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Environmental · L5 · Diurnal Boundary-Layer Stability Cycle

How surface heating and cooling drive the ABL through unstable, neutral, and stable regimes over a day.

by @openstemUpdated Environmental
☀️ Daytime heatingUnstable: L < 0, convective thermalsTransition near sunsetNeutral: |L| → ∞🌙 Nighttime radiative coolingStable: L > 0, suppressed turbulence

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