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A Climate Feedback Mechanism Involving Oceanic Upwelling, Atmospheric Co2 and Water Vapour

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Variations in the Global Water Budget

Abstract

Two major problems of climatic history on time scales of 1–103 years have commanded recent attention, namely the abrupt transitions (of less than 100 years duration) between warm and cold phases, and the apparently simultaneous global increase or decrease of sensible heat flux and evaporation during glacial (cold) and interglacial (warm) phases, respectively. A global geophysical feedback mechanism is proposed, based on recent evidence relating to oceanic upwelling (and downwelling). These data indicate a simultaneous increase or decrease in the atmospheric content of carbon dioxide and water vapour, both of which are responsible for changes in the ‘greenhouse effect’ in response to changes in the intensity of upwelling. Quantitative estimates are given of the variations in oceanic evaporation during the transition between the late-glacial and the Holocene. This feedback mechanism probably has caused significant changes of atmospheric CO2 and H2O on a time scale of about 100 years, leading to abrupt climatic fluctuations and marked variations in the heat budget of the ocean-atmosphere system.

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References

  • Angell, J.K. 1981 Comparison of variations in atmospheric quantities with sea surface temperature variations in the Equatorial Eastern Pacific. Mon. Weath. Rev., 109, 230–243.

    Article  Google Scholar 

  • Anon 1961–70 Marine Climatotogioal Summaries, 1961–70. Hamburg: Seewetteramt.

    Google Scholar 

  • Bacastow, R.B., Adams, J.A., Keeling, CD., Moss, D.J., Whorf, T.P. & Wong, C.S. 1980 Atmospheric carbon dioxide, the southern oscillation and the weak 1975 El Niño. Science, N.Y., 210, 66–68.

    Article  Google Scholar 

  • Baes, C.F. Jr 1981 The response of the oceans to increasing atmospheric carbon dioxide. Institute of Energy Analysis, Oak Ridge Associated Universities. ORAU/JEA-81-6(M).

    Google Scholar 

  • Baumgartner, A. & Reichel, E. 1975 The World Water Balance: Mean Annual Global, Continental and Maritime Precipitation, Evaporation and Runoffs, 179 pp. Amsterdam: Elsevier.

    Google Scholar 

  • Berner, W., Oeschger, H. & Stouffer, B. 1980 Information on the CO2 cycle from ice core studies. Radiocarbon, 22, 227–235.

    Google Scholar 

  • Broecker, W.S., Peng, T.H. & Engh, R. 1980 Modelling the carbon system. Radiocarbon, 22, 565–598.

    Google Scholar 

  • CLIMAP Project Members 1976 The surface of the ice-age Earth. Modelling the ice-age climate. Science, N.Y., 191, 1131–1144.

    Article  Google Scholar 

  • Coope, G.R. 1977 Fossil coleopteran assemblages as sensitive indicators of climatic changes during the Devonian (Last) cold stage. Phil. Trans R. Soc. Lond., B, 280, 313–340.

    Article  Google Scholar 

  • Delmas, R.J., Ascencio, J.M. & Legrand, M. 1980 Polar ice evidence that atmospheric CO2 20 000 yr BP was 50% of present. Nature, Lond., 284, 155–157.

    Article  Google Scholar 

  • Doberitz, R. 1969 Cross spectrum and filter analysis of monthly rainfall and wind data in the tropical Atlantic region. Bonner Met. Abhandl., 11, 53 pp.

    Google Scholar 

  • Eicher, U. & Siegenthaler, U. 1976 Palynological and oxygen isotope investigations on Late Glacial sediment cores from Swiss lakes. Boreas, 5, 109–117.

    Article  Google Scholar 

  • Eicher, U., Siegenthaler, U. & Wegmüller, S. 1981 Pollen and oxygen isotope analyses on Late- and Post-Glacial sediments of the Tourbière de Chirens (Dauphiné, France). Quat. Res., 15, 160–170.

    Article  Google Scholar 

  • Flohn, H. 1973 Globale Energiebilanz und Klimaschwankungen. Bonner Met. Abhandl., 19; Rhein. Westfäl. Ak. Wiss. No. 234, pp. 75–117.

    Google Scholar 

  • Flohn, H. 1979 On time scales and causes of abrupt palaeoclimatic events. Quat. Res., 12, 135–149.

    Article  Google Scholar 

  • Flohn, H. 1980 Possible climatic consequences of a man-made global warming. Int. Inst. Appl. Systems Anal. Rept RR-80-30, xi + 80 pp. Laxenburg (Austria): IIASA.

    Google Scholar 

  • Flohn, H. 1981 Klimaänderungen als Folge der CO2-Zunahme? Phys. Blätt., 37, 184–190.

    Google Scholar 

  • Frenzel, B. 1968 Grundzüge der pleistozänen Vegetationsgeschichte Nordeurasiens. In: Erdwissenschaftliche Forschungen, Vol. 1, 326 pp. Wiesbaden: Steiner Verlag.

    Google Scholar 

  • Gates, W.L., Cook, K.H. & Schlesinger, M.E. 1981 Preliminary analysis of experiments on the climatic effects of increased CO2 with an atmospheric general circulation model and a climatological ocean. J. geophys. Res., 86, 6385–6393.

    Article  Google Scholar 

  • Hastenrath, S. & Lamb, P. 1978 Heat Budget Atlas of the Tropical Atlantic and Eastern Pacific Oceans, 90 pp. University of Wisconsin Press.

    Google Scholar 

  • Hastenrath, S. & Lamb, P. 1979 Climatic Atlas of the Indian Ocean, Part II, xvii + 93 pp. University of Wisconsin Press.

    Google Scholar 

  • Hays, J.D., Imbrie, J. & Shackleton, N.J. 1976 Variations in the Earth’s orbit: Pacemaker of the ice ages. Science, N.Y., 194, 1121–1132.

    Article  Google Scholar 

  • Henning, D. & Flohn, H. 1980 Some aspects of evaporation and sensible heat flux of the Tropical Atlantic. Contr. atmos. Phys., 53, 430–441.

    Google Scholar 

  • Hollin, J.D. 1980 Climate and sea level in isotope stage 5: an East Antarctic ice surge at ∼ 95 000 BP? Nature, Lond., 283, 629–633.

    Article  Google Scholar 

  • Keeling, CD. & Bacastow, R.B. 1977 Impact of industrial gases on climate. In: Energy and Climate, pp. 72–95. Washington, D.C.: US Nat. Acad. Sciences.

    Google Scholar 

  • Kellogg, W.W. 1973 Climatic feedback mechanisms involving the polar regions. In: Climate of the Arctic, 24th Alaska Science Conference (ed. G. Weller & S.A. Bowling), pp. 111–116.

    Google Scholar 

  • Kellogg, W.W. 1977 Effects of human activities on global climate. WMO Tech. Note 156, xviii + 47 pp. Geneva: WMO.

    Google Scholar 

  • Kellogg, W.W. 1981 Feedback mechanisms in the climate system affecting future levels of carbon dioxide. In: Analysis and Interpretation of Atmospheric CO2 data (World Climate Research Program WCP-14), pp. 243–251.

    Google Scholar 

  • Korff, H.C.I. & Flohn, H. 1969 Zusammenhang zwischen dem Temperaturgefälle Äquator-Pol und den planetarischen Luftdruckgürteln. Annl. Met. (N.F.), 4, 163–164.

    Google Scholar 

  • Kukla, G. 1980 End of the last interglacial: a predictive model of the future? Palaeoecol. Africa, 12, 395–408.

    Google Scholar 

  • L’vovich, M. 1979 World Water Resources and Their Future, viii + 415 pp. Washington, D.C.: Am. Geophys. Un.

    Google Scholar 

  • Manabe, S. & Wetherald, R.T. 1980 On the distribution of climatic change resulting from an increase in CO2-content of the atmosphere. J. atmos. Sci., 37, 99–118.

    Article  Google Scholar 

  • Merlivat, L. & Jouzel, J. 1979 Global climatic interpretation of the deuterium oxygen-18 relationship for precipitation. J. geophys. Res., 84, 5029–5033.

    Article  Google Scholar 

  • Müller. H. 1979 Climatic changes during the last three interglacials. In: Man’s Impact on Climate (ed. W. Bach, J. Pankrath & W. Kellogg): Devl. atmos. Sci., 10, 29–41.

    Google Scholar 

  • Newell, R.E. 1974 Changes in the poleward energy flux in the atmosphere and ocean as a possible cause for ice ages. Quat. Res., 4, 117–127.

    Article  Google Scholar 

  • Newell, R.E., Navato, A.R. & Hsiung, J. 1978 Long-term global sea surface temperature fluctuations and their possible influence on atmospheric CO2 concentrations. Pure appl. Geophys., 116, 351–371.

    Article  Google Scholar 

  • Newell, R.E. & Dopplick, T.G. 1979 Questions concerning the possible influence of anthropogenic CO2 on atmospheric temperature. J. appl. Met., 8, 822–825.

    Article  Google Scholar 

  • Pflaumann, U. 1980 Variations of the surface water temperatures along the eastern North Atlantic continental margin (sediment surface samples, Holocene climatic optimum, and Last Glacial maximum). Palaeoecol. Africa, 12, 191–212.

    Google Scholar 

  • Prell, W.L., Hŭtson, W.H., Williams, D.F., Bé, A.W.H., Geitzenaŭuer, K. & Molfino, B. 1980 Surface circulation of the Indian Ocean during the Last Glacial maximum, approximately 18 000 yr B.P. Quat. Res., 14, 309–336.

    Article  Google Scholar 

  • Ramanathan, Y. 1981 The role of ocean-atmosphere interactions in the CO2 climate problem. J. atmos. Sci., 38, 918–930.

    Article  Google Scholar 

  • Reiter, E.R. 1978 The interannual variability of the ocean-atmosphere system. J. atmos. Sci., 35, 349–370.

    Article  Google Scholar 

  • Sarnthein, M. & Koopman, B. 1980 Late Quaternary deep-sea record on Northwest Africa dust supply and wind circulation. Palaeoecol. Africa, 12, 239–253.

    Google Scholar 

  • Shackleton, N.J. 1977 Carbon-13 in Uvigerina: tropical forest history and the Equatorial Pacific carbonate dissolution cycles. In: The Fate of Fossil Fuel CO2 in the Oceans (ed. N.R. Andersen & A. Malakoff ) : Mar. Sci., 6, 401–427.

    Google Scholar 

  • Sonntag, C., Thornweihe, U., Rudolph, J., Löhnert, E.P., Junghans, Chr., Münnich, K.O., Klitzsch, E., El Shazly, E.M. & Swailem, F.M. 1980 Isotopic identification of Saharian groundwaters, groundwater formation in the past. Palaeoecol. Africa, 12, 159–171.

    Google Scholar 

  • Trempel, U. 1978 Eine klimatologische Auswertung der meteorologischen Beobachtungen deutscher Handelsschiffen vor der Westküste Südamerikas im Zeitraum 1869–1970. Diploma Thesis: Univ. Bonn. [Unpublished.]

    Google Scholar 

  • Weber, K.-H. 1981 Abschätzungen des Energieaustausches an der Meeresoberfläche im Arabischen und Roten Meer. Diploma Thesis: Univ. Bonn. [Unpublished.]

    Google Scholar 

  • Woillard, G.M. 1979 Abrupt end of the last interglacial s.s. in NE-France. Nature, Lond., 281, 558–562.

    Article  Google Scholar 

  • Wyrtki, K. 1975 El Niño — the dynamic response of the Equatorial Pacific Ocean to atmospheric forcing. J. phys. Oceanogr., 5, 572–584.

    Article  Google Scholar 

  • Wyrtki, K. 1981 An estimate of equatorial upwelling in the Pacific. J. phys. Oceanogr., 11, 1206–1214.

    Article  Google Scholar 

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© 1983 D. Reidel Publishing Company

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Flohn, H. (1983). A Climate Feedback Mechanism Involving Oceanic Upwelling, Atmospheric Co2 and Water Vapour. In: Street-Perrott, A., Beran, M., Ratcliffe, R. (eds) Variations in the Global Water Budget. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-6954-4_31

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  • DOI: https://doi.org/10.1007/978-94-009-6954-4_31

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-009-6956-8

  • Online ISBN: 978-94-009-6954-4

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