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Cited by 275

The DOI matches its Crossref record; 53 of the 53 references it cites were found in a registry or an index.

Ice-sheet model sensitivities to environmental forcing and their use in projecting future sea level (the SeaRISE project)

Open access
Bindschadler, Robert A., Nowicki, Sophie, Abe-Ouchi, Ayako, Aschwanden, Andy, Choi, Hyeungu, Fastook, Jim, Granzow, Glen, Greve, Ralf, Gutowski, Gail, Herzfeld, Ute, Jackson, Charles, Johnson, Jesse, Khroulev, Constantine, Levermann, Anders, Lipscomb, William H., Martin, Maria A., Morlighem, Mathieu, Parizek, Byron R., Pollard, David, Price, Stephen F., Ren, Diandong, Saito, Fuyuki, Sato, Tatsuru, Seddik, Hakime, Seroussi, Helene, Takahashi, Kunio, Walker, Ryan, Wang, Wei Li·2013·Journal of Glaciology

Abstract

Ten ice-sheet models are used to study sensitivity of the Greenland and Antarctic ice sheets to prescribed changes of surface mass balance, sub-ice-shelf melting and basal sliding. Results exhibit a large range in projected contributions to sea-level change. In most cases, the ice volume above flotation lost is linearly dependent on the strength of the forcing. Combinations of forcings can be closely approximated by linearly summing the contributions from single forcing experiments, suggesting that nonlinear feedbacks are modest. Our models indicate that Greenland is more sensitive than Antarctica to likely atmospheric changes in temperature and precipitation, while Antarctica is more sensitive to increased ice-shelf basal melting. An experiment approximating the Intergovernmental Panel on Climate Change’s RCP8.5 scenario produces additional first-century contributions to sea level of 22.3 and 8.1 cm from Greenland and Antarctica, respectively, with a range among models of 62 and 14 cm, respectively. By 200 years, projections increase to 53.2 and 26.7 cm, respectively, with ranges of 79 and 43 cm. Linear interpolation of the sensitivity results closely approximates these projections, revealing the relative contributions of the individual forcings on the combined volume change and suggesting that total ice-sheet response to complicated forcings over 200 years can be linearized.

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Metadata

Authors
Bindschadler, R. A., Nowicki, S., Abe-Ouchi, A., Aschwanden, A., Choi, H., Fastook, J., Granzow, G., Greve, R., Gutowski, G., Herzfeld, U., Jackson, C., Johnson, J., Khroulev, C., Levermann, A., Lipscomb, W. H., Martin, M. A., Morlighem, M., Parizek, B. R., Pollard, D., Price, S. F., Ren, D., Saito, F., Sato, T., Seddik, H., Seroussi, H., Takahashi, K., Walker, R., & Wang, W. L.
Venue
Journal of Glaciology
Published
2013
Volume
59
Issue
214
Pages
195-224
ISSN
  • 0022-1430 (ISSN-L)
  • 1727-5652
OpenAlex
W2020899321
Cited by
275
References
53
FWCI
20.55
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Ice-sheet model sensitivities to environmental forcing and their use in projecting future sea level (the SeaRISE project). https://app.cochat.ai/papers/10.3189/2013jog12j125
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Bindschadler, R. A., Nowicki, S., Abe-Ouchi, A., Aschwanden, A., Choi, H., Fastook, J., Granzow, G., Greve, R., Gutowski, G., Herzfeld, U., Jackson, C., Johnson, J., Khroulev, C., Levermann, A., Lipscomb, W. H., Martin, M. A., Morlighem, M., Parizek, B. R., Pollard, D., . . . Wang, W. L. (2013). Ice-sheet model sensitivities to environmental forcing and their use in projecting future sea level (the SeaRISE project). Journal of Glaciology. https://doi.org/10.3189/2013jog12j125

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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