PPolySim OS
Use case · powered by Lapse Rate

Lapse Rate for a jet-stream shift

Simulate a jet-stream shift live in your browser. This runs the real Lapse Rate solver — adjust the inputs, watch it respond instantly, and export the result. No install, no account.

Atmospheric Lapse Rate & Cloud BaseLive

Controls

Presets

Air cools with height at the environmental lapse rate. Rising air cools until it hits its dew point at the lifting condensation level — the cloud base — estimated by (T − Td)/8 km. The pressure falls with altitude following the barometric formula.

▶ Run in Python

Data Inspector

Cloud base0.88 km
Pressure at 3 km701 hPa
T at 5 km-17.5 °C

Governing equation

Reading this result: Cloud base is set by the dew-point depression, not the lapse rate: it sits at roughly (T − Td)/8 km, while the lapse rate only controls how cold it gets on the way up.

Runs locally in your browser — free forever. Scale to the cloud when reality gets heavy.

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About this simulation

The full Lapse Rate tool models a jet-stream shift with the same numerics engineers and scientists use — running entirely client-side. Change any parameter and the result updates in real time, so you can build intuition, check a design, or teach the concept without spreadsheets or installs.

More you can do with Lapse Rate

Other ways to simulate a jet-stream shift

Frequently asked questions

How do I simulate a jet-stream shift?
Open this page and use the live Lapse Rate tool below — set your inputs and the simulation runs instantly in your browser using real numerics. No install, no account needed.
Is it free?
Yes. The simulation runs free in your browser. A one-time unlock or a Pro plan adds advanced parameters, saved presets, data import, and clean exports.
Can I use my own numbers?
Absolutely — every input is adjustable, and with data import you can drive a jet-stream shift from your own measurements.