Evaluation of centennial-millennial eastern Indian Ocean climate variability & mechanisms during the Holocene: Surface & thermocline reconstructions

全新世百年-千年东印度洋气候变率机制评估：表面温跃层重建Delia Oppo伍兹霍尔海洋研究所摘要该项目旨在了解热带东印度洋在数十年、百年和千年时间尺度上的气候影响和动态通过重建印度洋偶极（IOD）的变化。PI建议通过混合层和温跃层从不同深度栖息地的多个物种的浮游有孔虫中生成Mg/Ca-和d18 O数据，以生成冰川，冰消，从快速积累的海洋沉积物中重建海面和温跃层温度以及d18 O海水（60厘米/千公里），这是以前收集的不莱梅大学的同事从东印度洋西部的苏门答腊岛和南部的爪哇岛。 该研究将探索过去25，000年印度洋暖池中IOD的SST变化和周期性，并重点关注特定的晚全新世时期，如中世纪变暖和小冰期。该项目还将试图将印度洋日较差的变化与厄尔尼诺/南方涛动、亚洲和非洲季风以及通过印度尼西亚洋流的环流的变化联系起来。

Evaluation of centennial-millennial eastern Indian Ocean climate variability & mechanisms during the Holocene: Surface & thermocline reconstructionsDelia OppoWoods Hole Oceanographic InstitutionAbstractThis project seeks to understand the climatic influences and dynamics, on multidecadal, centennial, and millennial time scales, of the tropical Eastern Indian Ocean by reconstructing changes in the Indian Ocean Dipole (IOD). The PI proposes to generate Mg/Ca- and d18O data from multiple species of planktonic foraminifer from different depth habitats through the mixed layer and thermocline to produce glacial, deglacial, and Holocene reconstructions of sea surface and thermocline temperatures and d18Oseawater from rapidly accumulating marine sediments (60 cm/ky) that were previously collected by Univ. Bremen colleagues from the eastern Indian Ocean west of Sumatra and south of Java. The research will explore SST variability and cyclicity of the IOD in the Indian Ocean warm pool during the last 25,000 years, as well as focus on specific late Holocene time periods such as the Medieval Warming and Little Ice Age. The project will also attempt to link IOD variability with changes in ENSO, the Asian and African monsoons and circulation through the Indonesian Throughflow.