WATER & CARBON CYCLE SIMULATION

Every year some 500,000 km³ of water evaporates and falls back again, a closed loop powered by the Sun. The carbon cycle runs alongside it but leaves a readable trace: the Keeling curve carries an annual sawtooth, because Northern Hemisphere forests draw CO₂ down each summer and give it back each winter. As emissions grow the sawtooth survives while the whole line tilts upward, and deforestation cuts straight into the uptake side of the balance.

▸ Building the sea–land–tree landscape…
▸ Loading the water cycle (evaporation→rain)
▸ Loading the carbon cycle (photosynthesis↔respiration)
▸ Wiring the CO₂ Keeling curve
▸ Calibrating the carbon sinks…
▸ Ready — Online. ✅
0%
⌂ Earth

Simulation room Water & Carbon Cycles

Water & Carbon
Online
closed loop · Keeling
CO₂ gauge
🌿 Atmospheric carbon
280 (pre-ind.) → 420 (now)
Mode—
CO₂—
Season—
Emissions—
Vs. baseline—
Note
The water & carbon cycles are nearly closed; burning fossil fuels pumps CO₂ faster than the sinks absorb → it accumulates.
—
Pick a mode & adjust emissions on the right · watch the Keeling curve below · click a structure for details
Your browser has canvas disabled — the simulation cannot render.
Keeling curve — CO₂ over time CO₂ (ppm)
About Water & Carbon Cycle

Every year some 500,000 km³ of water evaporates and falls back again, a closed loop powered by the Sun. The carbon cycle runs alongside it but leaves a readable trace: the Keeling curve carries an annual sawtooth, because Northern Hemisphere forests draw CO₂ down each summer and give it back each winter. As emissions grow the sawtooth survives while the whole line tilts upward, and deforestation cuts straight into the uptake side of the balance.

Related topics in Earth