这使大气升温，导致海水表面温度上升。
This heats up the atmosphere, causing sea surface temperatures to rise.
当海水表面温度下降时，较深一些的海水就会上浮，同时把这些必须营养成分带到水面处，供生活在那里的浮游植物生长的需要。
When surface waters are cold, deeper depths are allowed to upwell, bringing these essential nutrients toward the surface where the phytoplankton may use them.
世界上最高海水表面温度就出现在澳大利亚的北部。
The world's highest sea surface temperatures occur just to Australia's north.
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