Greenland’s glaciers are melting from the bottom up

Where Ocean Water Melts Greenland’s Glaciers From Below | SLICE EARTH | FULL DOC · 43:28 · Video: SLICE Earth · Watch at the source

In short: While surface melting captures headlines, a more insidious process is happening beneath the waves. Ocean water is infiltrating the grounding zones of Greenland's glaciers, moving through tides to erode the ice from below. This hidden mechanism is fundamentally altering the boundary between land, ice, and sea.

Scientists are increasingly focused on the 'grounding zone'—the critical area where a glacier leaves the bedrock and begins to float. On the Petermann Glacier, researchers are using high-resolution radar to track how seawater penetrates beneath ice that is still grounded. This process is driven by tides moving through these zones, creating a feedback loop where ocean water helps melt the ice from the bottom up, potentially accelerating the glacier's retreat more rapidly than surface melt alone.

This subsurface erosion is part of a broader, alarming trend in Greenland's ice sheet dynamics. Since 1990, meltwater production has skyrocketed. A study led by the University of Barcelona found that the surface area affected by extreme melting events has expanded by approximately 2.8 million km2 per decade. Furthermore, the volume of water released during these episodes has surged from an average of 12.7 gigatons per decade (between 1950 and 2023) to 82.4 gigatons per decade since 1990—a sixfold increase.

The data suggests a powerful thermodynamic effect; rising temperatures are intensifying melting beyond what atmospheric circulation alone would explain. For instance, when comparing similar air mass circulations, meltwater output has risen by 25% since 1990 compared to the 1950-1975 period. Should current patterns persist, high greenhouse gas emission models indicate that extreme meltwater fluctuations might triple before the century concludes.

Understanding these mechanics is vital for predicting global sea-level rise. Although 9.18 trillion tonnes of ice vanished from mountain glaciers from 1976 to 2024, sea-level rise is mainly caused by polar ice sheet depletion. If Greenland's ice sheet were to melt completely, it would contribute roughly seven meters to global sea levels.

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