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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Geochemistry of coral from Papua New Guinea as a proxy for ENSO ocean-atmosphere interactions in the Pacific Warm Pool
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Geochemistry of coral from Papua New Guinea as a proxy for ENSO ocean-atmosphere interactions in the Pacific Warm Pool

机译:来自巴布亚新几内亚的珊瑚的地球化学,作为ENSP太平洋暖池中海洋与大气相互作用的替代物

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摘要

A Porites sp. coral growing offshore from the Sepik and Ramu Rivers in equatorial northern Papua New Guinea has yielded an accurate 20-year history (1977-1996) of sea surface temperature (SST), river discharge, and wind-induced mixing of the upper water column. Depressions in average SSTs of about 0.5-1.0degreesC (indicated by coral Sr/Ca) and markedly diminished freshwater runoff to the coastal ocean (indicated by coral delta(18)O, delta(13)C and UV fluorescence) are evident during the El Ni (n) over tildeo - Southern Oscillation (ENSO) events of 1982-1983, 1987 and 1991-1993. The perturbations recorded by the coral are in good agreement with changes in instrumental SST and river discharge/precipitation records, which are known to be diagnostic of the response of the Pacific Warm Pool ocean-atmosphere system to El Ni (n) over tildeo. Consideration of coastal ocean dynamics indicates that the establishment of northwest monsoon winds promotes mixing of near-surface waters to greater depths in the first quarter of most years, making the coral record sensitive to changes in the Asian-Australian monsoon cycle. Sudden cooling of SSTs by similar to1degreesC following westerly wind episodes, as indicated by the coral Sr/Ca, is consistent with greater mixing in the upper water column at these times. Furthermore, the coral UV fluorescence and oxygen isotope data indicate minimal contribution of river runoff to surface ocean waters at the beginning of most years, during the time of maximum discharge. This abrupt shift in flood-plume behaviour appears to reflect the duration and magnitude of northwest monsoon winds, which tend to disperse flood plume waters to a greater extent in the water column when wind-mixing is enhanced. Our results suggest that a multi-proxy geochemical approach to the production of long coral records should provide comprehensive reconstructions of tropical paleoclimate processes operating on interannual timescales. (C) 2004 Elsevier Ltd. All rights reserved.
机译:多孔藻在巴布亚新几内亚赤道北部的塞皮克河和拉木河附近生长的珊瑚已经产生了准确的20年历史(1977-1996)海面温度(SST),河水排放以及风诱发的上水柱混合。在夏季期间,平均SST降低约0.5-1.0°C(由珊瑚Sr / Ca表示),并且显着减少了流入沿海海洋的淡水径流(由珊瑚δ(18)O,δ(13)C和紫外线荧光指示)。 1982-1983年,1987年和1991-1993年发生的海浪-厄尔尼诺事件引起的厄尔尼诺事件。珊瑚记录的扰动与仪器海表温度和河流排泄/降水记录的变化非常吻合,众所周知,这可以诊断太平洋暖池海洋大气系统对提尔迪奥对El Ni(n)的响应。对沿海海洋动力学的考虑表明,西北季风风的建立在大多数年份的第一季度促进了近地表水的混合到更大的深度,使珊瑚记录对亚洲-澳大利亚季风周期的变化敏感。如珊瑚Sr / Ca所示,西风突然发生后,SST的骤冷温度接近1°C,这与此时上部水柱中的混合量更大有关。此外,珊瑚的紫外线荧光和氧同位素数据表明,在大多数年份开始的最大流量时期,河流径流对地表海洋水的贡献最小。洪水软泥行为的这种突然变化似乎反映了西北季风的持续时间和强度,当加强风向混合时,它们倾向于在更大程度上分散洪水羽流在水柱中的分布。我们的研究结果表明,采用多种代理地球化学方法来生产长珊瑚记录,应能在年际尺度上全面重建热带古气候过程。 (C)2004 Elsevier Ltd.保留所有权利。

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