Atmospheric and oceanic evidences of El Nino Southern Oscillation events in the south central Pacific Ocean from coral stable isotopic records over the last 137 years
M. Boiseau et al., Atmospheric and oceanic evidences of El Nino Southern Oscillation events in the south central Pacific Ocean from coral stable isotopic records over the last 137 years, PALEOCEANOG, 13(6), 1998, pp. 671-685
We measured delta(18)O and delta(13)C in Porites lutea collected in the Moo
rea lagoon where the instrumental records show that an El Nino-Southern Osc
illation (ENSO) event implies both a cloud cover decrease and a weak sea su
rface temperature(SST) increase. Two proxies allow an ENSO record to be rec
onstructed at Moorea: the annual delta(13)C anomaly, associated with the So
uth Pacific Convergence Zone motion, and an annual delta(18)O anomaly showi
ng increased SST. The frequency bands exhibited by the singular spectral an
alysis (SSA) and the multitaper method of the annual delta(18)O and delta(1
3)C records are centered on 2.5 and 5.2 years and 2.4 and 3.2 years, respec
tively, which are the main ENSO modes. We used SSA to reconstruct ENSO even
ts at Moorea over the past 137 years. Results indicate that climate variabi
lity at this site is strongly affected by ENSO events.