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Climate Overshoot Could Leave Long-Term Ice Damage, Report Finds

An international assessment warns that a temporary rise above 1.5°C can cause persistent changes to frozen regions.

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Environment news editorial illustration for New Report Warns Temporary Warming Could Cause Lasting Ice Loss

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Source: International Cryosphere Climate Initiative, 2026-11-02.

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Read and understand · 1/3What affects the damage from an overshoot, according to the report?

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How high temperatures rise and how long they stay elevated. The second paragraph identifies both the height and duration of warming.

Clue: The report was produced by the International Cryosphere Climate Initiative in coordination with the UN Environment Programme. It examines an “overshoot” scenario: warming passes a threshold before falling again. The effects depend on how high temperatures rise and how long they remain elevated.

Read and understand · 2/3Which effects of ice loss does the report describe?

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Rising seas and pressure on mountain communities’ water supplies. The third paragraph names rising seas and pressure on water supplies.

Clue: According to the authors, some losses from glaciers and ice sheets could be effectively irreversible over human timescales. The consequences include rising seas and pressure on water supplies for communities that depend on mountain ice.

Read and understand · 3/3How does the article describe possible ice recovery?

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Some ice may recover partly over decades or centuries, but not every loss will reverse.. The final paragraph allows partial recovery for some ice while stating that not every loss would be reversed.

Clue: The report also says deep emissions cuts could limit further damage. Lower temperatures could allow some sea ice and glaciers to recover partly over decades or centuries, but not every loss would be reversed.

Your turn

Explain why the height and duration of an overshoot matter and describe one possible consequence.

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The effects depend on how far and how long temperatures rise above the threshold. Some ice losses could be effectively irreversible on human timescales and contribute to rising seas.

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