Articles | Volume 8, issue 5
https://doi.org/10.5194/gmd-8-1547-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/gmd-8-1547-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
NEMO–ICB (v1.0): interactive icebergs in the NEMO ocean model globally configured at eddy-permitting resolution
R. Marsh
CORRESPONDING AUTHOR
University of Southampton, National Oceanography Centre, Southampton, UK
V. O. Ivchenko
University of Southampton, National Oceanography Centre, Southampton, UK
N. Skliris
University of Southampton, National Oceanography Centre, Southampton, UK
S. Alderson
National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK
G. R. Bigg
Department of Geography, University of Sheffield, Sheffield, UK
G. Madec
National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK
LOCEAN-IPSL, CNRS-IRD-UPMC-MNHN, Paris, France
A. T. Blaker
National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK
Y. Aksenov
National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK
B. Sinha
National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK
A. C. Coward
National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK
J. Le Sommer
LGGE, UMR5183, CNRS-UJF, Grenoble, France
N. Merino
LGGE, UMR5183, CNRS-UJF, Grenoble, France
V. B. Zalesny
Institute of Numerical Mathematics, Russian Academy of Sciences, Gubkin St. 8, Moscow, 119333, Russia
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- The effects of Antarctic iceberg calving‐size distribution in a global climate model A. Stern et al. 10.1002/2016JC011835
- Modeling tabular icebergs submerged in the ocean A. Stern et al. 10.1002/2017MS001002
- A model for assessing iceberg hazard G. Bigg et al. 10.1007/s11069-018-3243-x
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- A comparison of Eulerian and Lagrangian methods for vertical particle transport in the water column T. Nordam et al. 10.5194/gmd-16-5339-2023
- The Role of Tides in Ocean‐Ice Shelf Interactions in the Southwestern Weddell Sea U. Hausmann et al. 10.1029/2019JC015847
- The Parcels v2.0 Lagrangian framework: new field interpolation schemes P. Delandmeter & E. van Sebille 10.5194/gmd-12-3571-2019
- Wave inhibition by sea ice enables trans-Atlantic ice rafting of debris during Heinrich events T. Wagner et al. 10.1016/j.epsl.2018.05.006
- Using Vertically Integrated Ocean Fields to Characterize Greenland Icebergs' Distribution and Lifetime J. Marson et al. 10.1029/2018GL077676
- The history of a cluster of large icebergs on leaving the Weddell Sea pack ice and their impact on the ocean G. Bigg & R. Marsh 10.1017/S0954102022000517
- Parameterizing the basal melt of tabular icebergs A. FitzMaurice & A. Stern 10.1016/j.ocemod.2018.08.005
- Modelling twentieth century global ocean circulation and iceberg flux at 48°N: implications for west Greenland iceberg discharge D. Wilton et al. 10.1016/j.pocean.2015.07.003
- Modeling the breakup of tabular icebergs M. England et al. 10.1126/sciadv.abd1273
- Physical processes and feedbacks obscuring the future of the Antarctic Ice Sheet D. Li 10.1016/j.geogeo.2022.100084
- Icebergs Melting C. Cenedese & F. Straneo 10.1146/annurev-fluid-032522-100734
- A simulation of small to giant Antarctic iceberg evolution: Differential impact on climatology estimates T. Rackow et al. 10.1002/2016JC012513
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- How climate model biases skew the distribution of iceberg meltwater T. Wagner & I. Eisenman 10.1002/2016GL071645
- Modeling Ice Shelf Cavities and Tabular Icebergs Using Lagrangian Elements A. Stern et al. 10.1029/2018JC014876
- How Winds and Ocean Currents Influence the Drift of Floating Objects T. Wagner et al. 10.1175/JPO-D-20-0275.1
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- Effect of a sheared flow on iceberg motion and melting A. FitzMaurice et al. 10.1002/2016GL071602
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- Parameterizing Tabular‐Iceberg Decay in an Ocean Model A. Huth et al. 10.1029/2021MS002869
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- On the future navigability of Arctic sea routes: High-resolution projections of the Arctic Ocean and sea ice Y. Aksenov et al. 10.1016/j.marpol.2015.12.027
- PARASO, a circum-Antarctic fully coupled ice-sheet–ocean–sea-ice–atmosphere–land model involving f.ETISh1.7, NEMO3.6, LIM3.6, COSMO5.0 and CLM4.5 C. Pelletier et al. 10.5194/gmd-15-553-2022
- Mechanisms for Late 20th and Early 21st Century Decadal AMOC Variability A. Megann et al. 10.1029/2021JC017865
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- On the representation of capsizing in iceberg models T. Wagner et al. 10.1016/j.ocemod.2017.07.003
- Regional Changes in Icescape Impact Shelf Circulation and Basal Melting E. Cougnon et al. 10.1002/2017GL074943
- Antarctic icebergs melt over the Southern Ocean: Climatology and impact on sea ice N. Merino et al. 10.1016/j.ocemod.2016.05.001
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- An assessment of basal melt parameterisations for Antarctic ice shelves C. Burgard et al. 10.5194/tc-16-4931-2022
- Southern Ocean warming and Antarctic ice shelf melting in conditions plausible by late 23rd century in a high-end scenario P. Mathiot & N. Jourdain 10.5194/os-19-1595-2023
- Modelling capsizing icebergs in the open ocean P. Bonnet et al. 10.1093/gji/ggaa353
- Prospects for seasonal forecasting of iceberg distributions in the North Atlantic R. Marsh et al. 10.1007/s11069-017-3136-4
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- The Effects of Atmospheric and Lateral Buoyancy Fluxes on Labrador Sea Mixed Layer Depth L. Gillard et al. 10.1016/j.ocemod.2022.101974
- Future Response of Antarctic Continental Shelf Temperatures to Ice Shelf Basal Melting and Calving M. Thomas et al. 10.1029/2022GL102101
- Two-timescale response of a large Antarctic ice shelf to climate change K. Naughten et al. 10.1038/s41467-021-22259-0
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Latest update: 13 Dec 2024
Short summary
Calved icebergs account for around 50% of total freshwater input to the ocean from the Greenland and Antarctic ice sheets. As they melt, icebergs interact with the ocean. We have developed and tested interactive icebergs in a state-of-the-art global ocean model, showing how sea ice, temperatures, and currents are disturbed by iceberg melting. With this new model capability, we are better prepared to predict how future increases in iceberg numbers might influence the oceans and climate.
Calved icebergs account for around 50% of total freshwater input to the ocean from the Greenland...
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