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Abstract
Arctic
sea ice is retreating rapidly, raising prospects of a future ice-free
Arctic Ocean during summer. Since climate-model simulations of the
sea-ice loss differ substantially, we here use a robust linear
relationship between monthly-mean September sea-ice area and cumulative
CO2 emissions to infer the future evolution of Arctic summer
sea ice directly from the observational record. The observed linear
relationship implies a sustained loss of 3 ± 0.3 m2 of September sea-ice area per metric ton of CO2 emission. Based on this sensitivity, Arctic sea-ice will be lost throughout September for an additional 1000 Gt of CO2
emissions. Most models show a lower sensitivity, which is possibly
linked to an underestimation of the modeled increase in incoming
longwave radiation and of the modeled Transient Climate Response.
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