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Last Glacial Maximum to Early Holocene Wind Strength in the Mid-latitudes of the Southern Hemisphere from Aeolian Dust in the Tasman Sea

Published online by Cambridge University Press:  20 January 2017

Paul P. Hesse  and
Grant H. McTainsh
Paul P. Hesse
Affiliation:
Department of Physical Geography, Macquarie University, Sydney, New South Wales, 2109, Australia
Grant H. McTainsh
Affiliation:
Faculty of Environmental Sciences, Griffith University, Nathan, Queensland, 4111, Australia
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Abstract

Dust transported by Southern Hemisphere mid-latitude westerly winds from Australia and deposited in the Tasman Sea shows no evidence for stronger winds during the last glacial maximum (LGM), compared to the Holocene. Features of the particle-size distributions of the dust do, however, indicate enhanced dry deposition of dust in the LGM changing to rainfall scavenging during deglaciation and the early Holocene as climate ameliorated. From these results it appears that activation of desert dunefields over 40% of Australia during the LGM was the result of a reduction in stabilizing vegetation and more frequent episodes of sand movement rather than of increased wind strength. The LGM climate of inland Australia must have been considerably more stressful for plants as a result of lower precipitation and/or carbon dioxide stress to achieve the implied levels of surface destabilization. Enhanced atmospheric dust loads in the Southern Hemisphere and deposition over Antarctica were most likely the result of greatly expanded source areas in the mid-latitude southern continents and a weaker hydrological cycle rather than greater entrainment or more efficient transport by stronger winds. During the LGM wind strength appears to have varied regionally, and predominantly in high latitudes, rather than uniformly for all zonal winds.

Keywords

wind strengthTasman SeaQuaternary palaeoclimatesaeolian dust
Type
Research Article
Information
Quaternary Research , Volume 52 , Issue 3 , November 1999 , pp. 343 - 349
Copyright
University of Washington

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References

Alloway, B.V., Stewart, R.B., Neall, V.E., Vucetich, C.G. (1992). Climate of the last glaciation in New Zealand, based on aerosolic quartz influx in an andesitic terrain. Quaternary Research. 38, 170–179.Google Scholar
Ash, J.E., Wasson, R.J. (1983). Vegetation and sand mobility in the Australian dunefield. Zeitschrift fur Geomorphologie, N.F., Suppl. Bd.. 45, 7–25.Google Scholar
Bagnold, R.A. (1937). The size-grading of sand by wind. Proceedings of the Royal Society of London, A. 163, 250–264.Google Scholar
Basile, I., Grousset, F.E., Revel, M., Petit, J.R., Biscaye, P.E., Barkov, N.I. (1997). Patagonian origin of glacial dust deposited in East Antarctica (Vostok and Dome C) during glacial stages 2, 4 and 6. Earth and Planetary Science Letters. 146, 573–589.CrossRefGoogle Scholar
Boven, K.L., Rea, D.K. (1998). Partitioning of eolian and hemipelagic sediment in eastern equatorial Pacific core TR 163-31B and the Late Quaternary paleoclimate of the northern Andes. Journal of Sedimentary Research. 68, 850–855.Google Scholar
Clemens, S.C. (1998). Dust responses to seasonal atmospheric forcing: Proxy evaluation and calibration. Paleoceanography. 13, 471–490.CrossRefGoogle Scholar
Clemens, S.C., Prell, W.L. (1991). One million year record of summer monsoon winds and continental aridity from the Owen Ridge (site 722), Northwest Arabian Sea. Prell, W.L., Niitsuma, N. Proceedings, ODP, Scientific Results. Ocean Drilling Program, College Station., 365–388.Google Scholar
Dare-Edwards, A.J. (1984). Aeolian clay deposits of south-eastern Australia: Parna or loessic clay?. Transacts of the Institute of British Geographers. N.S. 9, 337–344.Google Scholar
De Angelis, M., Legrand, M., Petit, J.R., Barkov, N.I., Korotkevitch, Y.S., Kotlyakov, V.M. (1984). Soluble and insoluble impurities along the 950 m deep Vostok ice core (Antarctica)—Climatic implications. Journal of Atmospheric Chemistry. 1, 215–239.CrossRefGoogle Scholar
deMenocal, P.B., Rind, D. (1993). Sensitivity of Asian and African climate to variations in seasonal insolation, glacial ice cover, sea surface temperature, and Asian orography. Journal of Geophysical Research. 98, 7265–7287.CrossRefGoogle Scholar
Fieller, N.R.J., Flenley, E.C., Olbricht, W. (1992). Statistics of particle size data. Applied Statistics. 41, 127–146.CrossRefGoogle Scholar
Genthon, C. (1992). Simulations of desert dust and sea-salt aerosols in Antarctica with a general circulation model of the atmosphere. Tellus. 44B, 371–389.Google Scholar
Hesse, P.P. (1993). A Quaternary Record of the Australian Environment from Aeolian Dust in Tasman Sea Sediments. Australian National University, Canberra.Google Scholar
Hesse, P.P. (1994). The record of continental dust from Australia in Tasman Sea Sediments. Quaternary Science Reviews. 13, 257–272.CrossRefGoogle Scholar
Hesse, P.P. (1997). Mineral magnetic “tracing” of aeolian dust in southwest Pacific sediments. Palaeogeography, Palaeoclimatology, Palaeoecology. 131, 327–353.CrossRefGoogle Scholar
Hovan, S.A., Rea, D.K., Pisias, N.G. (1991). Late Pleistocene continental climate variability recorded in northwest Pacific sediments. Paleoceanography. 6, 349–370.CrossRefGoogle Scholar
Janecek, T.R. (1985). Eolian sedimentation in the northwest Pacific Ocean: A preliminary examination of the data from Deep-Sea Drilling Project Sites 576 and 578. Turner, K.L. Initial Reports of the Deep-Sea Drilling Project. NSF, Washington., 589–603.Google Scholar
Jenkins, C. J. (1984). Erosion and Deposition at Abyssal Depths in the Tasman Sea. A Seismic Stratigraphic Study of the Bottom-Current Patterns. Ocean Science Institute Report 4, University of Sydney, .Google Scholar
Jenkins, C.J. (1992). Abyssal sediment drifts, erosion and history of bottom water flow in the Tasman Sea southwest of New Zealand. Australian Journal of Earth Sciences. 39, 195–210.CrossRefGoogle Scholar
Joussaume, S. (1989). Desert dust and climate: An investigation using an atmospheric general circulation model. Leinen, M., Sarnthein, M. Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport. Kluwer, Dordrecht., 253–263.Google Scholar
Kershaw, A.P., Nanson, G.C. (1993). The last full glacial cycle in the Australian region. Global and Planetary Change. 7, 1–9.Google Scholar
Knight, A.W., McTainsh, G.H., Simpson, R.W. (1995). Sediment loads in an Australian dust storm: Implications for present and past dust processes. Catena. 24, 195–213.Google Scholar
Kutzbach, J.E., Guetter, P.J., Behling, P.J., Selin, R. (1993). Simulated climate changes: Results of the COHMAP climate-model experiments. Wright, H.E. Global Climates Since the Last Glacial Maximum. University of Minnesota Press, Minneapolis., 24–93.Google Scholar
Le Bolloch, O., Guerzoni, S., Molinaroli, E. (1996). Atmosphere-ocean mass fluxes at two coastal sites in Sardinia. Guerzoni, S., Chester, R. The Impact of Desert Dust across the Mediterranean. Kluwer, Dordrecht., 217–222.CrossRefGoogle Scholar
Li, X., Maring, H., Savoie, D., Voss, K., Prospero, J.M. (1996). Dominance of mineral dust in aerosol light scattering in the North Atlantic trade winds. Nature. 380, 416–419.CrossRefGoogle Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C., Shackleton, N.J. (1987). Age dating and the orbital theory of the ice ages: Development of a high resolution 0 to 300 000 year chronostratigraphy. Quaternary Research. 27, 1–29.CrossRefGoogle Scholar
McTainsh, G. (1989). Quaternary aeolian dust processes and sediments in the Australian region. Quaternary Science Reviews. 8, 235–253.Google Scholar
McTainsh, G.H., Lynch, A.W., Hales, R. (1998). Size characteristics of aeolian dusts in Eastern Australia, with Saharan comparisons. Earth Surface Processes and Landforms. 22, 1207–1216.Google Scholar
Miller, G.H., Magee, J.W., Jull, A.J.T. (1997). Low-latitude glacial cooling in the Southern Hemisphere from amino-acid racemization in emu eggshells. Nature. 385, 241–244.CrossRefGoogle Scholar
Nanson, G.C., Price, D.M., Short, S.A. (1992). Wetting and drying of Australia over the past 300 ka. Geology. 20, 791–794.Google Scholar
Parkin, D.W. (1974). Trade-winds during the glacial cycles. Proceedings of the Royal Society of London, Series A. 337, 73–100.Google Scholar
Parkin, D.W., Shackleton, N.J. (1973). Trade wind and temperature correlations down a deep-sea core off the Saharan coast. Nature. 245, 455–457.Google Scholar
Passlow, V., Wang, P.X., Chivas, A.R. (1997). Late Quaternary palaeoceanography near Tasmania, southern Australia. Palaeogeography, Palaeoclimatology, Palaeoecology. 131, 433–463.CrossRefGoogle Scholar
Petit, J.R., Briat, M., Royer, A. (1981). Ice age aerosol content from East Antarctic ice core samples and past wind strength. Nature. 293, 391–394.CrossRefGoogle Scholar
Porter, S.C., An, Z.-S. (1995). Correlation between climate events in the North Atlantic and China during the last glaciation. Nature. 375, 305–308.Google Scholar
Prospero, J.M., Glaccum, R.A., Nees, R.T. (1981). Atmospheric transport of soil dust from Africa to South America. Nature. 289, 570–572.Google Scholar
Prospero, J.M., Nees, R.T. (1986). Impact of the North African drought and El Nino on mineral dust in the Barbados trade winds. Nature. 320, 735–738.Google Scholar
Rea, D.K. (1994). The paleoclimatic record provided by eolian deposition in the deep sea: The geologic history of wind. Reviews of Geophysics. 32, 159–195.Google Scholar
Rea, D.K., Hovan, S.A. (1995). Grain size distribution and depositional processes of the mineral component of abyssal sediments: Lessons from the North Pacific. Paleoceanography. 10, 251–258.Google Scholar
Rea, D.K., Janecek, T.R. (1981). Mass-accumulation rates of the non-authigenic inorganic crystalline (eolian) component of deep-sea sediments from the western Mid-Pacific Mountains, Deep Sea Drilling Project Site 463. Stout, L.N. Initial Reports of the Deep Sea Drilling Project. NSF, Washington., 653–659.Google Scholar
Rea, D.K., Pisias, N.G., Newberry, T. (1991). Late Pleistocene paleoclimatology of the central equatorial Pacific: Flux patterns of biogenic sediments. Paleoceanography. 6, 227–244.Google Scholar
Robson, D, Fieller, N and Stillman, E.(1997). Shefsize, Dept. Probability and Statistics. University of Sheffield, .Google Scholar
Sarnthein, M., Tetzlaff, G., Koopmann, B., Wolter, K., Pflaumann, U. (1981). Glacial and interglacial wind regimes over the eastern subtropical Atlantic and North-West Africa. Nature. 293, 193–196.Google Scholar
Schutz, L. (1979). Saharan dust transport over the North Atlantic Ocean—Model calculations and measurements. Morales, C. Saharan Dust, Mobilization, Transport, Deposition. Wiley, Chichester., 267–277.Google Scholar
Steffensen, J.P. (1997). The size distribution of microparticles from selected segments of the Greenland Ice Core Project ice core representing different climatic periods. Journal of Geophysical Research. 102, 26,755–26,763.Google Scholar
Tegen, I., Lacis, A.A., Fung, I. (1996). The influence on climate forcing of mineral aerosols from disturbed soils. Nature. 380, 419–422.CrossRefGoogle Scholar
Thompson, L.G. (1977). Variations in microparticle concentration, size distribution and elemental composition found in Camp Century, Greenland and Byrd station, Antarctica, deep ice cores. Proceedings of the Grenoble Symposium on Isotopes and Impurities in Snow and Ice. p. 351–364.Google Scholar
Wasson, R.J. (1984). Late Quaternary palaeoenvironments in the desert dunefields of Australia. Vogel, J.C. Late Cainozoic Palaeoclimates of the Southern Hemisphere. Balkema, Rotterdam., 183–208.Google Scholar
Wasson, R.J. (1987). Desert dune building, dust raising and palaeoclimate in the southern hemisphere during the last 280,000 year. CLIMANZ 3. CSIRODivision of Water Resources, Melbourne., p. 123–137.Google Scholar
Wilkniss, P.E., Larson, R.E., Bressan, D.J., Steranka, J. (1974). Atmospheric radon and continental dust near the Antarctic and their correlation with air mass trajectories computed from Nimbus 5 satellite photographs. Journal of Applied Meteorology. 13, 512–515.Google Scholar
Yu, B., Hesse, P.P., Neil, D.T. (1993). The relationship between antecedent regional rainfall and the occurrence of dust events at Mildura, Australia. Journal of Arid Environments. 24, 109–124.Google Scholar
Yung, Y.L., Lee, T., Wang, C.-H., Shieh, Y.-T. (1996). Dust: A diagnostic of the hydrologic cycle during the Last Glacial Maximum. Science. 271, 962–963.CrossRefGoogle Scholar