Publications des scientifiques de l'IRD

Brienen R. J. W., Helle G., Pons T. L., Guyot Jean-Loup, Gloor M. (2012). Oxygen isotopes in tree rings are a good proxy for Amazon precipitation and El Nino-Southern Oscillation variability. Proceedings of the National Academy of Sciences of the United States of America, 109 (42), p. 16957-16962. ISSN 0027-8424.

Titre du document
Oxygen isotopes in tree rings are a good proxy for Amazon precipitation and El Nino-Southern Oscillation variability
Année de publication
2012
Type de document
Article référencé dans le Web of Science WOS:000310515800047
Auteurs
Brienen R. J. W., Helle G., Pons T. L., Guyot Jean-Loup, Gloor M.
Source
Proceedings of the National Academy of Sciences of the United States of America, 2012, 109 (42), p. 16957-16962 ISSN 0027-8424
We present a unique proxy for the reconstruction of variation in precipitation over the Amazon: oxygen isotope ratios in annual rings in tropical cedar (Cedrela odorata). A century-long record from northern Bolivia shows that tree rings preserve the signal of oxygen isotopes in precipitation during the wet season, with weaker influences of temperature and vapor pressure. Tree ring delta O-18 correlates strongly with delta(18)Oin precipitation from distant stations in the center and west of the basin, and with Andean ice core delta O-18 showing that the signal is coherent over large areas. The signal correlates most strongly with basin-wide precipitation and Amazon river discharge. We attribute the strength of this (negative) correlation mainly to the cumulative rainout processes of oxygen isotopes (Rayleigh distillation) in air parcels during westward transport across the basin. We further find a clear signature of the El Nino-Southern Oscillation (ENSO) in the record, with strong ENSO influences over recent decades, but weaker influence from 1925 to 1975 indicating decadal scale variation in the controls on the hydrological cycle. The record exhibits a significant increase in delta O-18 over the 20th century consistent with increases in Andean delta O-18 ice core and lake records, which we tentatively attribute to increased water vapor transport into the basin. Taking these data together, our record reveals a fresh path to diagnose and improve our understanding of variation and trends of the hydrological cycle of the world's largest river catchment.
Plan de classement
Sciences du milieu [021] ; Sciences du monde végétal [076]
Localisation
Fonds IRD [F B010057317]
Identifiant IRD
fdi:010057317
Contact