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• W4313612039 abstract "Uncertainty about sea-level rise is dominated by uncertainty about iceberg calving, mass loss from glaciers or ice sheets by fracturing. Review of the rapidly growing calving literature leads to a few overarching hypotheses. Almost all calving occurs near or just downglacier of a location where ice flows into an environment more favorable for calving, so the calving rate is controlled primarily by flow to the ice margin rather than by fracturing. Calving can be classified into five regimes, which tend to be persistent, predictable, and insensitive to small perturbations in flow velocity, ice characteristics, or environmental forcing; these regimes can be studied instrumentally. Sufficiently large perturbations may cause sometimes-rapid transitions between regimes or between calving and noncalving behavior, during which fracturing may control the rate of calving. Regime transitions underlie the largest uncertainties in sea-level rise projections, but with few, important exceptions, have not been observed instrumentally. This is especially true of the most important regime transitions for sea-level rise. Process-based models informed by studies of ongoing calving, and assimilation of deep-time paleoclimatic data, may help reduce uncertainties about regime transitions. Failure to include calving accurately in predictive models could lead to large underestimates of warming-induced sea-level rise. ▪ Iceberg calving, the breakage of ice from glaciers and ice sheets, affects sea level and many other environmental issues. ▪ Modern rates of iceberg calving usually are controlled by the rate of ice flow past restraining points, not by the brittle calving processes. ▪ Calving can be classified into five regimes, which are persistent, predictable, and insensitive to small perturbations. ▪ Transitions between calving regimes are especially important, and with warming might cause faster sea-level rise than generally projected." @default.
• W4313612039 created "2023-01-07" @default.
• W4313612039 creator A5008369869 @default.
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• W4313612039 date "2023-05-31" @default.
• W4313612039 modified "2023-10-18" @default.
• W4313612039 title "Iceberg Calving: Regimes and Transitions" @default.
• W4313612039 cites W1558742170 @default.
• W4313612039 cites W1593291553 @default.
• W4313612039 cites W1650003622 @default.
• W4313612039 cites W1663601194 @default.
• W4313612039 cites W1757085556 @default.
• W4313612039 cites W1808380395 @default.
• W4313612039 cites W1809469167 @default.
• W4313612039 cites W1827931359 @default.
• W4313612039 cites W1946463938 @default.
• W4313612039 cites W1957873071 @default.
• W4313612039 cites W1966210493 @default.
• W4313612039 cites W1975963243 @default.
• W4313612039 cites W1982363931 @default.
• W4313612039 cites W1989304408 @default.
• W4313612039 cites W1991359553 @default.
• W4313612039 cites W1997282728 @default.
• W4313612039 cites W1998150864 @default.
• W4313612039 cites W2001035866 @default.
• W4313612039 cites W2004781260 @default.
• W4313612039 cites W2005260132 @default.
• W4313612039 cites W2019928287 @default.
• W4313612039 cites W2023512274 @default.
• W4313612039 cites W2026318490 @default.
• W4313612039 cites W2028651050 @default.
• W4313612039 cites W2033384296 @default.
• W4313612039 cites W2033384607 @default.
• W4313612039 cites W2033443586 @default.
• W4313612039 cites W2034585917 @default.
• W4313612039 cites W2041414130 @default.
• W4313612039 cites W2046146206 @default.
• W4313612039 cites W2047253720 @default.
• W4313612039 cites W2051791629 @default.
• W4313612039 cites W2052422366 @default.
• W4313612039 cites W2055563758 @default.
• W4313612039 cites W2058095946 @default.
• W4313612039 cites W2060880433 @default.
• W4313612039 cites W2061144636 @default.
• W4313612039 cites W2061839064 @default.
• W4313612039 cites W2077759887 @default.
• W4313612039 cites W2084481702 @default.
• W4313612039 cites W2086275337 @default.
• W4313612039 cites W2086700637 @default.
• W4313612039 cites W2090266865 @default.
• W4313612039 cites W2102213705 @default.
• W4313612039 cites W2103796175 @default.
• W4313612039 cites W2109376459 @default.
• W4313612039 cites W2110010948 @default.
• W4313612039 cites W2115365480 @default.
• W4313612039 cites W2128880463 @default.
• W4313612039 cites W2132751006 @default.
• W4313612039 cites W2137816126 @default.
• W4313612039 cites W2148893254 @default.
• W4313612039 cites W2151511446 @default.
• W4313612039 cites W2153259684 @default.
• W4313612039 cites W2154666809 @default.
• W4313612039 cites W2160215853 @default.
• W4313612039 cites W2161823728 @default.
• W4313612039 cites W2165359289 @default.
• W4313612039 cites W2252312519 @default.
• W4313612039 cites W2254804242 @default.
• W4313612039 cites W2270437352 @default.
• W4313612039 cites W2278432994 @default.
• W4313612039 cites W2320249130 @default.
• W4313612039 cites W2323401052 @default.
• W4313612039 cites W2323556434 @default.
• W4313612039 cites W2361628718 @default.
• W4313612039 cites W2574695739 @default.
• W4313612039 cites W2586187244 @default.
• W4313612039 cites W2605401275 @default.
• W4313612039 cites W2607405708 @default.
• W4313612039 cites W2618435920 @default.
• W4313612039 cites W2618470372 @default.
• W4313612039 cites W2735511192 @default.
• W4313612039 cites W2736365427 @default.
• W4313612039 cites W2777681314 @default.
• W4313612039 cites W2807804074 @default.
• W4313612039 cites W2808447386 @default.
• W4313612039 cites W2913710319 @default.
• W4313612039 cites W2913777366 @default.
• W4313612039 cites W2913920822 @default.
• W4313612039 cites W2942126231 @default.
• W4313612039 cites W2963104580 @default.
• W4313612039 cites W2972215770 @default.
• W4313612039 cites W2979615038 @default.

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