Dataset of atmospheric factors for the late Pleistocene continental drift and modern topography numerical experiment-National Tibetan Plateau Data Center

The climate model used is a fast air sea coupled model (famous) developed jointly by the British meteorological agency and the University of England. In the famous model, the horizontal resolution of the atmospheric model is 5 °× 7.5 ° and there are 11 layers in the vertical direction; the horizontal resolution of the ocean model is 2.5 °× 3.75 ° and there are 20 layers in the vertical direction. The atmosphere and the ocean are coupled once a day without flux adjustment

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Cite as:

LI Xinzhou. Dataset of atmospheric factors for the late Pleistocene continental drift and modern topography numerical experiment. National Tibetan Plateau Data Center, 2019. (Download the reference： RIS | Bibtex )

Related Literatures:

1. Liu, X., Dong, B., Yin, Z.Y., Smith, R.S., & Guo, Q. (2017). Continental drift and plateau uplift control origination and evolution of Asian and Australian monsoons. Scientific reports, 7, 40344.( View Details | Bibtex)

2. Liu, X.D., Dong, B.W., Yin, Z.Y., Smith, R.S. and Guo, Q.C. (2019). Continental Drift, Plateau Uplift, and the Evolutions of Monsoon and Arid Regions in Asia, Africa, and Australia during the Cenozoic, Sci. China: Earth Sci., 62, 1053-1075( View Details | Bibtex)

Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.

Support Program

Pan-Third Pole Environment Study for a Green Silk Road-A CAS Strategic Priority A Program (No:XDA20000000)

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