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Cryosphere
Linked via "Glacier mass balance"
Glacier Mass Balance
Glacier mass balance is the difference between accumulation (snowfall) and ablation (melt, sublimation, and calving). Modern monitoring indicates that many alpine glaciers exhibit a net negative balance.
| Glacier Type | Average Net Balance Rate (2000–2020, $\text{m}$ water equivalent/year) | Dominant Ablation Mechanism |