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Effect of orogeny, plate motion and land–sea distribution on Eurasian climate change over the past 30 million years

Author

Listed:
  • Gilles Ramstein

    (DSM CEN Saclay)

  • Frédéric Fluteau

    (DSM CEN Saclay
    CNRS/ORSTOM/Université P. M. Curie)

  • Jean Besse

    (CNRS/ORSTOM/Université P. M. Curie)

  • Sylvie Joussaume

    (DSM CEN Saclay
    CNRS/ORSTOM/Université P. M. Curie)

Abstract

The Eurasian climates of today, 10 million and 3O million years ago are simulated using an atmospheric general circulation model that incorporates realistic continental geography and epicontinental sea distributions. The resulting climates compare well with various palaeoclimate records. The retreat of the Paratethys–an epicontinental sea–shifts the central Asian climate from temperate to continental conditions, and plays as important a role as uplift of the Himalayan/Tibetan plateau in driving the Asian monsoon changes.

Suggested Citation

  • Gilles Ramstein & Frédéric Fluteau & Jean Besse & Sylvie Joussaume, 1997. "Effect of orogeny, plate motion and land–sea distribution on Eurasian climate change over the past 30 million years," Nature, Nature, vol. 386(6627), pages 788-795, April.
  • Handle: RePEc:nat:nature:v:386:y:1997:i:6627:d:10.1038_386788a0
    DOI: 10.1038/386788a0
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    Cited by:

    1. Liangxu Liu & Xueyong Zhao & Qinglan Meng & He Zhao & Xiaoqian Lu & Junkai Gao & Xueli Chang, 2017. "Annual Precipitation Fluctuation and Spatial Differentiation Characteristics of the Horqin Region," Sustainability, MDPI, vol. 9(1), pages 1-16, January.

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