WLWeather Lab NC

Day 16 of 30

Convection-to-Jet Model Checkpoint

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Learning target

I can build a connected model from unequal heating to regional weather.

Essential question

How do small particle-level differences contribute to planet-scale patterns?

Scaffolded notes

Build the idea

1

Causes connect across scales

Solar-energy differences change surface temperature. Surface temperature affects nearby air-particle motion and density. Density and pressure differences create convection and wind. Rotation deflects large-scale motion, helping organize global wind belts and jet streams.

2

Models need directional links

A connected model uses arrows and cause-and-effect language: because, therefore, increases, decreases, rises, sinks, and deflects. Each arrow should be explainable. Avoid linking terms only because they appeared in the same chapter.

3

Predictions test a model

If a surface temperature contrast becomes larger, a model may predict a stronger pressure gradient or circulation. Evidence can support, refine, or challenge the prediction. A model is revised when evidence does not fit.

Stop and explain

Check your thinking

1. Where does the energy driving most atmospheric circulation originate?

Possible response: The Sun.

2. What role does Earth rotation play?

Possible response: It deflects large-scale moving air and helps organize wind patterns.

Interactive challenge

Try the science

Arrange the causal chain from energy source to large-scale pattern.

  1. Global winds shaped by rotation
  2. Convection and pressure-driven wind
  3. Temperature and density differences
  4. Unequal solar heating

Before you leave

Exit ticket

Write one four-step cause-and-effect chain from sunlight to wind.