Slow warming of the northern South China Sea during the last deglaciation
| Type | Article | ||||||||
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| Date | 2008-08 | ||||||||
| Language | English | ||||||||
| Author(s) | Shintani Tomoya1, Yamamoto Masanobu1, 2, Chen Min-Te3 | ||||||||
| Affiliation(s) | 1 : Hokkaido Univ, Grad Sch Environm Sci, Sapporo, Hokkaido, Japan. 2 : Hokkaido Univ, Fac Environm Earth Sci, Sapporo, Hokkaido, Japan. 3 : Natl Taiwan Ocean Univ, Inst Appl Geophys, Chilung, Taiwan. |
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| Source | Terrestrial Atmospheric And Oceanic Sciences (1017-0839) (Chinese Geoscience Union), 2008-08 , Vol. 19 , N. 4 , P. 341-346 | ||||||||
| DOI | 10.3319/TAO.2008.19.4.341(IMAGES) | ||||||||
| WOS© Times Cited | 22 | ||||||||
| Keyword(s) | alkenone, sea surface temperature, South China Sea, MD97-2146, the last deglaciation, the last glacial maximum | ||||||||
| Abstract | We have generated a record of alkenone sea surface temperatures (SSTs) during the last 28000 years from Core MD97-2146 for the northern South China Sea (SCS). The SST record showed a typical pattern for change in the northern SCS SST. The SST during the LGM was similar to 25 degrees C, this decreased to similar to 24 degrees C to 17 ka, increased to similar to 25.5 degrees C to 14.5 ka, decreased again to similar to 24.5 degrees C to 11.8 ka, increased gradually to similar to 27 degrees C to 6 ka, and then increased more gradually to reach similar to 27.5 degrees C at present. The SST difference (Delta SSTNSCS = SSTMD97-2146 - SSTMD97-2141) between Cores MD97-2146 (the northern SCS; this study) and MD97-2141 (the Sulu Sea; Rosenthal et al. 2003) was used to characterize the SST changes in the northern SCS relative to changes in the adjacent WTP region. The Delta SSTNSCS decreased from 21 to 11.8 ka and increased after 11.8 ka, indicating slower warming of the northern SCS during the last deglaciation than that of the adjacent western tropical Pacific region. We infer that the slow warming of the northern SCS was principally a result of stronger winter monsoon during the last deglaciation and early Holocene. In addition, the cool water inflow through the Taiwan Strait after 13 ka and the warm water inflow through the Sunda Shelf after 11 ka could influence the SST in the northern SCS. | ||||||||
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