  • Share the objective: Climate feedbacks and natural climate cycles. Read the success criteria together.

I do: model it · 10 min

  • Work through the example out loud, saying why you do each step, not just what you do.
  • Example: Is this a positive or negative climate feedback: more COâ‚‚ boosts plant growth, which takes up some COâ‚‚?
  • Step 1: A negative feedback works against the initial change.
  • Step 2: So the answer is: negative feedback (reduces warming)
  • Answer: negative feedback (reduces warming)
  • Pause after each step and ask a student to say what comes next.

We do: guided practice · 10 min

  • Do these together. Students try each step on whiteboards before you reveal it.
  • Use the hints as prompts rather than giving the answer.
  1. Is this a positive or negative climate feedback: a warmer Earth radiates more energy to space? (positive feedback (amplifies warming) / negative feedback (reduces warming)) → negative feedback (reduces warming)Prompt: Does the effect cause more warming or less?
  2. Fresh snow has an albedo of 0.85 (it reflects that fraction of sunlight). If 400 W/m² of sunlight arrives, how much is absorbed, in W/m²? → 60 W/m²Prompt: Absorbed fraction = 1 − albedo.

You do: independent practice · 10 min

  • Students work on the student sheet. Circulate and check the first two answers of every student early.
  • Students who finish: write a question of their own for a partner, with the answer.

The 8 questions are on the student sheet below, with answers in the key.

Exit ticket · 5 min

  • Two questions on their own. Sort answers into got it / nearly / not yet to plan the next lesson.
  1. Is this a positive or negative climate feedback: warmer air holds more water vapour, a greenhouse gas? (positive feedback (amplifies warming) / negative feedback (reduces warming)) → positive feedback (amplifies warming)Prompt: Does the effect cause more warming or less?
  2. Why might a "tipping point" in the climate system be especially worrying? (Past a threshold, change can become self-sustaining and hard to reverse / It makes the climate change back instantly / It reduces sea level / It only affects weather for one day) → Past a threshold, change can become self-sustaining and hard to reversePrompt: Think about ice sheets once they start to collapse.

Watch out for

  • Everyday meanings of words getting in the way of the science meaning: define key words explicitly.
  • Remembering facts without the reason: ask "why?" and "what is the evidence?"

Support and stretch

Support

  • Review first: Analyse climate data: COâ‚‚ records and temperature trends.
  • Use concrete materials: weather maps.
  • Give the first step of each question, or a partly worked example to finish.
  • Pair with a confident partner for the guided practice.

Stretch

  • Explain a common mistake in writing and how to fix it.
  • Write a word problem that uses today's skill, then solve a partner's.

Homework and more practice

Free online practice with hints and printable worksheets for this skill: eurekami.com/science/grade-12.

Free lesson plan from eurekami.com/lesson-plan-builder

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Climate feedbacks and natural climate cycles

Name

Date

Score/ 8

  1. Question 1

    Is this a positive or negative climate feedback: warmer air holds more water vapour, a greenhouse gas?

    • A. positive feedback (amplifies warming)
    • B. negative feedback (reduces warming)
  2. Question 2

    Sea ice has an albedo of 0.6 (it reflects that fraction of sunlight). If 200 W/m² of sunlight arrives, how much is absorbed, in W/m²?

    AnswerW/m²

  3. Question 3

    What are Milankovitch cycles?

    • A. the 11-year sunspot cycle
    • B. slow changes in Earth's orbit and tilt that pace ice ages over tens of thousands of years
    • C. yearly ocean tides
    • D. daily changes in weather
  4. Question 4

    Is this a positive or negative climate feedback: a warmer Earth radiates more energy to space?

    • A. positive feedback (amplifies warming)
    • B. negative feedback (reduces warming)
  5. Question 5

    Forest has an albedo of 0.15 (it reflects that fraction of sunlight). If 300 W/m² of sunlight arrives, how much is absorbed, in W/m²?

    AnswerW/m²

  6. Question 6

    Why can Milankovitch cycles not explain today's warming?

    • A. They cause cooling only
    • B. They only affect Mars
    • C. They act over thousands of years, but today's warming has happened in about 150 years
    • D. They stopped working in 1900
  7. Question 7

    Is this a positive or negative climate feedback: more COâ‚‚ boosts plant growth, which takes up some COâ‚‚?

    • A. positive feedback (amplifies warming)
    • B. negative feedback (reduces warming)
  8. Question 8

    Desert sand has an albedo of 0.4 (it reflects that fraction of sunlight). If 200 W/m² of sunlight arrives, how much is absorbed, in W/m²?

    AnswerW/m²

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Answer key: Climate feedbacks and natural climate cycles

  1. 1. A. positive feedback (amplifies warming)

  2. 2. 80 W/m²

  3. 3. B. slow changes in Earth's orbit and tilt that pace ice ages over tens of thousands of years

  4. 4. B. negative feedback (reduces warming)

  5. 5. 255 W/m²

  6. 6. C. They act over thousands of years, but today's warming has happened in about 150 years

  7. 7. B. negative feedback (reduces warming)

  8. 8. 120 W/m²