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.
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
Bard E, Rickaby R (2009) Migration of the subtropical front as a modulator of glacial climate. Nature 460:380–393
Boos WR (2012) Thermodynamic scaling of the hydrological cycle of the Last Glacial Maximum. J Clim 25:992–1006
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
Brady EC, Otto-Bliesner BL, Kay JE, Rosenbloom N (2013) Sensitivity to glacial forcing in the CCSM4. J Clim 26:1901–1925
Chavaillaz Y, Codron F, Kageyama M (2013) Southern westerlies in LGM and future (RCP4. 5) climates. Clim Past 9:517–524
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
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
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
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
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
Held IM, Soden BJ (2006) Robust responses of the hydrological cycle to global warming. J Clim 19:5686–5699
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
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
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
Kalney E et al (1996) The NCEP/NCAR 40-year re-analysis project. Bull Am Meteorol Soc 77:437–471
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
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
Kohfeld KE, Harrison SP (2001) DIRTMAP: the geologic record of dust. Earth Sci Rev 54:81–114
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
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
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
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
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
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
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
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
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
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
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
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
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
Rojas M (2013) Sensitivity of Southern Hemisphere circulation to LGM and 4xCO2 climates. Geophys Res Lett 40:1–6
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
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
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
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
Taylor KE, Stouffer RJ, Meehl GA (2012) An overview of CMIP5 and the experiment design. Bull Am Meteorol Soc 93:485–498
Toggweiler JR, Russell JL, Carson SR (2006) Midlatitude westerlies, atmospheric CO2, and climate change during the ice ages. Paleoceanography 21:PA2005
Valdes PJ (2000) South American paleoclimate model simulations: how reliable are the models? J Quat Sci 15:357–368
Waelbroeck C et al (2009) Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum. Nat Geosci 2:127–132
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
Wolff EW et al (2006) Southern Ocean sea-ice extent, productivity and iron flux over the past eight glacial cycles. Nature 440:491–496
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
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
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
Corresponding author
Rights and permissions
About this article
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
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00382-015-2530-4