Hostname: page-component-586b7cd67f-tf8b9 Total loading time: 0 Render date: 2024-11-27T23:31:12.488Z Has data issue: false hasContentIssue false

Changes of Subtropical North Pacific Radiocarbon and Correlation with Climate Variability

Published online by Cambridge University Press:  18 July 2016

Ellen R M Druffel
Affiliation:
Department of Earth System Science, University of California, Irvine, California 92697, USA. Email: [email protected].
S Griffin
Affiliation:
Department of Earth System Science, University of California, Irvine, California 92697, USA. Email: [email protected].
T P Guilderson
Affiliation:
Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California 94551, USA
M Kashgarian
Affiliation:
Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California 94551, USA
J Southon
Affiliation:
Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California 94551, USA
D P Schrag
Affiliation:
Laboratory for Geochemical Oceanography, Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, USA
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

We show that high-precision radiocarbon (Δ14C) measurements from annual bands of a Hawaiian surface coral decreased by 7‰ from AD 1893 to 1952. This decrease is coincident with the Suess Effect, which is mostly due to the dilution of natural levels of 14C by 14C-free fossil fuel CO2. This decrease is equal to that expected in surface waters of the subtropical gyres, and indicates that the surface waters of the North Pacific were in steady state with respect to long term mixing of CO2 during the past century. Correlation between Δ14C and North Pacific gyre sea surface temperatures indicates that vertical mixing local to Hawaii and the North Pacific gyre as a whole is the likely physical mechanism to result in variable Δ14C. Prior to 1920, this correlation starts to break down; this may be related to the non-correlation between biennial Δ14C values in corals from the southwest Pacific and El Niño events observed during this period as well.

Type
Articles
Copyright
Copyright © The Arizona Board of Regents on behalf of the University of Arizona 

References

Bjerknes, J. 1969. Atmospheric teleconnections from the equatorial Pacific. Monthly Weather Review 97:163–72.2.3.CO;2>CrossRefGoogle Scholar
Broecker, W, Peng, T, Engh, R. 1980. Modeling the carbon system. Radiocarbon 22(3):565–98.Google Scholar
Broecker, W, Peng, T, Stuiver, M. 1978. An estimate of the upwelling rate in the equatorial Atlantic based on the distribution of bomb radiocarbon. Journal of Geophysical Research 83:6179–86.Google Scholar
Broecker, WS, Peng, TH. 1974. Gas exchange rates between air and sea. Tellus 26:2135.Google Scholar
Cathcart, E. 1996. . Univ. of San Diego.Google Scholar
Cole, J, Fairbanks, R. 1990. The Southern Oscillation recorded in the oxygen isotopes of corals from Tarawa Atoll. Paleoceanograpy 5:667–83.Google Scholar
Davis, R. 1976. Predictability of sea surface temperature and sea level pressure anomalies over the North Pacific Ocean. Journal of Physical Oceanography 6: 249–66.2.0.CO;2>CrossRefGoogle Scholar
Deser, C, Alexander, M, Timlin, M. 1996. Upper-ocean thermal variations in the North Pacific during 1970–1991. Journal of Climate 9:1840.Google Scholar
Druffel, E. 1997. Pulses of rapid ventilation in the North Atlantic surface ocean during the last century. Science 275:1454–7.Google Scholar
Druffel, ERM. 1987. Bomb radiocarbon in the Pacific: annual and seasonal timescale variations. Journal of Marine Chemistry 45:667–98.Google Scholar
Druffel, E, Griffin, S. 1999. Variability of surface ocean radiocarbon and stable isotopes in the southwestern Pacific. Journal of Geophysical Research 104(C10): 23607–13.Google Scholar
Druffel, ERM. 1985. Detection of El Niño and decade timescale variations of sea surface temperature from banded coral records: implications for the carbon dioxide cycle. In: Proceedings of the AGU Chapman Conference on Natural CO2 Changes. Geophysical Monographs 32:111–2.Google Scholar
Druffel, ERM. 1989. Decade time scale variability of ventilation in the North Atlantic determined from high precision measurements of bomb radiocarbon in banded corals. Journal of Geophysical Research 94: 3271–85.Google Scholar
Druffel, ERM, Griffin, S. 1993. Large variations of surface ocean radiocarbon: evidence of circulation changes in the southwestern Pacific. Journal of Geophysical Research 98:20249–59.Google Scholar
Dunbar, RB, Wellington, GM. 1981. Stable isotopes in a branching coral monitor seasonal temperature variation. Nature 293:453–5.Google Scholar
Fairbanks, RG, Dodge, RE. 1979. Annual periodicity of the 18O/16O and 13C/12C ratios in the coral Montastrea Annularis. Geochimica et Cosmochimica Acta 43:1009–20.Google Scholar
Fine, R, Peterson, W, Ostlund, H. 1987. The penetration of tritium into the tropical Pacific. Journal of Physical Oceanography 17(5):553–64.Google Scholar
Griffin, SM, Druffel, ERM. 1985. Woods Hole Oceano-graphic Institution Radiocarbon Laboratory: sample treatment and gas preparation. Radiocarbon 27(1):4351.Google Scholar
Gu, D, Philander, S. 1995. Secular changes of annual and interannual variability in the tropics during the past century. Journal of Climate 8:864–76.2.0.CO;2>CrossRefGoogle Scholar
Gu, D, Philander, S. 1997. Interdecadal climate fluctuations that depend on exchanges between the tropics and extratropics. Science 275:805–7.Google Scholar
Guilderson, T, Schrag, D. 1998. Abrupt shift in subsurface temperatures in the tropical Pacific associated with changes in El Niño. Science 281:240–3.CrossRefGoogle ScholarPubMed
Guilderson, T, Schrag, D, Goddard, E, Kashgarian, M, Wellington, G, Linsley, B. 2000. Southwest subtropical Pacific surface water radiocarbon in a high-resolution coral record. Radiocarbon 42(2):249–56.Google Scholar
Guilderson, T, Schrag, D, Kashgarian, M, Southon, J. 1998. Radiocarbon variability in the Western Equatorial Pacific inferred from a high-resolution coral record from Nauru Island. Journal of Geophysical Research 103(C11):24641–51.CrossRefGoogle Scholar
Guilderson, T, Schrag, D, Goddard, E, Kashgarian, M, Druffel, E. 2001. Subtropical North Pacific surface water radiocarbon history in a high-resolution coral record. Journal of Physcial Oceanography. Submitted.Google Scholar
Hasselmann, K. 1976. Stochastic climate models, Part I: Theory. Tellus 28:473–85.Google Scholar
Hudson, J, Shinn, E, Halley, R, Lidz, B. 1976. Sclerochronology: a tool for interpreting past environments. Geology 4:361–4.Google Scholar
Kaplan, A, Cane, MA, Kushmin, Y, Clement, AC, Blumenthal, , Rajagopalan, B. 1998. Analyses of global sea surface temperature 1856–1991. Journal of Geophysical Research. 103(C9):18,56789.Google Scholar
Knutson, DW, Buddemeier, RW, Smith, SV. 1972. Coral chronometers: seasonal growth bands in reef corals. Science 177:270–2.Google Scholar
Latif, M, Barnett, T. 1994. Causes of decadal climate variability over the North Pacific and North America. Science 266:634–7.Google Scholar
Linn, LJ, Delaney, ML, Druffel, ERM. 1990. Trace metals in contemporary and 17th-century Galapagos corals: proxy records of seasonal and annual variations. Geochimica et Cosmochima Acta 54:387–94.Google Scholar
Linsley, B, Wellington, G, Schrag, D. 2000. Decadal sea surface temperature variability in the sub-tropical South Pacific (1726 to 1997 A.D.). Science 290(5494):1145–8.CrossRefGoogle Scholar
Lysne, J, Chang, P, Giese, B. 1997. Impact of the extratropical Pacific on equatorial variability. Geophysical Research Letters 24(21):2589–92.Google Scholar
Mantua, N, Hare, S, Zhang, Y, Wallace, J, Francis, R. 1969. A Pacific interdecadal climate oscillation with impacts on salmon production. Bulliten of the American Meteorological Society 78:1069–79.Google Scholar
McConnaughey, T. 1989. 13C and 18O isotopic disequilibrium in biological carbonates, I, Patterns. Geochimica et Cosmochemica Acta 53:151–62.Google Scholar
Namias, J. 1969. Seasonal interactions between the North Pacific Ocean and the atmosphere during the 1960s. Monthly Weather Reviews 97:173–92.Google Scholar
Quay, P, Stuiver, M, Broecker, W. 1983. Upwelling rates for the equatorial Pacific Ocean derived from the bomb 14C distribution, Journal of Marine Research 41:769–92.Google Scholar
Schrag, D. 1999. Rapid analysis of high-precision Sr/Ca ratios in corals and other marine carbonates. Paleoceanography 14(2): 97102.Google Scholar
Shen, G, Cole, J, Lea, D, Linn, L, McConnaughey, T, Fairbanks, R. 1992. Surface ocean variability at Galapagos from 1936–1982: calibration of geochemical tracers in corals. Paleoceanography 7(5):563–88.Google Scholar
Stuiver, M, Polach, HA. Discussion: Reporting of14C data. Radiocarbon 19(3):355–63.Google Scholar
Stuiver, M, Quay, P. 1981. Atmospheric14C changes resulting from fossil fuel CO2 release and cosmic ray flux variability. Earth and Planetary Science Letters 53:349–62.Google Scholar
Suess, HE. 1953. Natural radiocarbon and the rate of exchange of carbon dioxide between the atmosphere and the sea. In: Proceedings of the Conference on Nuclear Processes in Geological Settings. Chicago: University of Chicago Press. p 52–6.Google Scholar
Swart, P, Coleman, M. 1980. Isotopic data for scleractinian corals explain their paleotemperature uncertainties. Nature 283: 557–9.Google Scholar
Toggweiler, J, Dixon, K, Bryan, K. 1989. Simulations of radiocarbon in a coarse-resolution world ocean model 1. Steady state prebomb distributions. Journal of Geophysical Research 94(C6):8217–42.Google Scholar
Trenberth, K, Hoar, T. 1997. El Niño and climate change. Geophysical Research Letters 24:3057–60.Google Scholar
Trenberth, K, Hurrell, J. 1994. Decadal atmosphere-ocean variations in the Pacific. Climate Dynamics 9:303–19.Google Scholar
Vogel, JS, Southon, JR, Nelson, DE. 1987. Catalyst and binder effects in the use of filamentous graphite for AMS. Nuclear Instruments and Methods in Physics Research B 29:50–6.Google Scholar
Weber, J. 1974. 13C/12C ratios as natural isotopic tracers elucidating calcification processes in reef-building and non-reef-building corals. In: Proceedings of the Second International Coral Reef Symposium. Brisbane: Great Barrier Reef Committee. p 289–98.Google Scholar
Weber, J, Woodhead, P. 1972. Temperature dependence of oxygen-18 concentration in reef coral carbonates. Journal of Geophysical Research 77:463–73.CrossRefGoogle Scholar
Weil, S, Buddemeier, R, Smith, S, Kroopnick, P. 1981. The stable isotopic composition of coral skeletons: control by environmental variables. Geochimica et Cosmochimica Acta 45:1147–53.Google Scholar
White, W. 1995. Design of a global observing system for gyre-scale upper ocean temperature variability. Progress in Oceanography 136:169217.Google Scholar
Zorita, E, Frankignoul, C. 1997. Modes of No. Atlantic decadal variability in the ECHAM1/lsg coupled ocean-atmosphere general circulation model. Journal of Climate 10:183200.2.0.CO;2>CrossRefGoogle Scholar