中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A diatom-based reconstruction of summer sea-surface salinity in the Southern Okinawa Trough, East China Sea, over the last millennium

文献类型:期刊论文

作者Li, Dongling2; Knudsen, Mads Faurschou3; Jiang, Hui1,2; Olsen, Jesper4; Zhao, Meixun5; Li, Tiegang6; Knudsen, Karen Luise3; Seidenkrantz, Marit-Solveig3; Sha, Longbin2
刊名JOURNAL OF QUATERNARY SCIENCE
出版日期2012-11-01
卷号27期号:8页码:771-779
关键词diatom-based transfer function Kuroshio Current Pacific Decadal Oscillation Southern Okinawa Trough spectral and wavelet analyses summer sea-surface salinity (SSS)
ISSN号0267-8179
通讯作者Jiang, H (reprint author), E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.
英文摘要A high-resolution diatom record from site MD05-2908 in the Southern Okinawa Trough, East China Sea, reveals pronounced multidecadal- to centennial-scale palaeoceanographic changes throughout the last millennium. Summer sea-surface salinity (SSS) was reconstructed using a weighted averaging partial least squares diatom-based training set. The reconstructed SSS shows slightly decreasing values during the period AD 9051930 with considerable fluctuations superimposed on this general trend. Relatively high-salinity conditions during the interval AD 9051450 probably suggest a low flood frequency in north-eastern Taiwan. Furthermore, the high SSS values are associated with a strong and stable influence of the Kuroshio Current on the Southern Okinawa Trough during the Medieval Climate Anomaly. The period AD 14501930 is characterized by three low-salinity intervals (AD 14501500, AD 16251725 and AD 17701880) separated by periods of relatively high salinity. The low SSS intervals indicate increased freshwater discharge into the Southern Okinawa Trough during the Little Ice Age, probably as a result of higher flood frequencies in north-eastern Taiwan. Spectral and wavelet analyses suggest that this pattern was linked to multidecadal variations in summer SSS, presumably associated with the Pacific Decadal Oscillation. Copyright (c) 2012 John Wiley & Sons, Ltd.
学科主题Geosciences, Multidisciplinary ; Paleontology
收录类别SCI
原文出处10.1002/jqs.2562
语种英语
WOS记录号WOS:000311056700002
公开日期2013-09-24
源URL[http://ir.qdio.ac.cn/handle/337002/12489]  
专题海洋研究所_海洋地质与环境重点实验室
作者单位1.E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China
2.E China Normal Univ, Key Lab Geog Informat Sci, Shanghai 200062, Peoples R China
3.Aarhus Univ, Dept Geosci, Ctr Climate Studies, DK-8000 Aarhus C, Denmark
4.Queens Univ Belfast, Sch Geog Archaeol & Palaeoecol, Belfast BT7 1NN, Antrim, North Ireland
5.Ocean Univ China, Minist Educ, Key Lab Marine Chem Theory & Technol, Qingdao, Peoples R China
6.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
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Li, Dongling,Knudsen, Mads Faurschou,Jiang, Hui,et al. A diatom-based reconstruction of summer sea-surface salinity in the Southern Okinawa Trough, East China Sea, over the last millennium[J]. JOURNAL OF QUATERNARY SCIENCE,2012,27(8):771-779.
APA Li, Dongling.,Knudsen, Mads Faurschou.,Jiang, Hui.,Olsen, Jesper.,Zhao, Meixun.,...&Sha, Longbin.(2012).A diatom-based reconstruction of summer sea-surface salinity in the Southern Okinawa Trough, East China Sea, over the last millennium.JOURNAL OF QUATERNARY SCIENCE,27(8),771-779.
MLA Li, Dongling,et al."A diatom-based reconstruction of summer sea-surface salinity in the Southern Okinawa Trough, East China Sea, over the last millennium".JOURNAL OF QUATERNARY SCIENCE 27.8(2012):771-779.

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来源:海洋研究所

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