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| Content Provider | Springer Nature Link |
|---|---|
| Author | Osborne, Michael C. Dunbar, Robert B. Mucciarone, David A. Druffel, Ellen Sanchez Cabeza, Joan Albert |
| Copyright Year | 2014 |
| Abstract | The West Pacific Warm Pool (WPWP) is a critical region of the global climate system that is closely linked with the El Niño-Southern Oscillation (ENSO). We have generated two monthly resolved coral δ18O (δ18OCRL) records from a key region of the WPWP, the Republic of Palau (7′N, 135′E). The isotopic time series span the years 1793–2008 and 1899–2008. During the period of overlap, the two records are well correlated at interannual and annual periods. Multiple lines of evidence demonstrate a strong ENSO signal in Palau δ18OCRL. Our records are consistent with previous investigations of twentieth-century tropical Pacific climate variability. We identify a regionally coherent bi-decadal cycle in the WPWP following the termination of the Little Ice Age. The Palau δ18OCRL records show long-term trends towards warming/freshening, suggesting a century scale increase in the strength of the hydrologic cycle associated with the WPWP. Our study represents an important addition to the network of tropical paleo-archives. |
| Starting Page | 719 |
| Ending Page | 731 |
| Page Count | 13 |
| File Format | |
| ISSN | 07224028 |
| Journal | Coral Reefs |
| Volume Number | 33 |
| Issue Number | 3 |
| e-ISSN | 14320975 |
| Language | English |
| Publisher | Springer Berlin Heidelberg |
| Publisher Date | 2014-04-04 |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Paleoclimate Palau El Niño-Southern Oscillation (ENSO) Oxygen isotopes Little Ice Age (LIA) Freshwater & Marine Ecology Oceanography |
| Content Type | Text |
| Resource Type | Article |
| Subject | Aquatic Science |
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