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Polar Vortex Hovmöller: Height–Time SSW Cross-Section

2D height-time (Hovmöller) simulation of a Sudden Stratospheric Warming: a finite-difference wave-mean-flow PDE across a vertical column shows the zonal wind decelerate, reverse, and the warming anomaly descend from the stratosphere over days.

Climate, Ecology & Environment2DAdvanced60 FPS📱 Mobile-adapted⇄ 3D version
2d-stratospheric-sudden-warming-polar-vortex ↗ Open standalone

This is the vertical-structure companion to the 3D polar-vortex simulator: instead of watching air parcels orbit a single stratospheric surface, it solves the wave-mean-flow interaction as a finite-difference PDE across 26 height levels from the ground to the upper stratosphere, and plots the result as a scrolling height–time (Hovmöller) diagram — the same kind of diagnostic meteorologists read reanalysis data with. Set the wave-forcing amplitude and watch the color front propagate upward at a finite group velocity, decelerating and eventually reversing the 60°N/10 hPa wind (the formal Sudden Stratospheric Warming criterion) while the compensating warming anomaly appears aloft and diffuses downward over the following days — a distinct but physically equivalent view of the same event captured by the 3D model.

⚙ Under the hood

2D height-time (Hovmöller) simulation of a Sudden Stratospheric Warming: a finite-difference wave-mean-flow PDE across a vertical column shows the zonal wind decelerate, reverse, and the warming anomaly descend from the stratosphere over days.

climatestratospherepolar vortexatmospheric dynamicswave-mean flowweather forecasting

2D · HTML5 Canvas 2D · 60 FPS target · runs fully client-side, no install

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