Physics
Scientific paper
Jan 2012
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012georl..3901701d&link_type=abstract
Geophysical Research Letters, Volume 39, Issue 1, CiteID L01701
Physics
Global Change: Climate Variability (1635, 3305, 3309, 4215, 4513), Paleoceanography: Insolation Forcing, Paleoceanography: Sea Surface Temperature
Scientific paper
The Holocene variability in sea surface and thermocline water temperatures (SST and TWT) in the Indo-Pacific Warm Pool (IPWP) has been reconstructed by planktonic foraminiferal Mg/Ca from sediments of the western tropical Philippine Sea. Afterward the Younger Dryas interval (YD), SST warmed gradually till ∼10 ka and remained approximately constant afterwards, but TWT rose more rapidly to a peak between ∼12 and ∼10 ka and then declined by ∼1.5°C through the Holocene. The trend of TWT closely followed the boreal summer insolation and could be correlated to tropical climate changes represented by southward movement of the Inter-tropical Convergence Zone (ITCZ) and related changes in East Asian monsoons.
Bassinot Franck
Cheng Xinrong
Dang Haowen
Jian Zhimin
Qiao Peijun
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