Skip to main content
Log in

The de-correlation of westerly winds and westerly-wind stress over the Southern Ocean during the Last Glacial Maximum

  • Published:
Climate Dynamics Aims and scope Submit manuscript

Abstract

Motivated by indications from paleo-evidence, this paper investigates the changes of the Southern Westerly Winds (SWW) and westerly-wind stress between the Last Glacial Maximum (LGM) and pre-industrial in the PMIP3/CMIP5 simulations, highlighting the role of Antarctic sea ice in modulating the wind effect on ocean. Particularly, a de-correlation occurs between the changes in SWW and westerly-wind stress, caused primarily by an equatorward expansion of winter Antarctic sea ice that undermines the efficacy of wind in generating stress over the liquid ocean. Such de-correlation may reflect the LGM condition in reality, in view of the fact that the model which simulates this condition has most fidelity in simulating modern SWW and Antarctic sea ice. Therein two models stand out for their agreements with paleo-evidence regarding the change of SWW and the westerly-wind stress. They simulate strengthened and poleward-migrated LGM SWW in the atmosphere, consistent with the indications from dust records. Whilst in the ocean, they well capture an equatorward-shifted pattern of the observed oceanic front shift, with most pronounced equatorward-shifted westerly wind stress during the LGM.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Anderson RF, Ali S, Bradtmiller L, Fleisher MQ, Burckle LH (2009) Wind-driven upwelling in the Southern Ocean and the deglacial rise of atmospheric CO2. Science 323:1443–1448

    Article  Google Scholar 

  • Bard E, Rickaby R (2009) Migration of the subtropical front as a modulator of glacial climate. Nature 460:380–393

    Article  Google Scholar 

  • Boos WR (2012) Thermodynamic scaling of the hydrological cycle of the Last Glacial Maximum. J Clim 25:992–1006

    Article  Google Scholar 

  • Braconnot P, Harrison SP, Kageyama M, Bartlein PJ, Masson-Delmotte V, Abe-Ouchi A, Otto-Bliesner BL, Zhao Y (2012) Evaluation of climate models using palaeoclimatic data. Nat Clim Change 2:417–424

    Article  Google Scholar 

  • Brady EC, Otto-Bliesner BL, Kay JE, Rosenbloom N (2013) Sensitivity to glacial forcing in the CCSM4. J Clim 26:1901–1925

    Article  Google Scholar 

  • Chavaillaz Y, Codron F, Kageyama M (2013) Southern westerlies in LGM and future (RCP4. 5) climates. Clim Past 9:517–524

    Article  Google Scholar 

  • Cook KH, Vizy EK (2006) Coupled model simulations of the West African monsoon system: twentieth-and twenty-first-century simulations. J Clim 19:3681–3703

    Article  Google Scholar 

  • Delmonte B, Petit JR, Maggi V (2002) Glacial to Holocene implications of the new 27000-year dust record from the EPICA Dome C (East Antarctica) ice core. Clim Dyn 18:647–660

    Article  Google Scholar 

  • Fraser CI, Nikula R, Spencer HG, Waters JM (2009) Kelp genes reveal effects of subantarctic sea ice during the Last Glacial Maximum. Proc Natl Acad Sci 106:3249–3253

    Article  Google Scholar 

  • Gersonde R et al (2003) Last glacial sea surface temperatures and sea-ice extent in the Southern Ocean (Atlantic-Indian sector): a multiproxy approach. Paleoceanography. doi:10.1029/2002PA000809

    Google Scholar 

  • Gersonde R, Crosta X, Abelmann A, Armand L (2005) Sea-surface temperature and sea ice distribution of the Southern Ocean at the EPILOG Last Glacial Maximum—a circum-Antarctic view based on siliceous microfossil records. Quat Sci Rev 24:869–896

    Article  Google Scholar 

  • Held IM, Soden BJ (2006) Robust responses of the hydrological cycle to global warming. J Clim 19:5686–5699

    Article  Google Scholar 

  • Heusser L, Heusser CJ, Mix A, McManus J (2006a) Chilean and Southeast Pacific paleoclimate variations during the last glacial cycle: directly correlated pollen and d18O records from ODP Site 1234. Quat Sci Rev 25:3404–3415

    Article  Google Scholar 

  • Heusser L, Heusser CJ, Pisias N (2006b) Vegetation and climate dynamics of southern Chile during the past 50,000 years: results of ODP Site 1233 pollen analysis. Quat Sci Rev 25:474–485

    Article  Google Scholar 

  • Hulton NRJ, Purvesa RS, McCullocha RD, Sugdena DE, Bentleyb MJ (2002) The last glacial maximum and deglaciation in southern South America. Quat Sci Rev 21:233–241

    Article  Google Scholar 

  • Kalney E et al (1996) The NCEP/NCAR 40-year re-analysis project. Bull Am Meteorol Soc 77:437–471

    Article  Google Scholar 

  • Kim SJ, Flato GM, Boer GJ (2003) A coupled climate simulation of the Last Glacial Maximum, part 2: approach to equilibrium. Clim Dyn 20:635–661

    Google Scholar 

  • Kitoh A, Murakami S, Kiode H (2001) A simulation of the last glacial maximum with a coupled atmosphere–ocean GCM. Geophys Res Lett 28:2221–2224

    Article  Google Scholar 

  • Kohfeld KE, Harrison SP (2001) DIRTMAP: the geologic record of dust. Earth Sci Rev 54:81–114

    Article  Google Scholar 

  • Kohfeld KE, Graham RM, de Boer AM, Sime LC, Wolff EW, Le Quéré C, Bopp L (2013) Southern Hemisphere westerly wind changes during the Last Glacial Maximum: paleo-data synthesis. Quat Sci Rev 68:76–95

    Article  Google Scholar 

  • Lamy F, Kaiser J, Ninnemann U, Hebbeln D, Arz HW, Stoner J (2004) Antarctic timing of surface water changes off Chile and Patagonian ice sheet response. Science 304:1959–1962

    Article  Google Scholar 

  • Mahowald NM et al (2006) Change in atmospheric mineral aerosols in response to climate: last glacial period pre-industrial, modern and doubled carbon dioxide climates. J Geophys Res Atmos. doi:10.1029/2005JD006653

    Google Scholar 

  • Markgraf V (1989) Paleoclimates in central and South America since 18,000 BP based on pollen and lake-level records. Quat Sci Rev 8:1–24

    Article  Google Scholar 

  • Menviel L, Timmermann A, Mouchet A, Timm O (2008) Climate and marine carbon cycle response to changes in the strength of the Southern Hemispheric westerlies. Paleoceanography 23:PA4201

    Google Scholar 

  • Nelson CS, Hendy IL, Neil HL, Hendy CH, Weaver PPE (2000) Last glacial jetting of cold waters through the Subtropical convergence zone in the Southwest Pacific off eastern New Zealand, and some geological implications. Palaeogeogr Palaeoclimatol Palaeoecol 156:103–121

    Article  Google Scholar 

  • Orsi AH, Whitworth T III, Nowlin WD Jr (1995) On the meridional extent and fronts of the Antarctic Circumpolar Current. Deep Sea Res I 42:641–673

    Article  Google Scholar 

  • Otto-Bliesner B, Brady EC, Clauzet G, Thomas R, Levis S, Kothavala Z (2006) Last glacial maximum and Holocene climate in CCSM3. J Clim 19:2526–2544

    Article  Google Scholar 

  • Paruelo JM, Beltran A, Jobbagy E, Sala OE, Golluscio RA (1998) The climate of Patagonia: general patterns and controls on biotic. Ecol Austral 8:85–101

    Google Scholar 

  • Peeters FJC et al (2004) Vigorous exchange between the Indian and Atlantic Oceans at the end of the past five glacial periods. Nature 430:661–665

    Article  Google Scholar 

  • Petit JR et al (1999) Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature 399:429–436

    Article  Google Scholar 

  • Prell WL et al (1980) Surface circulation of the Indian Ocean during the last glacial maximum, approximately 18,000 yr BP. Quat Res 14:309–336

    Article  Google Scholar 

  • Risien CM, Chelton DB (2008) A global climatology of surface wind and wind stress fields from eight years of QuikSCAT scatterometer data. J Phys Oceanogr 38:2379–2413

    Article  Google Scholar 

  • Rojas M (2013) Sensitivity of Southern Hemisphere circulation to LGM and 4xCO2 climates. Geophys Res Lett 40:1–6

    Article  Google Scholar 

  • Rojas M, Moreno P, Kageyama M, Crucifix M, Hewitt C, Abe-Ouchi A, Ohgaito R, Brady EC, Hope P (2009) The southern westerlies during the last glacial maximum in PMIP2 simulations. Clim Dyn 32:525–548

    Article  Google Scholar 

  • Schäfer-Neth C, Paul A (2003) The Atlantic Ocean at the last glacial maximum: 1. objective mapping of the GLAMAP sea-surface conditions. In: Wefer G, Mulitza S, Ratmeyer V (eds) The South Atlantic in the Late Quaternary: material budget and current systems. Springer, Berlin, pp 531–548

    Chapter  Google Scholar 

  • Shin SI, Liu Z, Otto-Bliesner B, Brady EC, Kutzbach J, Harrison S (2003) A simulation of the Last Glacial Maximum climate using the NCAR-CCSM. Clim Dyn 20:127–151

    Google Scholar 

  • Siani G, Michel E, De Pol-Holz R, DeVries T, Lamy F, Carel M, Isguder G, Dewilde F, Lourantou A (2013) Carbon isotope records reveal precise timing of enhanced Southern Ocean upwelling during the last deglaciation. Nat Commun 4. doi:10.1038/ncomms3758

  • Sime LC, Kohfeld KE, Le Quéré C, Wolff EW, de Boer AM, Graham RM, Bopp L (2013) Southern Hemisphere westerly wind changes during the Last Glacial Maximum: model-data comparison. Quat Sci Rev 64:104–120

    Article  Google Scholar 

  • Taylor KE, Stouffer RJ, Meehl GA (2012) An overview of CMIP5 and the experiment design. Bull Am Meteorol Soc 93:485–498

    Article  Google Scholar 

  • Toggweiler JR, Russell JL, Carson SR (2006) Midlatitude westerlies, atmospheric CO2, and climate change during the ice ages. Paleoceanography 21:PA2005

    Article  Google Scholar 

  • Valdes PJ (2000) South American paleoclimate model simulations: how reliable are the models? J Quat Sci 15:357–368

    Article  Google Scholar 

  • Waelbroeck C et al (2009) Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum. Nat Geosci 2:127–132

    Article  Google Scholar 

  • Williams NJ, Harle KJ, Gale SJ, Heijnis H (2006) The vegetation history of the last glacial–interglacial cycle in eastern New South Wales, Australia. J Quat Sci 21:735–750

    Article  Google Scholar 

  • Wolff EW et al (2006) Southern Ocean sea-ice extent, productivity and iron flux over the past eight glacial cycles. Nature 440:491–496

    Article  Google Scholar 

  • Wyrwoll K-H, Dong B, Valdes P (2000) On the position of southern westerlies at the last glacial maximum: an outline of AGCM simulation results and evaluation of their implications. Quat Sci Rev 19:881–898

    Article  Google Scholar 

  • Yang J (2006) The seasonal variability of the Arctic Ocean Ekman transport and its role in the mixed layer heat and salt fluxes. J Clim 19:5366–5387

    Article  Google Scholar 

Download references

Acknowledgments

This work is primarily supported by NSF AGS-1249145. Jian Lu and L. Ruby Leung were partly supported by the Office of Science of the US Department of Energy as part of the Regional and Global Climate Modeling program. The Pacific Northwest National Laboratory is operated for DOE by Battelle Memorial Institute under contract DE-AC05-76RL01830.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Wei Liu.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Liu, W., Lu, J., Leung, L.R. et al. The de-correlation of westerly winds and westerly-wind stress over the Southern Ocean during the Last Glacial Maximum. Clim Dyn 45, 3157–3168 (2015). https://doi.org/10.1007/s00382-015-2530-4

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00382-015-2530-4

Keywords

Navigation