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- W1514159251 abstract "[1] 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." @default.
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- W1514159251 date "2012-01-01" @default.
- W1514159251 modified "2023-10-10" @default.
- W1514159251 title "Decoupled Holocene variability in surface and thermocline water temperatures of the Indo-Pacific Warm Pool" @default.
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- W1514159251 doi "https://doi.org/10.1029/2011gl050154" @default.
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