- The inflow-outflow interface under a linear storm boundary
- W031143Z
- The inflow-outflow interface under a linear storm boundary. The sky is lighter at right because falling rain drags air down and adiabatic warming in the downdrafts evaporates any lower clouds there. But at left, all the air is rising to form dense cloud material filled with many fine droplets that block the light and throw a dark shadow over the sky.
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