English Dictionary

Wegener-Bergeron-Findeisen process

固有名詞

(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.

日本語の意味

気象学における、過冷却水と氷の混在する混合状態の雲内で、氷晶が成長する過程。 / 周囲の水蒸気圧が水面と氷面の飽和水蒸気圧の間にある領域で発生する、氷晶の成長現象。

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.

混相雲における氷晶成長過程は、周囲の水蒸気圧が水の飽和蒸気圧と氷の飽和蒸気圧の間にあるときに、過冷却水滴を減らして氷晶を成長させる。

意味（1）

(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.

the Wegener-Bergeron-Findeisen process （ canonical ）