Glacier ice accumulation occurs through accumulation of snow and other frozen precipitation, as well as through other means including rime ice (freezing of water vapor on the glacier surface), avalanching from hanging glaciers on cliffs and mountainsides above, and re-freezing of glacier meltwater as . Accumulation is one element in the glacier mass balance formula, with ablation counteracting. With successive years in which accumulation exceeds ablation, then a glacier will experience positive mass balance, and its terminus will advance.
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| - Glacier ice accumulation (en)
- Accumulazione di ghiaccio nel ghiacciaio (it)
- Зоны льдообразования (ru)
- Зони льодоутворення (uk)
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| - Glacier ice accumulation occurs through accumulation of snow and other frozen precipitation, as well as through other means including rime ice (freezing of water vapor on the glacier surface), avalanching from hanging glaciers on cliffs and mountainsides above, and re-freezing of glacier meltwater as . Accumulation is one element in the glacier mass balance formula, with ablation counteracting. With successive years in which accumulation exceeds ablation, then a glacier will experience positive mass balance, and its terminus will advance. (en)
- L'accumulo di ghiaccio nel ghiacciaio si realizza per mezzo della neve e altri tipi di precipitazioni da gelo, così come attraverso altri mezzi compreso la calabrosa (congelamento di vapore acqueo sulla superficie del ghiacciaio), le valanghe (provocate dai o pendenti dalle falesie e dai versanti montani sovrastanti) e il ri-congelamento dell' del ghiacciaio come . L'accumulazione è uno elemento della formula di bilancio di massa del ghiacciaio, in contrapposizione all'ablazione. Negli anni successivi, quando l'accumulo verrà ad eccedere l'ablazione, allora il ghiacciaio sperimenterà un bilancio di massa positivo, e il suo termine avanzerà. (it)
- Зоны льдообразования — участки на ледниках, где интенсивность и ход льдообразования разные, что приводит к неодинаковому строению фирново-ледяной толщи и разной скорости превращения фирна в лёд. (ru)
- Зони льодоутворення — ділянки на льодовиках, де інтенсивність і хід льодоутворення різні, що призводить до неоднакової будови фірново-льодової товщі і різної швидкості перетворення фірна на кригу. (uk)
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| - Glacier ice accumulation occurs through accumulation of snow and other frozen precipitation, as well as through other means including rime ice (freezing of water vapor on the glacier surface), avalanching from hanging glaciers on cliffs and mountainsides above, and re-freezing of glacier meltwater as . Accumulation is one element in the glacier mass balance formula, with ablation counteracting. With successive years in which accumulation exceeds ablation, then a glacier will experience positive mass balance, and its terminus will advance. (en)
- L'accumulo di ghiaccio nel ghiacciaio si realizza per mezzo della neve e altri tipi di precipitazioni da gelo, così come attraverso altri mezzi compreso la calabrosa (congelamento di vapore acqueo sulla superficie del ghiacciaio), le valanghe (provocate dai o pendenti dalle falesie e dai versanti montani sovrastanti) e il ri-congelamento dell' del ghiacciaio come . L'accumulazione è uno elemento della formula di bilancio di massa del ghiacciaio, in contrapposizione all'ablazione. Negli anni successivi, quando l'accumulo verrà ad eccedere l'ablazione, allora il ghiacciaio sperimenterà un bilancio di massa positivo, e il suo termine avanzerà. (it)
- Зоны льдообразования — участки на ледниках, где интенсивность и ход льдообразования разные, что приводит к неодинаковому строению фирново-ледяной толщи и разной скорости превращения фирна в лёд. (ru)
- Зони льодоутворення — ділянки на льодовиках, де інтенсивність і хід льодоутворення різні, що призводить до неоднакової будови фірново-льодової товщі і різної швидкості перетворення фірна на кригу. (uk)
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