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Cited by 278

The DOI matches its Crossref record; 34 of the 34 references it cites were found in a registry or an index.

Ice-Sheet Response to Oceanic Forcing

Joughin, Ian, Alley, Richard B., Holland, David M.·2012·Science

Abstract

Warming and Melting: Mass loss from the ice sheets of Greenland and Antarctica account for a large fraction of global sea-level rise. Part of this loss is because of the effects of warmer air temperatures, and another because of the rising ocean temperatures to which they are being exposed. Joughin et al. (p. 1172 ) review how ocean-ice interactions are impacting ice sheets and discuss the possible ways that exposure of floating ice shelves and grounded ice margins are subject to the influences of warming ocean currents. Estimates of the mass balance of the ice sheets of Greenland and Antarctica have differed greatly—in some cases, not even agreeing about whether there is a net loss or a net gain—making it more difficult to project accurately future sea-level change. Shepherd et al. (p. 1183 ) combined data sets produced by satellite altimetry, interferometry, and gravimetry to construct a more robust ice-sheet mass balance for the period between 1992 and 2011. All major regions of the two ice sheets appear to be losing mass, except for East Antarctica. All told, mass loss from the polar ice sheets is contributing about 0.6 millimeters per year (roughly 20% of the total) to the current rate of global sea-level rise.

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Metadata

Authors
Joughin, I., Alley, R. B., & Holland, D. M.
Venue
Science
Published
2012-11-30
Volume
338
Issue
6111
Pages
1172-1176
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2046654683
Cited by
278
References
34
FWCI
17.85
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Ice-Sheet Response to Oceanic Forcing. https://app.cochat.ai/papers/10.1126/science.1226481
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Joughin, I., Alley, R. B., & Holland, D. M. (2012). Ice-Sheet Response to Oceanic Forcing. Science. https://doi.org/10.1126/science.1226481

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