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Weather Forecasting Series Archive

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Convective Boundary Layer Growth & Entrainment Zone Dynamics: How Solar Heat Fluxes and Turbulent Thermals Erode Nocturnal Inversions
WEATHER FORECASTING

Convective Boundary Layer Growth & Entrainment Zone Dynamics: How Solar Heat Fluxes and Turbulent Thermals Erode Nocturnal Inversions

### At dawn, the lowest kilometre of our atmosphere is trapped under an invisible, stagnant lid. Within hours, solar radiative forcing unleashes a towering turbulent engine that scours the valleys, mixes the troposphere, and erects the day’s cloudscape.

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Advection Fog Dynamics & Marine Layer Inversions: How Maritime Air Advection and Cold Coastal Upwelling Forge Persistent Sea Fog Banks
WEATHER FORECASTING

Advection Fog Dynamics & Marine Layer Inversions: How Maritime Air Advection and Cold Coastal Upwelling Forge Persistent Sea Fog Banks

``` Warm, Subsiding Free Troposphere (Dry, 25°C - 30°C) ======================================================================== <--- INVERSION BASE ▲ ▲ ▲ Turbulent Marine Layer: Saturated Fog Deck (Cold, 12°C) ▲ ▲ ▲ ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ <--- SEA SURFACE Frigid Upwelling Current (Ekman Transport, SST ~ 10°C) ```

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