Raven sets a tall clear jar of water on the Station Rooftop table. Next to it sit a cup of ice, a salt shaker and blue food coloring.
"Today we make a tiny North Atlantic," she says.
Rocket is already stirring. "Cold plus salt plus blue. Then I pour it in and it goes... where?"
"Predict first, then pour," Raven says. "What do you notice about how the blue moves?"
Nova hovers above the jar and lowers a thin beam of light into the water. "Watch the walls of the jar, not just the top," she hints.
Rocket tips the cup. A blue ribbon slides down the glass and pools at the bottom like a cold river.
"The conveyor belt," he whispers. "In a jar."
You will test whether cold, salty water sinks below room-temperature water, the way NOAA describes near the poles.
Then you will test warm fresh water the same way and compare. Record what you see in the table.
| Test | My prediction | What I saw at 2 minutes | What I saw at 10 minutes |
|---|---|---|---|
| Cold, salty, colored water | |||
| Warm, fresh, colored water |
Near the poles, sea ice forms and leaves its salt behind. The water around it gets colder and saltier, so it sinks.
Your cold, salty water is a model of that polar water. The jar is a model of the ocean.
Warm water is less dense, so it tends to spread near the top instead of diving to the bottom.
A model is never the whole ocean. The real conveyor belt takes about 1,000 years, not two minutes.
| What the lab shows | True or false? |
|---|---|
| Cold, salty water is denser than room-temperature fresh water. | ? |
| Denser water tends to sink. | ? |
| The jar shows exactly how fast the real ocean moves. | ? |
| Near the poles, forming sea ice leaves salt behind in the water. | ? |
In the real ocean, the sinking happens near the pole in the North Atlantic and in places off the coast of Antarctica.
Surface water flows in to replace the sinking water. That pull is part of what keeps the conveyor belt moving.
Scientists build models too, from jars like yours to huge computer programs. Models let them test how salt and heat change the currents.
Great lab work. Tomorrow you read real climate numbers for four cities.