Wegener-Bergeron-Findeisen process
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(meteorology) A process of ice crystal growth that occurs in mixed-phase clouds (containing a mixture of supercooled water and ice) in regions where the ambient vapor pressure falls between the saturation vapor pressure over water and the lower saturation vapor pressure over ice.
Wegener-Bergeron-Findeisen process
The Wegener-Bergeron-Findeisen process causes ice crystals to grow at the expense of supercooled water droplets in mixed-phase clouds when ambient vapor pressure is between the saturation vapor pressure over water and that over ice.
The Wegener-Bergeron-Findeisen process causes ice crystals to grow at the expense of supercooled water droplets in mixed-phase clouds when ambient vapor pressure is between the saturation vapor pressure over water and that over ice.
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