Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Radiocarbon variability in the western equatorial Pacific inferred from a high-resolution coral record from Nauru Island

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/98JC02271· OSTI ID:670200
;  [1]; ;  [2]
  1. Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts (United States)
  2. Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California (United States)
We have generated a high resolution coral {Delta}{sup 14}C record spanning the last 50 years to document the seasonal and interannual redistribution of surface waters in the western tropical Pacific. Prebomb (1947{endash}1956) {Delta}{sup 14}C values average {minus}63{per_thousand} and have a total range of 30{per_thousand}. Values begin to increase in 1957, reaching a maximum of 137{per_thousand} in mid-1983. Large interannual variability of up to 80{per_thousand} closely follows the El Ni{tilde n}o-Southern Oscillation (ENSO). During each ENSO warm phase, {Delta}{sup 14}C values begin to increase, reflecting the reduction of low-{sup 14}C water upwelling in the east and the invasion of subtropical water into the western equatorial tropical Pacific. Maximum {Delta}{sup 14}C values are in phase or lag the corresponding sea surface temperature maxima in the eastern tropical Pacific, whereas the rapid return to more negative {Delta}{sup 14}C is in phase with eastern Pacific ENSO indices. The highest-amplitude excursions occur during the 1965/1966 and 1972/1973 events, when the {sup 14}C contrast is highest between the eastern Pacific and subtropics. The 1982/1983 El Ni{tilde n}o, although a larger ENSO event, has a lower {Delta}{sup 14}C amplitude, reflecting the penetration of bomb radiocarbon into the equatorial undercurrent and the reduced contrast in {Delta}{sup 14}C between thermocline and subtropical surface waters at that time. This coral record demonstrates the potential for using similar radiocarbon time series for documenting variability in Pacific shallow circulation over interannual and decadal timescales. {copyright} 1998 American Geophysical Union
OSTI ID:
670200
Journal Information:
Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: C11 Vol. 103; ISSN JGREA2; ISSN 0148-0227
Country of Publication:
United States
Language:
English

Similar Records

Coral radiocarbon constraints on the source of the Indonesian throughflow
Journal Article · Sun Jun 01 00:00:00 EDT 1997 · Journal of Geophysical Research · OSTI ID:560685

Coral Radiocarbon Records of Indian Ocean Water Mass Mixing and Wind-Induced Upwelling Along the Coast of Sumatra, Indonesia
Journal Article · Thu Feb 05 23:00:00 EST 2004 · Journal of Geophysical Research · OSTI ID:15013890

Decadal- to interannual-scale source water variations in the Caribbean Sea recorded by Puerto Rican coral radiocarbon
Journal Article · Mon Dec 04 23:00:00 EST 2006 · Climate Dynamics, vol. 29, N/A, July 1, 2007, pp. 51-62 · OSTI ID:936956