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Update README with accurate app description
Browse filesCo-Authored-By: Claude Sonnet 4.6 <noreply@anthropic.com>
README.md
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#
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- **CAPE, CIN, LCL, LFC, EL** from the analytic sounding
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- **SRH** (0–2 km, 2–5 km) and **Updraft Helicity** relative to Bunkers right-mover
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Plan views and cross-sections are
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# Updraft Forcing
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A kinematic-diagnostic model for examining how environmental wind shear and mesocyclone intensity drive perturbation pressure and vertical accelerations in convective storms.
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Configure a Weisman-Klemp analytic sounding and drag the hodograph to set the wind profile, then explore:
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- **Skew-T log-P diagram** with parcel trace, CAPE/CIN shading, and meteorological wind barbs
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- **Perturbation pressure** decomposed into linear (shear interaction), nonlinear spin, nonlinear splat, and buoyancy terms (Trapp 2013)
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- **Vertical velocity** diagnosed from a 1-D pseudoadiabatic parcel model with overshooting top
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- **CAPE, CIN, LCL, LFC, EL** from the analytic sounding
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- **SRH** (0–2 km, 2–5 km) and **Updraft Helicity** relative to the Bunkers right-mover storm motion
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- **Prescribed mesocyclone ζ(z)** driving the nonlinear spin pressure term and updraft helicity
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Plan views and vertical cross-sections are available for all 3-D fields. Pressure perturbations are solved via a 2-D FFT + tridiagonal Poisson solver on a 100 × 100 × 161 grid (Δ = 100 m).
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