Cryo GL Marzeion 2014

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Attribution of global glacier mass loss to anthropogenic and natural causes

Last updated 2:55 PM on 5/29/26
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13 Terms

1
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What fraction of global ice mass is stored in glaciers?

2
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What hazards are linked to glacial retreat in mountains?

Destabilization of slopes and formation of unstable meltwater lakes, increasing rockslide risk

3
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What is the typical lag in glacier response to climate change?

A few decades

4
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When did global glacier retreat begin?

Around the mid-19th century

5
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What is the sign of modeled glacier mass balance (MB) in control runs?

Negative in both FULL and NAT runs

6
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How do NAT runs change over time?

Become less negative as glaciers retreat, stabilising in the mid-20th century

7
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How do FULL runs differ after mid-20th century?

Show a clear trend toward more negative glacier mass balance, consistent with observations

8
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How does anthropogenic contribution to glacier mass loss change over time?

Increases from −6 ± 35% (1851–1870) to 69 ± 24% (1991–2010)

9
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Is anthropogenic glacier signal detectable regionally?

Not always; detection varies by region

10
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Where is anthropogenic glacier signal detected with high confidence?

Alaska, western Canada, and western USA

11
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Where is model performance particularly poor?

Middle East (both FULL and NAT underestimate mass loss)

12
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What regions show model overestimation of mass loss?

Svalbard and the Russian Arctic (FULL run overestimates loss)

13
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Can glacier mass loss be fully separated into drivers?

No — cannot distinguish internal variability from natural forcing in some regions