Abstract
The Citarum river basin of western Java, Indonesia, which supplies water to 10 million residents in Jakarta, has become increasingly vulnerable to anthropogenic change. Citarum’s streamflow record, only ~45 years in length (1963-present), is too short for understanding the full range of hydrometeorological variability in this important region. Here we present a tree-ring based reconstruction of September–November Citarum streamflow (AD 1759–2006), one of the first such records available for monsoon Asia. Close coupling is observed between decreased tree growth and low streamflow levels, which in turn are associated with drought caused by ENSO warm events in the tropical Pacific and Indian Ocean positive dipole-type variability. Over the full length of record, reconstructed variance was at its weakest during the interval from ~1905–1960, overlapping with a period of unusually-low variability (1920–1960) in the ENSO-Indian Ocean dipole systems. In subsequent decades, increased variance in both the streamflow anomalies and a coral-based SST reconstruction of the Indian Ocean Dipole Mode signal the potential for intensified drought activity and related consequences for water supply and crop productivity in western Java, where much of the country’s rice is grown.
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Acknowledgments
This project was funded by the National Science Foundation’s Paleoclimate program, Grant No. OCE 04-02474. We thank Dr. Rizaldi Boer of Bogor National University, Java Indonesia, for providing the streamflow data. We very much appreciate the comments of the reviewers, which have significantly improved the manuscript. LDEO Contribution Number 7312.
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D’Arrigo, R., Abram, N., Ummenhofer, C. et al. Reconstructed streamflow for Citarum River, Java, Indonesia: linkages to tropical climate dynamics. Clim Dyn 36, 451–462 (2011). https://doi.org/10.1007/s00382-009-0717-2
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DOI: https://doi.org/10.1007/s00382-009-0717-2