Elsevier

Earth Science Frontiers

Volume 16, Issue 6, November 2009, Pages 226-239
Earth Science Frontiers

RESEARCH PAPER
Modeling the East Asian Climate During the Late Cretaceous (80 Ma)

https://doi.org/10.1016/S1872-5791(08)60120-7Get rights and content

Abstract

In this study, the East Asian climate during the Late Cretaceous (ca 80 Ma) is examined by using the Community Climate System Model Version 2 (CCSM2) from the National Center for Atmospheric Research (NCAR) and the reconstructed palaeogeographic data. The simulation results indicate that the large-scale prevailing wind directions and pressure systems over East Asia showed a remarkable seasonal variation during 80 Ma, so that it can be inferred that there existed a monsoon circulation over East Asia at that time. Compared to the present climate, the atmospheric circulation systems over the Eurasian continent in the Late Cretaceous showed a stronger meridional feature, which was possibly correspondent to a smaller lateral extension of the Eurasian continent at that time. Moreover, under a warmer background in the Late Cretaceous, the winter and summer monsoons over East Asia showed a synchronous variation, with a stronger winter monsoon as well as a stronger summer monsoon. The pattern of annual mean precipitation was similar to that of the present climate, with the maximum precipitation appearing in the intertropical convergence zone (ITCZ) between 10°S and 10°N. There was also more precipitation over the eastern coasts of the continent adjacent to the western Pacific, with the central value exceeding 1200 mm, and there was less precipitation in the midlatitudes of the inland areas. Although a more precipitation belt also appeared near 30°N over the western Pacific, which was similar to the present climate, there was no high precipitation belt over the land of East Asia. This feature implies that the uplift of the Tibetan Plateau plays an important role in the formation of the present baiu (plum rains). Moreover, the simulated climate over East Asia during 80 Ma was warmer relative to the present and the surface air temperature was 2 °C higher at the same latitudes compared to the present climate. This simulation result is closer to the estimation from the geological evidences.

References (40)

  • CJ Yapp et al.

    Carbon isotopes in continental weathering environments and variations in ancient atmospheric CO2 pressure

    Earth Planet. Sci. Lett.

    (1996)
  • EJ Barron et al.

    Cretaceous climate: A comparison of atmospheric simulations with the geologic record

    Palaeogeog, Palaeoclim, Palaeoecol

    (1982)
  • RA Berner

    A model for atmospheric CO2 over Phanerozoic time

    American Journal of Science

    (1991)
  • RA Berner

    GEOCARB II: A revised model of atmospheric CO2 over Phanerozoic time

    American Journal of Science

    (1994)
  • KL Bice et al.

    Possible atmospheric CO2 extremes of warm mid-Cretaceous (Late Albian–Turonian)

    Peleoceanography

    (2002)
  • BT Huber et al.

    Deep-sea paleotemperature record of extreme warmth during the Cretaceous

    Geology

    (2001)
  • PA Wilson et al.

    Testing the Cretaceous greenhouse hypothesis using glassy foraminiferal calcite from the core of the Turonian tropics on Demerara Rise

    Geology

    (2002)
  • RM DeConto

    Late Cretaceous Climate, Vegetation, and Ocean Interactions: An Earth System Approach to Modeling an Extreme Climate. Doctor Dissertation

    (1996)
  • BU Haq et al.

    Chronology of fluctuating sea levels since the Triassic

    Science

    (1987)
  • RA Spicer et al.

    A review of terrestrial and marine climates in Cretaceous with implications for modeling the greenhouse Earth

    Geological Magazine

    (1992)
  • LY Zhang

    the formation of Qinghai-Tibet Plateau and the division of Chinese Cenozoic climate evolution

  • DS Liu et al.

    Plateau uplift and their influences on the surrounding area

  • QH Huang et al.

    Study on cretaceous paleoclimate in the Songliao Basin

    Acta Micropalaeontologica Sinica

    (1999)
  • XS Jiang et al.

    Spatio-temporal distribution of the Cretaceous deserts in central and eastern China and its climatic significance

    Sedimentary Facies and Paleogeography

    (1996)
  • XS Jiang et al.

    Primary study on pattern of general circulation of atmosphere before uplift of the Tibetan Plateau in eastern Asia

    Science in China: Series D

    (2001)
  • CS Wang et al.

    Constraints on the early uplift history of the Tibetan Plateau

    Proceedings of the National Academy of Sciences

    (2008)
  • BL Otto-Bliesner et al.

    Vegetation-induced warming of high-latitude regions during the Late Cretaceous period

    Nature

    (1997)
  • GR Upchurch et al.

    Vegetation-atmosphere interactions and their role in global warming during the latest Cretaceous

    Philos. Trans. R. Soc. Lond

    (1998)
  • J Liu et al.

    Comparison of simulated and reconstructed temperature in East China during the last millennium

    Chinese Science Bulletin

    (2005)
  • P Zhao et al.

    Modeling the East Asian climate during the last glacial maximum

    Science in China: Series D

    (2003)
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