Articles | Volume 14, issue 7
https://doi.org/10.5194/tc-14-2205-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-2205-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
13 Jul 2020
Research article |
| 13 Jul 2020
Impact of West Antarctic ice shelf melting on Southern Ocean hydrography
Yoshihiro Nakayama
CORRESPONDING AUTHOR
Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan
Alfred Wegener Institute, Bremerhaven, Germany
Ralph Timmermann
Alfred Wegener Institute, Bremerhaven, Germany
Hartmut H. Hellmer
Alfred Wegener Institute, Bremerhaven, Germany
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Cited
17 citations as recorded by crossref.
- Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica P. Sheehan et al. 10.1029/2023GL102785
- The Salinity Budget of the Ross Sea Continental Shelf, Antarctica L. Yan et al. 10.1029/2022JC018979
- Global Consequences of Regional Connectivity Along the Antarctic Margin R. Beadling 10.1029/2023JC019908
- 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
- Persistent Ross Sea Freshening From Imbalance West Antarctic Ice Shelf Melting S. Jacobs et al. 10.1029/2021JC017808
- Improving Antarctic Bottom Water precursors in NEMO for climate applications K. Hutchinson et al. 10.5194/gmd-16-3629-2023
- Seasonality of Mesoscale Phytoplankton Control in Eastern Fram Strait V. Schourup‐Kristensen et al. 10.1029/2021JC017279
- Wind‐Driven Seasonal Intrusion of Modified Circumpolar Deep Water Onto the Continental Shelf in Prydz Bay, East Antarctica G. Guo et al. 10.1029/2022JC018741
- Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier Y. Nakayama et al. 10.1029/2021GL094149
- Investigation of ice shelf ocean interaction in the Amundsen Sea using numerical modeling and ocean state estimates Y. Nakayama 10.5928/kaiyou.29.6_233
- Hydrography, circulation, and response to atmospheric forcing in the vicinity of the central Getz Ice Shelf, Amundsen Sea, Antarctica V. Dundas et al. 10.5194/os-18-1339-2022
- Antarctic Peninsula warming triggers enhanced basal melt rates throughout West Antarctica M. Flexas et al. 10.1126/sciadv.abj9134
- Pathways and Timescales of Connectivity Around the Antarctic Continental Shelf H. Dawson et al. 10.1029/2022JC018962
- Ocean variability beneath Thwaites Eastern Ice Shelf driven by the Pine Island Bay Gyre strength T. Dotto et al. 10.1038/s41467-022-35499-5
- Drivers and Reversibility of Abrupt Ocean State Transitions in the Amundsen Sea, Antarctica J. Caillet et al. 10.1029/2022JC018929
- The Antarctic Coastal Current in the Bellingshausen Sea R. Schubert et al. 10.5194/tc-15-4179-2021
- Influence of Shelf Break Processes on the Transport of Warm Waters Onto the Eastern Amundsen Sea Continental Shelf M. Azaneu et al. 10.1029/2022JC019535
16 citations as recorded by crossref.
- Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica P. Sheehan et al. 10.1029/2023GL102785
- The Salinity Budget of the Ross Sea Continental Shelf, Antarctica L. Yan et al. 10.1029/2022JC018979
- Global Consequences of Regional Connectivity Along the Antarctic Margin R. Beadling 10.1029/2023JC019908
- 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
- Persistent Ross Sea Freshening From Imbalance West Antarctic Ice Shelf Melting S. Jacobs et al. 10.1029/2021JC017808
- Improving Antarctic Bottom Water precursors in NEMO for climate applications K. Hutchinson et al. 10.5194/gmd-16-3629-2023
- Seasonality of Mesoscale Phytoplankton Control in Eastern Fram Strait V. Schourup‐Kristensen et al. 10.1029/2021JC017279
- Wind‐Driven Seasonal Intrusion of Modified Circumpolar Deep Water Onto the Continental Shelf in Prydz Bay, East Antarctica G. Guo et al. 10.1029/2022JC018741
- Antarctic Slope Current Modulates Ocean Heat Intrusions Towards Totten Glacier Y. Nakayama et al. 10.1029/2021GL094149
- Investigation of ice shelf ocean interaction in the Amundsen Sea using numerical modeling and ocean state estimates Y. Nakayama 10.5928/kaiyou.29.6_233
- Hydrography, circulation, and response to atmospheric forcing in the vicinity of the central Getz Ice Shelf, Amundsen Sea, Antarctica V. Dundas et al. 10.5194/os-18-1339-2022
- Antarctic Peninsula warming triggers enhanced basal melt rates throughout West Antarctica M. Flexas et al. 10.1126/sciadv.abj9134
- Pathways and Timescales of Connectivity Around the Antarctic Continental Shelf H. Dawson et al. 10.1029/2022JC018962
- Ocean variability beneath Thwaites Eastern Ice Shelf driven by the Pine Island Bay Gyre strength T. Dotto et al. 10.1038/s41467-022-35499-5
- Drivers and Reversibility of Abrupt Ocean State Transitions in the Amundsen Sea, Antarctica J. Caillet et al. 10.1029/2022JC018929
- The Antarctic Coastal Current in the Bellingshausen Sea R. Schubert et al. 10.5194/tc-15-4179-2021
Latest update: 21 Sep 2023
Short summary
Previous studies have shown accelerations of West Antarctic glaciers, implying that basal melt rates of these glaciers were small and increased in the middle of the 20th century. We conduct coupled sea ice–ice shelf–ocean simulations with different levels of ice shelf melting from West Antarctic glaciers. This study reveals how far and how quickly glacial meltwater from ice shelves in the Amundsen and Bellingshausen seas propagates downstream into the Ross Sea and along the East Antarctic coast.
Previous studies have shown accelerations of West Antarctic glaciers, implying that basal melt...
