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- W4200345523 abstract "Abstract Community Climate System Model version 4 (CCSM4) simulated warmer sea surface temperatures (SSTs) in the South China Sea (SCS) for the mid-Holocene scenario compared to the pre-Industrial. Previous sensitivity experiments using the atmospheric component of the CCSM4, the Community Atmospheric Model version 4 (CAM4), showed that warmer SSTs in the SCS suppresses rainfall over Borneo, which is in-contrary to the effect of the stronger insolation over the island. In this study, we show that warmer SSTs in the SCS, as simulated in the CCSM4, is responding to a weaker low-level wind impacted by the stronger convectional rainfall over Borneo due to stronger insolation. These results suggest that warmer SSTs in the SCS might act as a negative feedback which damps the effect of the stronger insolation on rainfall changes over Borneo." @default.
- W4200345523 created "2021-12-31" @default.
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- W4200345523 date "2021-11-01" @default.
- W4200345523 modified "2023-09-27" @default.
- W4200345523 title "Sea surface temperatures in the South China Sea as a natural thermostat to the rainfall over Borneo: preliminary results" @default.
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- W4200345523 doi "https://doi.org/10.1088/1755-1315/925/1/012009" @default.
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