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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Regional calibration of coral-based climate reconstructions from palau, west pacific warm pool (WPWP)
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Regional calibration of coral-based climate reconstructions from palau, west pacific warm pool (WPWP)

机译:西太平洋暖池(WPWP)帕劳的珊瑚气候重建的区域校准

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摘要

Stable isotopic and trace element records from corals collected within the West Pacific Warm Pool (WPWP) are well suited to examine interannual to decadal climate variability associated with the El Ni?o-Southern Oscillation (ENSO) phenomenon. The most commonly used climate recorder in corals is δ~(18)O (δ~(18)O_(CRL)), a parameter subject to multiple regional and local environmental influences. Location-specific calibration of δ~(18)O_(CRL) is a necessary first step for developing long-term paleoceanographic reconstructions. Here we present four new coral δ~(18)O stratigraphies from the Republic of Palau (7.5°N 134.5°E), and compare our records with instrumental measurements for the period 1950-2008. We also compare our results with a previously published coral record from Palau. We employ a new sea surface salinity (SSS) product and validate its utility for coral-based paleoclimate calibrations. We not only examine differences among the records but also identify strong and regionally coherent environmental signals. We find that SSS variability is the dominant influence on δ~(18)O_(CRL) in Palau, while sea surface temperature (SST) is of secondary importance. Our results show that time-averaging multiple δ~(18)O_(CRL) records into a single composite series produce greater correlations with instrumental data and indices than individual stratigraphies alone. Our results are consistent with observations of a strengthening of the hydrological cycle in the WPWP region over the past 50years, though the magnitudes of long term linear trends differ among the different Palau δ~(18)O_(CRL) records. Interannual and interdecadal variabilities between the Palau δ~(18)O_(CRL) records are more consistent than the long term linear trends. Monthly Palauan δ~(18)O_(CRL) anomalies capture strong El Ni?o events with high fidelity over the calibration period. This study provides constraints for future paleoenvironmental investigations in Palau using longer coral records.
机译:来自西太平洋暖池(WPWP)内收集的珊瑚的稳定同位素和微量元素记录非常适合检查与厄尔尼诺-南方涛动(ENSO)现象相关的年际至年代际气候变化。珊瑚中最常用的气候记录器是δ〜(18)O(δ〜(18)O_(CRL)),该参数受多个区域和本地环境影响。 δ〜(18)O_(CRL)的位置特定校准是开发长期古海洋学重建的必要第一步。在这里,我们介绍了帕劳共和国(7.5°N 134.5°E)的四个新的珊瑚δ〜(18)O地层,并将我们的记录与1950-2008年期间的仪器测量值进行了比较。我们还将我们的结果与帕劳以前发表的珊瑚记录进行了比较。我们采用了新的海面盐度(SSS)产品,并验证了其可用于基于珊瑚的古气候校准。我们不仅要检查记录之间的差异,还要确定强烈的和区域一致的环境信号。我们发现,SSS的变异性是帕劳δ〜(18)O_(CRL)的主要影响因素,而海面温度(SST)次要。我们的研究结果表明,将多个δ〜(18)O_(CRL)记录的时间平均化为单个组合序列,与单独的地层相比,与仪器数据和指标的相关性更高。尽管在不同的帕劳δ〜(18)O_(CRL)记录中长期线性趋势的大小不同,但我们的结果与过去50年中WPWP地区水文循环加强的观察结果一致。帕劳δ〜(18)O_(CRL)记录之间的年际和年代际变化比长期线性趋势更一致。在标定期间,每月的Palauanδ〜(18)O_(CRL)异常捕获到的保真度很高的El Ni?o事件。这项研究为帕劳使用较长珊瑚记录的未来古环境研究提供了限制。

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