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Synchronous Tropical South China Sea SST Change and Greenland Warming During Deglaciation
- M. Kienast, S. Steinke, K. Stattegger, S. Calvert
- Environmental Science, GeographyScience
- 16 March 2001
Alkenone sea surface temperature records from the tropical South China Sea are presented that show an abrupt temperature increase of at least 1°C at the end of the last glacial period, synchronous with the Bølling warming observed at 14.6 thousand years ago.
Synchroneity of meltwater pulse 1a and the Bolling warming:New evidence from the South China Sea
A twofold decrease in long-chain n -alcane ( n -nonacosane) concentrations in a downcore record from the northern South China Sea indicates a rapid drop in the supply of terrigenous organic matter to…
Millennial-scale dynamics of the winter cold tongue in the southern South China Sea over the past 26 ka and the East Asian winter monsoon
Palaeoclimatic insights into forcing and response of monsoon rainfall
Palaeoclimatic evidence of monsoon rainfall dynamics across different regions and timescales could help to understand and predict the sensitivity and response of monsoons to various forcing mechanisms.
Low‐latitude control on seasonal and interannual changes in planktonic foraminiferal flux and shell geochemistry off south Java: A sediment trap study
 Results from sediment trap experiments conducted in the seasonal upwelling area off south Java from November 2000 until July 2003 revealed significant monsoon-, El Nino–Southern Oscillation–, and…
North Atlantic forcing of tropical Indian Ocean climate
It is shown that slowdowns of the Atlantic meridional overturning circulation during Heinrich stadials and the Younger Dryas stadial affected the tropical Indian Ocean hydroclimate through changes to the Hadley circulation including a southward shift in the rising branch (the intertropical convergence zone) and an overall weakening over the southern Indian Ocean.
Past dynamics of the East Asian monsoon: No inverse behaviour between the summer and winter monsoon during the Holocene
Glacial to Holocene swings of the Australian–Indonesian monsoon
The Australian‐Indonesian monsoon is an important component of the climate system in the tropical Indo‐Pacific region 1 . However, its past variability, relation with northern and southern…
East Asian summer monsoon weakening after 7.5 Ma: Evidence from combined planktonic foraminifera Mg/Ca and δ18O (ODP Site 1146; northern South China Sea)
Reconstructing the southern South China Sea upper water column structure since the Last Glacial Maximum: Implications for the East Asian winter monsoon development
difference in the stable oxygen isotopes (Dd 18 O) and Mg/Ca‐based temperatures (DT) of surface‐dwelling (G. ruber) and thermocline‐dwelling (P. obliquiloculata) planktonic foraminifera and the…