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印度—太平洋暖池是地球上最大的暖表水,主要热量来源自大气、大气对流和强降水。西太平洋暖池区海表温度(SST)微小的变化可影响到哈德利和沃克环流的上升位置和对流的强度,进而扰动行星尺度的大气环流、大气加热以及热带水文。西太平洋暖池气候变化主要来自对翁通爪哇高原单一低沉降速率的ODP806b站位的研究,它作为热端部分用于监测整个新近纪大尺度区域气候和梯度的变化。而更高分辨率的站位在西赤道太平洋的边缘海,但往往它们受到局部过程的强烈影响。因此,对西太平
India - The Pacific Warm Pool is the largest warm water on Earth, with the main heat coming from the atmosphere, atmospheric convection and heavy rainfall. Small changes in the SST in the western Pacific warm pool area can affect the upwelling and convection intensities of the Hadley and Walker cycles, which in turn perturb the planetary-scale atmospheric circulation, atmospheric heating, and tropical hydrology. The warming of the western Pacific warm pool comes mainly from the study of a single low-deposition rate ODP806b station on the Wengtong Java highland, which is used as a hot-end component to monitor changes in climate and gradients throughout the Neogene large-scale area. Higher resolution stations are on the margins of the western equatorial Pacific, but often they are strongly influenced by local processes. Therefore, the West Pacific