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Science · Earth and Space Science

Chapter 1: Earth as a System

Modeling Earth Systems

A model that matches the past has not yet predicted anything.

Lesson
4
Time
About 25 minutes
0 of 10 done
Part 1 of 9Something to Notice
Practice
Using mathematics and computational thinking
Crosscutting concept
Systems and system models
Core idea
ESS2.A: Earth Materials and Systems

Step 1: Something to Notice

Watch first. The explanation comes later.

Watch the idea first — 40 seconds. Then read on, and try it yourself in the next step.

Two models can fit the same historical record equally well and disagree completely about the next century.

How do you tell which one to believe?

Step 2: Find Out

Isolate the level of detail and note what each zoom leaves out.

Step 1 — Predict

A model reproduces the past record exactly. What does that establish?

Choose what you think will happen. You cannot see the experiment until you do — guessing first is what makes it worth watching.

Step 3: So Here Is Why

Now the explanation, after you have seen it happen.

Stores and flows

A model represents the world as reservoirs connected by fluxes.

Reservoir A store of matter or energy in a system model.

Every model leaves things out

On purpose

A model including everything would be as complex as the thing itself.

Fitting the past is a minimum, not a test

Not evidence

Enough adjustable parameters will match almost any record.

The test is predicting what was held back

A real test

A later period, a different region, or a variable the model never saw.

And the output should be a range

A range

Its width says how much the answer depends on assumptions nobody can pin down.

Matching the past is not yet a prediction

A model with enough adjustable parameters can be tuned to reproduce any history. Confidence comes from predicting data the model was not fitted to, which is a much harder test.

Uncertainty is quantified, not hidden

Good models report a range and say where it comes from — measurement error, unknown parameters, or scenario choices. A single number with no range is the less trustworthy output.

Step 4: A Common Mistake

Lots of people think

A model that reproduces past data must be right.

Step 5: Why Weather and Climate Models Differ in Kind

The same idea somewhere new.

A weather model predicts a specific state — rain in this place on Thursday — and becomes useless within about two weeks, because tiny errors in the starting conditions grow. A climate model predicts statistics: the distribution of temperatures over decades, not any particular day. That is why "they cannot forecast next week, so why believe a century" compares two different claims. Predicting the average of many rolls is easier than predicting one roll, not harder.

Different claims

Step 6: Think It Through

Practice makes it stick.

A Perfect Fit

Problem 1 of 2

A model reproduces the past record exactly. What does that establish?

Next Week and Next Century

Problem 2 of 2

Why can climate be projected further ahead than weather?

What a Model Shows

1 of 5

What is a reservoir in a system model?

2 of 5

Why does a model leave things out?

3 of 5

How is a model genuinely tested?

4 of 5

What does the width of a projected range tell you?

5 of 5

Weather and climate models differ how?

Step 7: Quick Check

Show what you know.

Question 1 of 1

A model reproduces the past perfectly. Is it right?

Step 8: Explain It in Writing

Claim, evidence, then reasoning.

The question

Explain how an Earth system model should be tested, and why fitting past data is not enough.

Fill in all three boxes. The reasoning box is the one that matters most.

What You Found Out

  • Models represent the world as reservoirs connected by fluxes.
  • Every model leaves things out, and that is what makes it useful.
  • Fitting past data is a minimum requirement, not evidence.
  • A model is tested by predicting what it was not fitted to.