Modelling oceanic oxygen change from the Holocene into the Anthropocene (A01)

该子项目的目的是进行瞬态模拟与全球国家的最先进的大气-海洋环流模式，结合一套地球化学模型，调查的时空变化的氧气最小区（OMZs）在全新世（过去10000年），并在未来几个世纪。聚焦于东热带南太平洋，与数据从古重建，我们将开发一个连贯的画面的内部和外部机制驱动OMZ的变化。

The aim of the subproject is to carry out transient simulations with a global state-of-the-art atmosphere-ocean general circulation model in combination with a suite of biogeochemical models to investigate the spatio-temporal variability of oxygen minimum zones (OMZs) during the Holocene (last 10000 years), and over the next few centuries. Focussing on the eastern tropical South Pacific, together with data from paleo reconstructions we shall develop a coherent picture of the internal and external mechanisms driving OMZ variability.