2022
DOI: 10.1002/essoar.10510395.1
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The Transient Sea Level response to external forcing in CMIP6 models

Abstract:  The rate of ice sheet mass loss and ocean expansion has a near linear relationship to global mean surface warming in both models and data.  The modeled transient sensitivity of the sea level budget to warming is compatible with historical behavior except for Antarctic mass loss.  Models of Antarctic mass loss may be biased as data shows increasing losses with warming in contrast to models.

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Cited by 1 publication
(5 citation statements)
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“…Perhaps most intriguingly, Grinsted et al. (2022) find a significant discrepancy between models and observations, namely that observations show that sea‐level rates are more sensitive to surface‐temperature changes than the models anticipate.…”
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confidence: 99%
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“…Perhaps most intriguingly, Grinsted et al. (2022) find a significant discrepancy between models and observations, namely that observations show that sea‐level rates are more sensitive to surface‐temperature changes than the models anticipate.…”
mentioning
confidence: 99%
“…Grinsted et al. (2022) hypothesize that mismatches between models and observations may arise from poor representation of ice flow and sliding on the West Antarctic ice sheet and the Antarctic Peninsula in models, which results in simulated ice discharge being too insensitive to temperature changes. Bamber et al.…”
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confidence: 99%
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