Articles | Volume 12, issue 12
https://doi.org/10.5194/cp-12-2241-2016
© Author(s) 2016. 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/cp-12-2241-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
19 Dec 2016
Research article |
| 19 Dec 2016
Sea ice led to poleward-shifted winds at the Last Glacial Maximum: the influence of state dependency on CMIP5 and PMIP3 models
British Antarctic Survey, Cambridge, UK
Dominic Hodgson
British Antarctic Survey, Cambridge, UK
Thomas J. Bracegirdle
British Antarctic Survey, Cambridge, UK
Claire Allen
British Antarctic Survey, Cambridge, UK
Bianca Perren
British Antarctic Survey, Cambridge, UK
Stephen Roberts
British Antarctic Survey, Cambridge, UK
Agatha M. de Boer
Bert Bolin Centre for Climate Research, Department of Geological Sciences, Stockholm
University, Stockhom, Sweden
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36 citations as recorded by crossref.
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- Climate and ecology of the palaeo-Agulhas Plain from stable carbon and oxygen isotopes in bovid tooth enamel from Nelson Bay Cave, South Africa J. Sealy et al. 10.1016/j.quascirev.2019.105974
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36 citations as recorded by crossref.
- The Roles of Wind and Sea Ice in Driving the Deglacial Change in the Southern Ocean Upwelling: A Modeling Study G. Mandal et al. 10.3390/su13010353
- Holocene dynamics of the Southern Hemisphere westerly winds and possible links to CO2 outgassing K. Saunders et al. 10.1038/s41561-018-0186-5
- Three modes of climate change since the Last Glacial Maximum in arid and semi-arid regions of the Asian continent Y. Zhang & Y. Li 10.1007/s11442-022-1942-4
- Paleoclimatic context of projected future warming in southern South America A. Berman et al. 10.1007/s00704-020-03196-2
- Evolution of Atlantic Meridional Overturning Circulation since the last glaciation: model simulations and relevance to present and future Z. Liu 10.1098/rsta.2022.0190
- An asymmetric relationship between Tibetan Plateau surface temperature regimes and oceanic–atmospheric circulations T. Bafitlhile & Y. Liu 10.1002/joc.8179
- Climate and ecology of the palaeo-Agulhas Plain from stable carbon and oxygen isotopes in bovid tooth enamel from Nelson Bay Cave, South Africa J. Sealy et al. 10.1016/j.quascirev.2019.105974
- Simulated Southern Ocean Upwelling at the Last Glacial Maximum and Early Deglaciation: The Role of Eddy‐Induced Overturning Circulation C. Chen & G. Wang 10.1029/2021GL092880
- Variable C∕P composition of organic production and its effect on ocean carbon storage in glacial-like model simulations M. Ödalen et al. 10.5194/bg-17-2219-2020
- A Last Glacial Maximum forcing dataset for ocean modelling A. Morée & J. Schwinger 10.5194/essd-12-2971-2020
- Poleward Shift in the Southern Hemisphere Westerly Winds Synchronous With the Deglacial Rise in CO2 W. Gray et al. 10.1029/2023PA004666
- Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
- Evaluating seasonal sea-ice cover over the Southern Ocean at the Last Glacial Maximum R. Green et al. 10.5194/cp-18-845-2022
- Beyond the bipolar seesaw: Toward a process understanding of interhemispheric coupling J. Pedro et al. 10.1016/j.quascirev.2018.05.005
- The Impact of Southern Ocean Topographic Barriers on the Ocean Circulation and the Overlying Atmosphere A. de Boer et al. 10.1175/JCLI-D-21-0896.1
- A glacial chronology for sub-Antarctic Marion Island from MIS 2 and MIS 3 E. Rudolph et al. 10.1016/j.quascirev.2023.108485
- Summer Westerly Jet in Northern Hemisphere during the Mid-Holocene: A Multi-Model Study C. Xu et al. 10.3390/atmos11111193
- Downscaling Last Glacial Maximum climate over southern Africa F. Engelbrecht et al. 10.1016/j.quascirev.2019.105879
- A multi-model analysis of moisture changes during the last glacial maximum S. Liu et al. 10.1016/j.quascirev.2018.05.029
- Wet–dry status change in global closed basins between the mid-Holocene and the Last Glacial Maximum and its implication for future projection X. Zhang et al. 10.5194/cp-16-1987-2020
- A Global Glacial Ocean State Estimate Constrained by Upper-Ocean Temperature Proxies D. Amrhein et al. 10.1175/JCLI-D-17-0769.1
- Northern Westerlies during the Last Glacial Maximum: Results from CMIP5 Simulations N. Wang et al. 10.1175/JCLI-D-17-0314.1
- New Record of Dust Input and Provenance During Glacial Periods in Western Australia Shelf (IODP Expedition 356, Site U1461) from the Middle to Late Pleistocene M. Courtillat et al. 10.3390/atmos11111251
- Seasonal Variation of the Westerly Jet over Asia in the Last Glacial Maximum: Role of the Tibetan Plateau Heating J. Lei et al. 10.1175/JCLI-D-20-0438.1
- Unraveling the complexities of the Last Glacial Maximum climate: the role of individual boundary conditions and forcings X. Shi et al. 10.5194/cp-19-2157-2023
- Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate T. Bracegirdle et al. 10.3390/geosciences9060255
- The influence of the ocean circulation state on ocean carbon storage and CO<sub>2</sub> drawdown potential in an Earth system model M. Ödalen et al. 10.5194/bg-15-1367-2018
- Simultaneous seasonal dry/wet signals in eastern and central Asia since the Last Glacial Maximum S. Peng et al. 10.5194/cp-20-2415-2024
- Linking Glacial‐Interglacial States to Multiple Equilibria of Climate D. Ferreira et al. 10.1029/2018GL077019
- CMIP5 Diversity in Southern Westerly Jet Projections Related to Historical Sea Ice Area: Strong Link to Strengthening and Weak Link to Shift T. Bracegirdle et al. 10.1175/JCLI-D-17-0320.1
- Modeling Water-Mass Distributions in the Modern and LGM Ocean: Circulation Change and Isopycnal and Diapycnal Mixing C. Jones & R. Abernathey 10.1175/JPO-D-20-0204.1
- A South Atlantic island record uncovers shifts in westerlies and hydroclimate during the last glacial S. Björck et al. 10.5194/cp-15-1939-2019
- Early glacial maximum and deglaciation at sub-Antarctic Marion Island from cosmogenic 36Cl exposure dating E. Rudolph et al. 10.1016/j.quascirev.2020.106208
- The Driving Mechanisms on Southern Ocean Upwelling Change during the Last Deglaciation W. Liu et al. 10.3390/geosciences11070266
- Glacial–Interglacial Precipitation Changes D. McGee 10.1146/annurev-marine-010419-010859
- The Roles of Orbital and Meltwater Climate Forcings on the Southern Ocean Dynamics during the Last Deglaciation G. Mandal et al. 10.3390/su14052927
Saved (preprint)
Latest update: 14 Dec 2024
Short summary
Latitudinal shifts in the Southern Ocean westerly wind jet could explain large observed changes in the glacial to interglacial ocean CO2 inventory. However there is considerable disagreement in modelled deglacial-warming jet shifts. Here multi-model output is used to show that expansion of sea ice during the glacial period likely caused a slight poleward shift and intensification in the westerly wind jet. Issues with model representation of the winds caused much of the previous disagreement.
Latitudinal shifts in the Southern Ocean westerly wind jet could explain large observed changes...
