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Earth rotation, ocean circulation and paleoclimate

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Abstract

During the 20 Ka glaciation maximum Earth's rate of rotation was significantly faster. The subsequent glacial eustatic rise in sea level meant an increase of the equatorial radius and hence led to a general deceleration in the Earth's rate of rotation. At about 6000 BP the glacial eustatic rise in sea level finished and a new situation began which was characterized by feedback interchanges of angular momentum between the solid Earth and the hydrosphere. There is a strong linkage between Earth's rate of rotation — total as well as differential — and the changes in ocean surface circulation. The ocean circulation changes are, in their turn, strongly linked to the paleoclimatic evolution of the boardering land masses. This is due to the high heat-storing capacity of the oceans, the ocean/ atmosphere heat flux, and the ocean/land interaction via heat transport by the winds. Consequently, we see a causal connection between Earth's rotation, oceanic circulation, ocean/atmosphere heating, atmospheric (wind) heat transport and continental paleoclimatic changes. We propose that the paleoclimatic changes on the decadal to millennial time scale are primarily driven by this mechanism. Observational data of changes in ocean water masses and paleoclimate are presented for the 20 Ka situation, for the high-amplitude changes 13-10 Ka ago, for the decadal-to-century changes during the Holocene, for the last centuries' instrumental data and for the ENSO-events. This implies that the oceanic system (the ocean surface circulation system) has a much more important role than previously appreciated.

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References

  • Alley, R. B.; Meese, D. A.; Shuman, C. A.; Gow, A. J.; Taylor, K. C.; Grootes, P. M,; White, J. W. C.; Ram, M.; Waddington, E. D.; Mayewski, P. A.; Zielinski, G. A.: Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event. Nature 362, 527–529 (1993)

    Google Scholar 

  • Bard, E.; Arnold, M.; Duprat, P. M. J,; Moyes, J.; Duplessy, J. C.: Retreat velocity of the North Atlanic polar front during the last deglaciation determined by14C acceleration mass spectronomy. Nature 328, 791–794 (1987)

    Google Scholar 

  • Barnes, R. T. H,; Hide, R.; White, A. A.; Wilson, C. A.: Atmospheric angular momentum correlated with length of the day changes and polar motion. Procedings of the Royal Society, London, Ser, A, 387, 31–73 (1983)

    Google Scholar 

  • Barron, J. A.; Keller, G.: Widespread Miocene deep-sea hiatuses: Coincidence with periods of glacial cooling. Geology 10, 577–581 (1982)

    Google Scholar 

  • Björklund, K. R. et al.: Evolution of the Upper Quaternary depositional environment in the Skagerak, a synthesis. Norsk geol. Tidsskr. 65, 139–149 (1985)

    Google Scholar 

  • Cachão, M.: Quaternary calcareous nannofossil assemblages and time series from Iberian Occidental margin. Abstracts, 1st symposium on the Atlantic Iberian continental margin, p. 9–10, Lissabon 1994.

  • Damon, P. E.; Linick, T. W.: Geomagnetic-heliomagnetic modulation of atmospheric radiocarbon production. Radiocarbon 28: 266–278 (1986)

    Google Scholar 

  • Dieke, R. H.: The secular acceleration of the earth's rotation and cosmology. In: Marsden, G. B.; Cameron, A. G. W. (ed.), The Earth-Moon System. 98–164. Plenum Press, New York 1966.

    Google Scholar 

  • Duplessy, J. C.: Palaeoceanographic changes in the North Atlantic at the end of the last glaciation. Lecture, QRA Annual Meeting, Edinburgh 1995, on “The Lateglacial palaeoceanography of the North Atlantic margins” (1995)

  • Duplessy, J. C.; Delibrias, G.; Turon, J. L.; Pujol, C.; Duprat, J.: Deglacial warming of the northeastern Atlantic Ocean: correlation with paleoclimatic evolution of the European continent. Palaeogeography Palaeoclimatology Palaeoecology 35, 121–144 (1981)

    Google Scholar 

  • Duplessy, J. C.; Bard, E.; Arnold, M.; Shackleton, N. J.; Dupart, J.; Labeyrie, L.: How fast did the oceans-atmosphere system run during the last deglaciation? Earth Planetary Sci. Letters 103, 27–40 (1991)

    Google Scholar 

  • Eddy, J. A.: The Maunder Minimum. Science 192: 1189–1202 (1976)

    Google Scholar 

  • Fatela, F.; Duprat, J.; Pujos, A.: How far southwards migrated the polar front, along the West Iberian margin, at 17,000 years BP?. GAIA, Revista de Geociencias, Universidade de Lisboa 8, 169–173 (1994)

    Google Scholar 

  • Frenzel, B. (ed.): Climatic trends and anomalies in Europe 1675–1715. Paläoklimaforschung 13, 1–479 (1994)

  • GRIP (Greenland Ice-core Project Members): Climate instability during the last interglacial period recorded in the GRIP ice core. Nature 364, 203–207 (1993)

    Google Scholar 

  • Golovkov, V. P.: Dynamics of the geomagnetic field and the internal structure of the Earth. In: Bucha, V. (ed.), Magnetic field and processes in the Earth's interior, p 395–501. Czech. Acad. Sci., Academia, Prague 1983.

    Google Scholar 

  • Guiot, J.: The combination of historical documents and biological data in the reconstruction of climate variations in space and time. Paläoklimatforschung/Paleoclimatic Research 7, Special Issue 2 (Frenzel, B. (ed.)), 93–104 (1992)

  • Hald, M.: Palaeoceanography on the European Arctic margin during the last deglaciation. Lecture, QRA Annual Meeting, Edinburgh 1995, on “The Lateglacial palaeoceanography of the North Atlanic margins” (1995).

  • Kalinin, Y. D.; Kiselev, V. M.: Solar conditionality of changes of the length of the day, the seismicity of the Earth and the geomagnetic moment. Geomag. Aeromag. 16, 858–800 (1976)

    Google Scholar 

  • Kellogg, T. B.: Late-Glacial — Holocene high-frequency climatic changes in deep-sea cores from the Denmark Strait. In: Mörner, N.-A.; Karlén, W. (eds.), Climatic Changes on a Yearly to Millennial Basis. pp. 123–133. Reidel, Dordrecht 1984.

    Google Scholar 

  • Koc, N.: Lateglacial North Atlantic sea-surface temperatures and gradients. Lecture, QRA Annual Meeting, Edinburgh 1995, on “The Lateglacial palaeoceanography of the North Atlantic margins” (1995).

  • Krymsky, P. F.: Mechanisms of impulsive moment transfer from solar wind to the Earth. Abstracts, IUGG XXI, A, 137, Boulder 1995.

    Google Scholar 

  • Lamb, H. H.: Climatic variations and changes in the wind and ocean circulation: The Little Ice Ages in the Northeast Atlantic. Quaternary Res. 11, 1–20 (1979)

    Google Scholar 

  • Lamb, H. H.: Some studies of the Little Ice Age of recent centuries and its great storms. In: Mörner, N.-A; Karlén, W. (eds.), Climatic Changes on a Yearly to Millennial Basis, pp. 309–329, Reidel, Dordrecht 1984.

    Google Scholar 

  • Lean, J.; Rind, D.: Solar variability: implications for global change. EOS 75 (1), 5–7 (1994)

    Google Scholar 

  • Legrand, J. P.; Le Goff, M.; Mazaudier, C.; Schröder, W.: L'activité aurale au XVIIe siècle. Comptes Rendus, Série Générale 8, 181–219 (1991)

    Google Scholar 

  • LeMouël, J. P.; Gire, C.; Jaupart, C.: Sur le corrélation entre la figure de la terre et les mouvements animant les couches externes de son noyau. Comptes Rendus Academie Scientifique, Paris B303, 613–618 (1986)

    Google Scholar 

  • Libreiro, S. M.; Moreno, J. C.; Abrantes, F.; Weaver, P. P. E.; McCave, I. N.: Late quaternary paleoceanography off Iberia: Tore Seamount (39°N, 12°W). Abstracts, 1st symposium on the Atlantic Iberian continental margin. Lisbon 1994, p, 28 (1994)

  • Mangerud, J.: Late Weichselian marine sediments containing shells, foraminifera, and pollen, at Agotnes, Western Norway. Norsk Geol. Tidsskr. 57, 23–54 (1977)

    Google Scholar 

  • Marsden, G. B.; Cameron, A. G. W. (eds.): The Earth-Moon System. Plenum Press, New York 1966.

    Google Scholar 

  • Moore, J. R.; van Andel, T. H.; Sancetta, S.; Psias, N.: Cenozoic hiatuses in marine sediments. Micropaleontology 24, 113–138 (1978)

    Google Scholar 

  • Mörner, N.-A.: The Late Quaternary history of the Kattegatt Sea and the Swedish West Coast; deglaciation, shorelevel displacement, chronology, isostasy and eustasy. Sveriges Geol. Undersök. C-640, 1–487 (1969)

    Google Scholar 

  • Mörner, N.-A.: Summary and conclusions. Boreas 5, 247–256 (1976)

    Google Scholar 

  • Mörner, N.-A.: The northwest European “sea level laboratory” and regional Holocene eustasy. Palaeogeogr., Palaeoclim., Palaeoecol. 29, 281–300 (1980)

    Google Scholar 

  • Mörner, N.-A.: Terrestrial, solar and galactic origin of the Earth's geophysical variables. Geogr. Ann, 66A, 1–9 (1984a)

    Google Scholar 

  • Mörner, N.-A.: Planetary, solar, atmospheric, hydrospheric and endogene processes as origin of climatic changes on the Earth. In: Mörner, N.-A.; Karlén, W. (eds.), Climatic Changes on a Yearly to Millennial Basis, pp. 483–507. Reidel, Dordrecht 1984.

    Google Scholar 

  • Mörner, N.-A.: Climatic changes on a yearly to millennial basis. Concluding remarks, In: Mörner, N.-A.; Karlén, W. (eds.), Climatic Changes on a Yearly to Millennial Basis, Reidel, pp. 637–651. Reidel, Dordrecht 1984c.

    Google Scholar 

  • Mörner, N.-A.: Terrestrial variations within given energy, mass and momentum budgets; Paleoclimate, sea level, paleomagnetism, differential rotation and geodynamics. In: Stephenson, F. R.; Wolfendale, A. W. (eds.), Secular Solar and Geomagnetic Variations in the last 10,000 years, pp. 455–478. Kluwer Acad. Press, Dordrecht-Boston-London 1988.

    Google Scholar 

  • Mörner, N.-A.: Changes in the Earth's rate of rotation on an EI Niño to century basis. In: Lowes, F. J. et al. (eds.), Geomagnetism and Palaeomagnetism, pp. 45–53. Kluwer Academic Publishers, Dordrecht-Boston-London 1989.

    Google Scholar 

  • Mörner, N.-A.: Transpolar VGP shifts and Earth's rotation. Geophysics and Astrophysics Fluid Dynamics 60, 149–155 (1991)

    Google Scholar 

  • Mörner, N.-A.: Sea level changes and Earth's rotation. J. Coastal Res. 8: 966–971 (1992)

    Google Scholar 

  • Mörner, N.-A.: Global Change: the high-amplitude changes 13-10 Ka ago — novel aspects. Global and Planetary Change 7, 243–250 (1993a)

    Google Scholar 

  • Mörner, N.-A.: Global Change: the last millennia. Global and Planetary Change 7, 211–217 (1993b)

    Google Scholar 

  • Mörner, N.-A.: Present El Niño-ENSO events and past Super-ENSO events. Bulletin de Institut Francais d'Etudes Andines 22 (1), 3–12 (1993c)

    Google Scholar 

  • Mörner, N.-A.: Internal response to orbital forcing and external cyclic sedimentary sequences. Spec. Publ. Int. Ass. Sediment. 19, 25–33 (1994a)

    Google Scholar 

  • Mörner, N.-A.: The Maunder Minimum. In: Climatic trends and anomalies in Europe 1675–1715 (Frenzel, B., ed.), Paläoklimaforschung 13, 1–8 (1994b)

    Google Scholar 

  • Mörner, N.-A.: Climatic-eustatic changes in the last 2000 years. the decade-to-entury variability, super-ENSO events and historical cold phases. Proc. NATO conference on Climatic Changes during the last 2000 years, in press, 1995a.

  • Mörner, N.-A.: Earth rotation, ocean circulation and paleoclimate. The North Atlantic — European case. In: Andrews, J.; Austin, B.; Bergsten, H.; Jennings, A. (eds.), The Lateglacial palaeoceanography of the North Atlantic margins. Geol. Soc. London, Spec. Publ., in press 1995b.

  • Mörner, N.-A.: Sea level and climate — The decadal-to-century signals. J. Coastal Res./Spec. Iss. 17, in press (1995c)

  • Mörner, N.-A.; Wallin, B.: A 10,000 year temperature record from Gotland, Sweden. Palaeogeogr. Palaeoclim. Palaeoecol. 21, 113–138 (1976)

    Google Scholar 

  • Morrison, L. V.; Stephenson, F. P.: Long-term changes in rotation of the Earth; 700 BC to AD 1980. Phil. Trans. R. Soc. Lond., A313: 47–70 (1984)

    Google Scholar 

  • Peacock, J. D. Marine molluscan proxy data applied to Scottish Late-Glacial and Flandrian sites. Lecture, QRA Annual Meeting, Edinburgh 1995, on “The Lateglacial palaeoceanography of the North Atlanic margins” (1995).

  • Pettersson, O.: Klimatförändringar i historisk och förhistorisk tid. Kungl. Sv. Vet. Akad. Handl. 51 (2), 1–81 (1913)

    Google Scholar 

  • Polyak, L.: Foraminiferal record and environmental change in the eastern Barents Sea. Lecture, QRA Annual Meeting, Edinburgh 1995, on “The Lateglacial palaeoceanography of the North Atlanic margins” (1995).

  • Rind, D.: The potential for modelling effects of different forcing factors on climate during the past 2000 years. Proc. NATO conference on Climatic Changes during the last 2000 years, in press, 1995.

  • Rochester, M. G.: Causes of fluctuations in the rotation of the Earth. Philosophical Transactions of the Royal Society, London A313, 95–105 (1984)

    Google Scholar 

  • Rosen, R. D.; Salstein, D. A.: Variations in atmospheric angular momentum on global and regional scales and the length of the day. Journal of Geophysical Research 36, 5451–5470 (1983)

    Google Scholar 

  • Ruddiman, W. F.; McIntyre, A.: The North Atlantic during the last deglaciation. Palaeogeography, Palaeoclimatology, Palaeoecology 35, 145–214 (1981)

    Google Scholar 

  • Schove, D. J.: The sunspot cycle, 649 BC to AD 2000. J. Geophys. Res. 60, 127–146 (1955)

    Google Scholar 

  • Shennan, I.: Holocene sea-level changes in the North Sea region. In: Tooley, M. Shennan, I. (eds.), Sea-Level Changes, p. 109–151. Blackwell, Oxford 1987.

    Google Scholar 

  • Stephenson, F. R.: The Earth's rotation as documented by historical data. In: Flodmark, S. (ed.), New Approaches in Geomagnetism and the Earth's Rotation, pp. 87–113. World Sci. Publ., Singapore 1991.

    Google Scholar 

  • Stuver, M.; Braziunas, T. F.: Sun, ocean, climate and atmospheric14CO2: an evaluation of causal and spectral relationships. The Holocene 3, 289–305 (1993)

    Google Scholar 

  • Stuiver, M.; Quay, P. D.: Changes in atmospheric carbon-14 attributed to a variable Sun. Science 270: 11–19 (1980)

    Google Scholar 

  • Thiede, J.: Reworked neritic fossils in upper Mesozoic and Cenozoic central Pacific deep-sea sediments monitor sea-level changes. Science 211, 1422–1424 (1981)

    Google Scholar 

  • Vandal, G. M.; Fitzgerald, W. F.; Boutron, C. F.; Candelone, J.-P.: Variations in mercury deposition to Antarctica over the past 34,000 years. Nature 362, 621–623 (1993)

    Google Scholar 

  • Wanner, H.; Brázdil, R.; Frich, P.; Frydendahl, K.; Jonsson, T.; Kingston, J.; Pfister, C.; Rosenörn, S.; Wishman, E.: Synoptic interpretation of monthly weather maps for the late Maunder Minimum (1675–1704). In: Climatic trends and anomalies in Europe 1675–1715. Frenzel, B. (ed.), Paläoklimaforschung 13: 401–424 (1994)

    Google Scholar 

  • Zazo, C.; Goy, J. L.; Lario, J.; Silva, P.: Littoral zone and rapid climatic changes during the last 20,000 years BP. The Iberia. Zeitschrift für Geomorphology N. S., in press (1995)

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  1. Paleogeophysics & Geodynamics, Stockholm University, S-10691, Stockho 1m, Sweden

    Mörner N. -A. (Prof. Dr.)

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Mörner, N.A. Earth rotation, ocean circulation and paleoclimate. GeoJournal 37, 419–430 (1995). https://doi.org/10.1007/BF00806932

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